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Pie Town, New Mexico (Revisited)

Posted by graywacke on July 25, 2017

Landing number 2358 (revisited); A Landing A Day blog post number 790.

Dan:  My previous landing (Quemado, Pie Town & Datil, New Mexico) requires a significant update!

In that post, I mentioned that I ordered a tee shirt from the Pieoneer (on Pieoneer.com):

I love the shirt!  It’s a little more purple than blue (the website calls it lavender) and it feels great.  (In fact, I have it on as I’m typing this post.)  But the big story on Action News is the personal note that I received:

Pie Lady of Pie Town is an award-winning short documentary film about one Kathy Knapp, the proprietor and baker from the Pieoneer.  And she signed my note!

Of course, I went to pieladyofpietown.com to check out the film.  Here’s a graphic showing just some of the awards the film has won:

Here’s their brief write-up on the film:

Kathy Knapp, once a happy, comfortable Dallas wife and business partner, ended up baking pies in a town with no traffic light, no gas station and sketchy utilities.

The Pie Lady of Pie Town is a 29 minute documentary, directed by Jane Rosemont about how Kathy’s new life has brought boundless rewards as well as deep hearthache.

It is an uplifting story of passion and perseverance. The characters in this town, straight out of the Old West, are a backdrop for her personal story.

The trailer is great!  It gives you a great feel for Pie Town (and even briefly features the Very Large Array).  Here’s the opening shot:

Certainly ties in with my new tee shirt!

You absolutely must check out the trailer.  Click HERE.

And yes, you can order the DVD.  Signing off from Pie Town –

That’ll do it . . .

KS

Greg

 

© 2017 A Landing A Day

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Quemado, Pie Town and Datil, New Mexico

Posted by graywacke on July 24, 2017

First timer?  In this formerly once-a-day blog (and now pretty much a once-every-four-or-five days blog), I use an app that provides a random latitude and longitude that puts me somewhere in the continental United States (the lower 48).  I call this “landing.”

I keep track of the watersheds I land in, as well as the town or towns I land near.  I do some internet research to hopefully find something of interest about my landing location. 

To find out more about A Landing A Day (like who “Dan” is) please see “About Landing” above.  To check out some recent changes in how I do things, check out “About Landing (Revisited).”

Landing number 2358; A Landing A Day blog post number 789.

Dan:  Today’s lat/long (34o 6.321’N, 108o 20.465’W) puts me in W-Cen New Mexico:

And my local landing map:

Traditionally, at this point in the post, I present a StreetAtlas streams-only map.  Well, as we New Jerseyans say:  fuggettaboutit.

As regulars know, I turn to Google Earth (GE) when I need to manually track what happens to rainfall that falls on my landing.  But first, there’s one thing I won’t fuggetabout and that’s the ceremonial placement of my GE yellow push-pin.  In GE’s inimitable style, the yellow pushpin will descend from the heavens.  To ride along on this descent, click HERE.

Getting back to my watershed analysis.  I ended up placing a series of “temp” yellow push-pins along my drainage pathway until I could figure out a named stream. 

Here’s the GE shot:

About halfway between my landing and the Grand Canyon, I was able to figure out that I was in the watershed of the Little Colorado River (20th hit). 

Wiki had a good Little Colorado River watershed map (showing the watershed extending SE into New Mexico):

I noticed the Zuni River, and with a little more cross-checking, was able to figure out that I, in fact, landed in the Zuni River watershed (2nd hit). 

Before I forget – of course the Little Colorado discharges to the Big Colorado, right there in the Grand Canyon (179th hit).

No surprise, I don’t have much in the way of GE Street View coverage.  But I’ll scare two birds with one stone (I’m a lousy thrower and could never kill two birds with one stone), putting the Orange Dude where my drainage makes its way under U.S. Route 60:

Just so you have some confidence in my analysis, here’s the large culvert under Route 60 that carries my drainage under the road:

And here’s what the OD sees, looking south (upstream) towards my landing:

Oh my!  Flash flood alert!  Flash flood alert!  I wonder if some runoff made it’s way under Route 60 (maybe washing that little barn away) . . .

So anyway, going back to my local landing map, you can see my three titular towns.  I think I’ll work my way west to east along Route 60.  So, I’ll start with Quemado.

Let me start with a GE overview:

In spite of its small population (230), it has some substance – a sewage treatment plant (I think) and a high school.  But surprisingly, Wiki has essentially nothing to say about Quemado, to the point that I probably shouldn’t have made it titular.  Oh, well. 

But anyway, I was perusing GE Panoramio shots, and noticed this by Jean Bourret:

What caught my eye are the four signs up near the roof that proclaim “BACK IN TIME ELAINE!” 

I have no idea what that means!  The other signs are pretty funny.  “Now Open”?? It would look more open if the owners would trim the weeds out front.   “Signs”??  Based on the signs on the building, is this where I’d go to get my sign made?

Anyway, I took to Street View to get another look at this building.  And here’s what the OD could see:

Wait a minute!  This is really different.  Which one is newer?  Well, it turns out that the GE SV shot is dated 8/2008, and the GE Pano shot was uploaded 10/2012.  So, the whole Elaine thing is more recent. . .

On the east side of town is a Catholic church, the Sacred Heart Church.  I usually don’t post church pictures, but this looks very cool, more like a historic ruin.  Here’s a GE Pano shot, also by Monsieur Bourret:

The church looks ancient (and may be), but it’s actually an active congregation!  I couldn’t find any history on the building . . .

So, it’s time to move to Pie Town (pop 128).  One might think that Pie Town was named after early settler John Pie, right?  Let’s see what Wiki has to say:

Its name comes from an early bakery that specialized in dried-apple pies; it was established by Clyde Norman in the early 1920s.

All right!  It really was named after pies!  So – you’ll never guess what Pie Town is famous for today.  Oh, so you can guess?  And – you’re right.  I’ll let some pictures do the talking.  I found an article in SeriousEats.com, with pictures by Jesse Oleson Moore:

 

And this, from Pieoneer.com (available for sale!):

[News Flash.  After writing this post, but before I published it, I went to the Pieoneer.com website and ordered the above shirt.]

And then, I found this, from NPR (12/6/12 by Claire O’Neal), which has nothing to do with pies:

The Depression is something we usually see in black and white. But there do exist some remarkable color photos from the era, taken by photographers who were hired to document the country in the 1930s and ’40s.

Russell Lee was one of more than a dozen itinerant photographers working for the Farm Security Administration, a New Deal project to redress rural poverty. He was driving across a remote part of New Mexico with his wife and stopped randomly in Pie Town to get something to eat. Who wouldn’t?

The scenes of rural New Mexico life caught his eye, and the rest became history.

Anyway, there are dozens of 1940 Pie Town Russell Lee photos on the web.  Here are a few of my favorites, beginning with a picture of a homesteader with pinto beans:

Shooting hawks that were stealing chickens:

Arriving at the town barbecue:

Men eating at the barbecue:

Getting a car unstuck:

Saying grace at the barbecue:

Homesteader’s cabin:

Moving on to Datil.  Wiki:

Datil is named after the nearby Datil Mountains. The name of the mountains came in turn from the Spanish word dátil, meaning “date”; the name most likely resulted from the fruit-like appearance of the seedpods of local yucca species.

The Very Large Array (VRA) is just 15 miles east of Datil.

VRA, eh?  Here’s a write-up from Atlas Obscura:

Western New Mexico is high, dry land, with scrub brush in the brown dirt and hills in the distance. There are no trees and few towns… and then there is the Very Large Array, 27 huge, white radio antennae arranged in a massive Y off US Route 60. Each dish is 230 tons and 82 feet in diameter, and by electronically combining all the data from the 27 dishes, astronomers can simulate the sensitivity of a dish with a diameter of 422 feet: bigger than any single dish in the world. Since its construction in the late 1970s, research has been conducted here on supernovae, black holes, dark energy and SETI, the Search for Extra-Terrestrial Life.

Here’s a NASA shot of the array:

And a closer-in GE Pano shot by Richard Ryer:

Speaking of GE Pano, it’s that time again, where I look for spectacular (but often have to settle for less-than-spectacular) GE Pano Shots.  I’ll start with this one from the less-than-spectacular camp, selected because it’s the closest to my landing (less than three miles north).  Evidently, this property is for sale, as the Pano shot is by NM West Properties:

Here’s a shot of “The Biscuit,” about 15 miles west of my landing by Lon Brehmer:

And I’ll close with a shot of The Frozen Biscuit by TammD:

That’ll do it . . .

KS

Greg

 

© 2017 A Landing A Day

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Lind, Washington

Posted by graywacke on July 19, 2017

First timer?  In this formerly once-a-day blog (and now pretty much a once-every-four-or-five days blog), I use an app that provides a random latitude and longitude that puts me somewhere in the continental United States (the lower 48).  I call this “landing.”

I keep track of the watersheds I land in, as well as the town or towns I land near.  I do some internet research to hopefully find something of interest about my landing location. 

To find out more about A Landing A Day (like who “Dan” is) please see “About Landing” above.  To check out some recent changes in how I do things, check out “About Landing (Revisited).”

Landing number 2357; A Landing A Day blog post number 788.

Dan:  Today’s lat/long (46o 59.291’N, 118o 28.967’W) puts me in SE Washington:

You can see I landed just outside of Lind:

I’m going to be using Google Earth (GE) to assist in my watershed analysis, so I’ll jump right on my yellow pushpin and cruise right on in to the greater Lind area.  Click HERE.

You may have surmised (correctly) that my streams-only Street Atlas map was lacking necessary detail for me to have a clue about my watershed analysis.  So, here’s what I figured out, thanks to GE:

As you can see, I landed in the watershed of an unnamed tributary, that extends more than 20 miles west from my landing before running into the East Low Canal.  Now I can switch over to my usual streams-only Street Atlas map:

So, the East Low Canal discharges to the Potholes East Canal; on to the Ringold Wasteway; on to the mighty Columbia (170th hit).

It turns out that a little over a year ago (May 2016), I landed about 35 miles WSW of today’s landing, in the watershed of the Potholes East Canal.  The “potholes” part of the name is associated with scablands created by the monstrous Missoula Lake floods.  As all my regular readers know (all three or four of you), I’ve featured these glacial-era floods numerous times in this blog.  Want to learn about the floods and the scablands?  Type “Othello” into the search box.

In my May 2016 post, I had this to say about the Ringold Wasteway:

I could find nothing about why the Ringold Wasteway is called the Ringold Wasteway, or, in fact why it’s called a wasteway at all . . .

Heading back to GE:  Here’s a spot where I can look at the “unnamed tributary” and my landing as well:

I had the Orange Dude look upstream towards my landing:

And here, looking downstream:

BTW – that’s not an orange cowboy hat in the foreground.  It’s a weird play of light . . .

And then, I sent the OD downstream quite a few miles to get another look at the unnamed trib:

And here’s what he sees:

Still not much of a stream. . .

So.  In somewhat of a rarity for ALAD, I’ve featured one and only one teeny little town. But Lind, bless its little heart, has two hooks.  We’ll need a little history to zero in on the first hook.  From Wiki:

The area was first settled in 1888 on a relatively barren area along the Northern Pacific Railway’s main line by the Neilson Brothers, James and Dugal. The town was named Lind by the railroad although the exact origin of that name has been lost.

In the autumn of 1888 the Neilson Brothers built the first Lind residence and two years later they built and stocked a store and opened a post office. James Neilson became the first postmaster. The first school opened in 1889 with six students in attendance. The Neilson Brothers platted the town site in June 1890 which consisted of only four square blocks.

So the Neilson brothers platted the town. Let’s take a look at the Street Atlas map of the town:

Perhaps frustrated by their apparent inability to get the town named Neilsonville, see what they did?  That’s North N Street, then North E Street.  Let me summarize:  N . . . E . . . I . . . L . . . S . . . oops!  They ran out of streets!  They’re missing O Street and N Street.  What a bummer.  Come on!  Let’s pretend the brothers Neilson managed to plat (and construct) a couple of extra streets.

Now, just imagine the Fourth of July celebration in 1910.  The Neilson brothers are up on the bandstand.  And then, when there’s a pause in the action, someone (likely a plant) shouts out:

Do you want to do the street cheer?
Crowd:  Yeah!
Give me an “N!”
And the crowd enthusiastically replies: “N!”
Give me an “E” – “E!”
Give me an “I” – “I!”
Give me an “L” – “L!”
Give me an “S” – “S!”
Give me an “O” – “O!”
Give me an “N” – “N!”
What’s that spell?  Neilson!  Louder:  Neilson!

The brothers grab hands, raise them up over their heads, and with huge smiles on their faces, acknowledge the crowd’s adoration . . .

JFTHOI, I checked GE.  And get this:

Accoding to GE, there’s an O Street!  But alas and alack, no N.

That was hook 1. What about hook 2?

We’ll now zoom ahead from July 4, 1910 to May 18, 1980.  Check out this picture taken in Lind about noon on that date, posted on the Lind town website:

Wow.  Wild clouds, eh?  And here’s a series of pictures also taken around noon in Lind:

And then here’s the town one hour later:

OK.  So here’s a series of screen shots from the website:

Here’s a GE shot to put things in geographical perspective:

And here’s some verbiage from the website:

It was in the morning of May 18, 1980, when a volcanic eruption in the south western part of the state would release an immense landslide of superheated gas and rock, with a fifteen-mile high plume of ash.

Did we even know about it, or were we concerned after we did hear about it, and did we even think that it could affect our town? No!

Although some said later that they heard the blast, most of us were not even aware of the impact the explosion would have on Lind and we just surmised that life would go on as usual. Not so!

I was standing in my neighbor’s yard and we briefly talked about the billowing clouds that appeared to be coming our way. They sure didn’t resemble the dust clouds or rain clouds that we were used to, but in all reality, they caused us no real concern.

I do remember, however, that we half-way joked that just maybe the end was near.

It was 1:00 P.M. and as the city’s street lights were coming on, we were beginning to show concern. The ash was falling all around us, covering everything in gray. Most of us gathered our family and went home to listen for news and explanation. We turned on the TV and radio, listened, wondered, worried. What is happening? Is the ash dangerous? When will it stop falling? And most asked question, “Will it still be dark in the morning?”

Here’s a shot of downtown Lind the next day:

The post goes on, describing the ash that covered the town and all of the difficulties trying to dig out / clean up.  Click HERE to check out the whole post.

Staying with the excellent Lind website, here are some back-in-the-day pictures.  I’ll start with this 1902 Lind overview:

And this 1906 shot of a farmer bring his wheat into town:

Here’s Lind’s first football team (1911):

Wow.  Just 12 guys.  Let me see – 11 on the field & 1 on the bench!  And that’s both offense & defense!

Here’s the last stage coach in Lind (1925):

I’ll close this post with a GE Panoramio shot by Valkyrie Rider,  Her shot overlooks Lind from the west:

That’ll do it . . .

KS

Greg

 

© 2017 A Landing A Day

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Big Cabin, Vinita, Spavinaw and Disney, Oklahoma

Posted by graywacke on July 14, 2017

First timer?  In this formerly once-a-day blog (and now pretty much a once-every-four-or-five days blog), I use an app that provides a random latitude and longitude that puts me somewhere in the continental United States (the lower 48).  I call this “landing.”

I keep track of the watersheds I land in, as well as the town or towns I land near.  I do some internet research to hopefully find something of interest about my landing location. 

To find out more about A Landing A Day (like who “Dan” is) please see “About Landing” above.  To check out some recent changes in how I do things, check out “About Landing (Revisited).”

Landing number 2356; A Landing A Day blog post number 787.

Dan:  Today’s lat/long (36o 30.532’N, 95o 13.704’W) puts me in NE Oklahoma:

My very-local landing map shows my immediate proximity to Big Cabin:

My somewhat-less-local landing map shows the usual VP* of mid-continent small towns:

*veritable plethora

I know my readers are chomping at the bit to find out in which watershed I landed. 

Well, here you go:

As you can see, I landed in the watershed of Rock Creek, on to the Neosho River (6th hit).  Zooming back a little:

The Rock Creek is connected to the – Neosho and the Neosho is connected to the – Arkansas (127th hit) – and the Arkansas is connected to the – Mississippi (916th hit) – and the Mississippi is connected to the Big Gulf (1258th hit) – and the Big Gulf is connected to —  all the waters of the world!

I wonder what percentage of my readers get the connection to “Dem Dry Bones?”

Anyway, it’s time for the Google Earth (GE) yellow push-pin to take its rightful place in NE Oklahoma.  Click HERE and it will be done.

GE Street View coverage of my landing is OK here in OK:

And here’s what the OD sees:

Sorry about that pesky train! 

I had the OD move a few miles SE to get a look at the Rock Creek, just before it enters the dammed-up Neosho:

Here’s the creek, much enlarged due to that dammed Neosho:

So I think this is going to be one of those little-bit-of-this, little-bit-of-that kind of posts.  I’ll start with this, from Wiki about Big Cabin:

In 2004 Big Cabin raised nearly three-fourths of its revenue from traffic citations for speeding. The state of Oklahoma enacted a law in 2004 that penalizes towns where the citation revenue exceeds 50% of the annual budget.

As a result, the town’s police force was prohibited from writing traffic tickets for six months.

Take that, Big Cabin and your obnoxious speed traps!  And BTW, yes, Big Cabin was named after a historic (but long gone) big cabin . . .

And then I saw that one Ralph Terry was born in Big Cabin.  He was a baseball player best known for pitching for the Yankees and giving up the 1962 bottom-of-the-ninth, World Series-winning homerun by Bill Mazerowski of the Pirates.

Sharing the “Notable People” billing with Ralph Terry is Grady Louis McMurtry.  Of course, I Googled him, and it got real thick real quick.  Check out Wiki’s intro:

Grady Louis McMurtry (1918 – 1985) was a student of author and occultist Aleister Crowley and an adherent of Thelema. He is best known for reviving the secret fraternal organization, Ordo Templi Orientis, which he headed from 1971 until his death in 1985.

So, I Googled Aleister Crowley, Thelema and Ordo Templi Orientis, and it got thicker and thicker. I started to copy some Wiki materials, but then realized that I was bored.  So as the editor-in-chief of ALAD, I made an executive decision to scrap this feature.  Here’s my two-sentence summary:

McMurtry and Crowley were very active in a mostly-19th century Freemason-ish secret quasi-religious movement. They took it very seriously, and dedicated their careers to promoting it.  Curious?  Hey, you’ve got a computer and know how to use Google.

 

Moving on to Vinita.  From Wiki:

Vinita was established in 1871 by Elias Boudinot (a Confederate General and politician). It was the first city in the state with electricity.

The city was first named “Downingville”, and was a primarily Native American community. It was later renamed “Vinita” after Boudinot’s friend, sculptor Vinnie Ream.

Vinnie Ream?  From Wiki

Lavinia Ellen “Vinnie” Ream (1847 – 1914) was an American sculptor. Her most famous work is the statue of Abraham Lincoln in the U.S. Capitol rotunda

Here’s a portrait of her with her work:

Peculiar, isn’t it, that a Confederate general ended up good friends with the creator of a Lincoln bust?

But the big story on Action News is that Vinita is the home of the world’s largest McDonald’s!

GE Panoramio shot by Robert E. Burke:

It wasn’t originally built as a McDonald’s, but they couldn’t resist the arch!

Spavinaw has one and only one claim to fame, but it’s a doosey.  So Big Cabin has Ralph Terry.  But Spavinaw has . . . Mickey Mantle!

And the two were teammates!  Mickey was a Yankee from 1951 until 1968 while Ralph was a Yankee from 1956 to 1957 and again from 1959 to 1964.

You can bet your bottom dollar that they exchanged stories about growing up in NE Oklahoma!

My final stop on this abbreviated tour (after skipping hookless Ketchum, Adair, Strang and Langley) is Disney.

Disney (named after Wesley Disney, an Oklahoma legislator) is geographically interesting.  It’s an island, created by the Grand Lake of the Cherokees, a reservoir created by the Pensacola Dam across the Neosho River.  Here’s a GE shot:

From Wiki:

When the dam was built in the early 30s, Disney was a different place—hundreds of workers, bosses, engineers, truck drivers, and all the services a large workforce would require were based in and near Disney.

Disney’s growth is limited by the size of the island and the technical difficulties with bringing municipal services across the dams.  Disney has its own water plant, no public sewer system (all septic), and no natural gas service.

Here’s a 1939 shot of Disney back in the dam-building heyday of the town (from TheOtherDisneys.com):

Something special was going on – I’m sure traffic wasn’t like this on a regular basis . . .

Here’s a GE Street View shot of the western-most spillway.  This spillway (along with the others) are bare bedrock!

Speaking of bare bedrock (which surrounds the island to the east, south and west), it provides a challenge for off extreme off-roaders.  Check out this video from RockBouncer.com (by Brian Lohnes), showing Bobby Tanner and his “death-defying” climb:

 

Here’s a GE Pano shot (by Tony E. Walker) of one of the spillways actually functioning as a spillway:

Staying with GE Pano shots, I’ll close with this reflective sunset shot over the lake by John Gibe:

That’ll do it . . .

KS

Greg

 

© 2017 A Landing A Day

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Mount Vernon and Citronelle, Alabama

Posted by graywacke on July 9, 2017

First timer?  In this formerly once-a-day blog (and now pretty much a once-every-four-or-five days blog), I use an app that provides a random latitude and longitude that puts me somewhere in the continental United States (the lower 48).  I call this “landing.”

I keep track of the watersheds I land in, as well as the town or towns I land near.  I do some internet research to hopefully find something of interest about my landing location. 

To find out more about A Landing A Day (like who “Dan” is) please see “About Landing” above.  To check out some recent changes in how I do things, check out “About Landing (Revisited).”

Landing number 2355; A Landing A Day blog post number 786.

Dan:  Today’s lat/long (31o 4.169’N, 88o 3.825’W) puts me in SE Alabama, just upstream from Mobile Bay (make sure you’re pronouncing it “moe-beel”):

Here’s my local landing map:

My very local streams-only map shows that I landed in the watershed of Bull Branch, on to Cedar Creek; on to the Mobile River (21st hit):

Zooming back a little, you can see the Mobile River making its way to Mobile Bay:

Let’s hop on board a yellow push-pin and head on in to the precise (yet random) location of landing 2355.  Click HERE for the trip.

As you can see, I landed in the middle of a big patch of woods, so I won’t bother with a Street View landing shot.  But I can get a view of Bull Branch:

And here’s what the Orange Dude sees:

And then there’s Cedar Creek:

Et voilà:

 

From Wiki, about Mt. Vernon:

Mt. Vernon (pop 1,600), is home to a historic psychiatric hospital, Searcy Hospital.  A land marker used for surveying land known as “Ellicott’s Stone” lies south of the town.

Ellicott’s Stone???  I featured Ellicott’s Mound not long ago – my January 1, 2017 Moniac & St. George, Georgia post.  From that post:

So a surveyor (Andrew Ellicott) built a mound marking the east end of the straight-line border between the US and Spanish Florida.  According to a treaty between the US & Spain, the line was to run from the confluence of the Flint & Chattahoochee Rivers, extending east southeast to a point marking the headwaters of the St. Mary’s River (which is where Mr. Ellicott placed his famous mound).

Here’s a GE shot showing the Mound’s location:

And a map showing the very straight line that Ellicott surveyed (the Mound is at the “Survey End Point:”

Back to now.  It turns out that the boundary between Florida and Georgia wasn’t the only straight line Mr. Ellicott surveyed. 

From Wiki, about Ellicott’s Stone:

Ellicott’s Stone is a boundary marker in northern Mobile County, Alabama. It was placed on April 10, 1799 by a joint U.S.-Spanish survey party headed by Andrew Ellicott and was added to the National Register of Historic Places in 1973.

The line stretched along the 31st parallel from the Mississippi River in the west to the Chattahoochee River in the east, and served as the boundary line between the Mississippi Territory in the United States and Spanish West Florida.

Here’s a map (note that I connected the MS/LA border to the AL/FL border with a black line):

And a Flickr shot by JimmyWayne:

Back to my earlier post:

Imagine doing this in 1800!  Dense forests everywhere; no roads, no modern surveying instruments (let alone GPS!).  He really knew his astronomy, and used the stars to determine his location.  But I can imagine starting at one end, and then being a few thousand feet too far north when you reached the other!  But no.  He nailed it.

On to the Searcy Hospital (located about 2.5 NE of my landing).  From Alabama Living:

In 1902, mental health officials in Alabama were concerned about the “increasing insanity among the negroes,” according to J.T. Searcy, superintendent of Alabama’s mental health facilities in the late 1800s and early 1900s. The doctor reported that the number of state patients had increased from 33 in 1870 to 71 in 1881, then to 241 in 1890 and 451 in 1900.

Soon, the growing numbers led to overcrowding at the state’s only asylum, the Alabama Hospital for the Insane.  Responding to the overcrowding, Searcy opened the Mount Vernon Insane Hospital, later renamed the Searcy Hospital.

And this little tidbit, from Wiki:

In 1906, 57 patients died due to an outbreak of a disease at the hospital. Initially the disease was a mystery, but it was later identified as one of the first major outbreaks of pellagra in the United States. The cause of pellagra was a mystery at the time, but one of the key observations was that it only struck the patients, not the staff.  The cause of pellagra was discovered to be the result of a vitamin deficiency, caused by the poor diet at the Hospital.

Here’s a picture of one of the buildings from Alabama Living:

And this GE Panoramio shot by Leigh Harrell:

Back to Wiki (and moving on to Citronelle):

On May 4, 1865, one of the last significant Confederate armies was surrendered by Lieutenant General Richard Taylor under the “Surrender Oak” in Citronelle.   This was the third in a series of surrenders that ended the war. Two previous surrenders occurred at Appomattox Court House, Virginia between General Robert E. Lee and General Ulysses S. Grant (the most famous, the one generally recognized as the end of the war); and the second and largest at Bennett Place near Durham, North Carolina between General William T. Sherman and General Joseph E. Johnston.

I didn’t realize that there were multiple “surrenders.”  Back to Wiki:

A living history/reenactment of the surrender occurs each year in Citronelle. The historic “Surrender Oak” no longer stands as it was destroyed by a hurricane in 1902.

Here’s the track of the 1902 “Hurricane 4” (from Wiki).  You can see its landfall just east of Mobile Bay:

By the way, they didn’t start naming hurricanes until 1953 . . .

Back to Wiki:

Citronelle sits atop the Citronelle Dome, a salt dome that is still rising, as shown by the centrifugal drainage of streams away from the center.

“Centrifugal drainage??”  Peculiar term, but I assume it means that drainage flows away from the dome; ergo, the dome has formed a hill.  How about a simple topographic map?  I stepped up and made the following:

OK, so why is Wiki talking about the dome?  Here’s some more:

In 1955 oil was discovered in this geologic structure at a greater depth than had previously been considered as feasible, and so the Citronelle Dome was among the first of many “deep” oil fields. The discovery well produced from the Glen Rose Formation at a depth of 10,879 ft.

I remember a post where I featured salt domes (my Newgulf and Boling Texas post from June 2013).  I’ll lift some of that excellent post:

So, what (you may ask) is a salt dome?  Well, I checked out Geology.com to freshen up my stale knowledge.  Since pictures are worth many words, let me start with a north-south geologic cross-section across Texas (from OK to the Gulf):

The purple layer is salt, formed by evaporating inland seas back during the Jurassic Period (thus the “J”).  FYI, the Jurassic was about 150 – 200 million years ago (the age of the dinosaurs).  After the salt was deposited, various thickness of sand, silt and clay were laid down on top of the salt.  Those are the green and orange layers shown on the cross section.

 Note that the salt layer is pretty deep, ranging from 5 km to 10 km  (aka 3 to 6 miles).

 It turns out that the salt layer is much less dense (lighter) than the overlying sands and clays, and that the salt (if given enough time), can flow, albeit very slowly.  Because the salt is less dense, it wants to rise (just like something less dense than water wants to float).

 See those purple spikes sticking up?  Those are salt domes – essentially large fingers of salt that have pushed up through the sand & clay.  Note that the ones near the coast have pushed up six miles!

 So, what does this have to do with oil?  Well, here goes:  Some of the rock layers are petroleum-producing – they were laid down with lots of organic material that under pressure & temperature (and enough time) – presto chango!  Crude!

 So, crude oil seeps out of the source rock, and tends to flow upward through the interconnected  nooks and crannies in the rock (keeping in mind that the rock is water saturated and the crude is lighter than water).

 So, the crude oil is creeping its way up, as long as the interconnected nooks and crannies give it a pathway.  The crude is particularly inclined to move through sandstone, because of all of the pore spaces between the sand grains.  So, maybe the oil is flowing up through a sandstone, and boom, it hits a real tight shale (made of clay).  No more nooks and crannies, no more movement.  The oil tends to accumulate at the top of the sand unit.

 Now it’s time to get back to salt domes.  Here’s another picture from Geology.com.

As the salt dome punches up, it deforms the surrounding rock layers (note how the layers bow upward around the salt).  See the speckled yellow unit?  It’s a sand (or sandstone).  The overlying gray is clay (or shale).  Thanks to the salt dome, the oil gets concentrated (or “trapped”) where the sand is pinched by the salt.

 So, now we’re drilling for oil, and we have smart geologists who know about salt domes and know about oil migration and how traps are formed.  So, they poke around (with a drill rig) until they run into one of the traps in the sand, and bingo, we now have a producing oil well.

Returning to the here and now, I’ll close with this artsy shot of Searcy Hospital (once again, a Pano shot by Leigh Harrell:

That’ll do it . . .

KS

Greg

 

© 2017 A Landing A Day

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Indian Springs and Mercury, Nevada

Posted by graywacke on July 4, 2017

First timer?  In this formerly once-a-day blog (and now pretty much a once-every-four-or-five days blog), I use an app that provides a random latitude and longitude that puts me somewhere in the continental United States (the lower 48).  I call this “landing.”

I keep track of the watersheds I land in, as well as the town or towns I land near.  I do some internet research to hopefully find something of interest about my landing location. 

To find out more about A Landing A Day (like who “Dan” is) please see “About Landing” above.  To check out some recent changes in how I do things, check out “About Landing (Revisited).”

Landing number 2354; A Landing A Day blog post number 785.

Dan:  Today’s lat/long (36o 35.295’N, 115o 55.021’W) puts me in far S Nevada:

My local landing map shows my two titular towns (and not much else!):

My StreetAtlas map shows me nothing of great significance concerning my watershed, so I’ll head straight to Google Earth (GE).  Hop on board, fasten your seatbelt and head for the Nevada desert.  Make sure you’ve got plenty o’ liquids for hydration, then click HERE.

So here’s a local GE shot showing my entire watershed analysis:

As you can see, runoff from that rare desert storm heads east, and ends up collecting in the general vicinity of the Elevation 3014 yellow push pin.  I added the various elevation pushpins in to show you that the water has no choice as to where it ends up.

How about that!  An obvious major road (U.S. Route 95) is right next to my landing:

And here’s what the Orange Dude sees:

The “town” of Mercury is nothing more than a government community to house employees of the Nevada Test Site (a huge piece of real estate located north of Route 95).  Its population (and infrastructure) peaked in the 1960s, at the height of our nuclear testing program.  It had 10,000 people.  The last underground nuclear test was in 1993, and according to Wiki, “the town is a shell of its former self,” with an unknown population, but likely somewhere around 500.

Here’s a GE Pano shot of the town (Photo Shop enhanced) by Brent Cooper:

Anyway, Yucca Flat is where the actual nuclear testing went on.  Here’s a GE shot showing both Yucca Flat and the mysterious “Area 51.”

Here’s a closer view of Yucca:

All of the circles are craters, the result of underground nuclear tests.  See the big crater at the far north end?  That’s Storax Sedan; more about that in a minute.

From Wiki:

Yucca Flat is a closed desert drainage basin, the site for 739 nuclear tests – nearly four of every five tests carried out at the Nevada Test Site.

Yucca Flat has been called “the most irradiated, nuclear-blasted spot on the face of the earth”.   In March 2009, TIME identified the 1970 Yucca Flat “Baneberry” Test, where 86 workers were exposed to radiation, as one of the world’s worst nuclear disasters.

[More about Baneberry in a bit.]

“Storax Sedan” [strange that they named the nuclear tests!] was a shallow underground nuclear test conducted at Yucca Flat as part of Operation Plowshare, a program to investigate the use of nuclear weapons for mining, cratering, and other civilian purposes.

The radioactive fallout from the test contaminated more US residents than any other nuclear test. The Sedan Crater is the largest man-made crater in the United States, and is listed on the National Register of Historic Places.

Here’s my GE shot of the crater:

Here’s a Wiki shot of the Storax Sedan blast:

And the crater:

Back to Wiki:

The “Baneberry” shot was on December 18, 1970. The Baneberry 10 kiloton test detonated 900 ft below the surface but its energy cracked the soil in unexpected ways, causing a fissure near ground zero and the failure of the shaft and cap.

A plume of fire and dust was released three and a half minutes after ignition, raining fallout on workers in different locations within NTS.

Here’s a Wiki pic of the “leak”:

I found out that there is an annual (only one per year) escorted tourist excursion to visit the Nevada Test Site.  There’s a great (and funny) article entitled “My Atomic Holiday” from The Atlantic (June 2012, article by Graeme Wood).  Click HERE to check it out.  Here’s a picture of the Storax Sedan crater from the article:

Of course, we must check out Area 51.  From Wiki:

The U.S. Air Force base commonly known as Area 51 is a highly classified facility [technically part of Edwards Air Force Base] within the Nevada Test Site.

The base’s current primary purpose is publicly unknown; however, based on historical evidence, it most likely supports the development and testing of experimental aircraft and weapons systems (black projects).  The intense secrecy surrounding the base has made it the frequent subject of conspiracy theories and a central component to unidentified flying object (UFO) folklore.

JFTHOI, I counted the cars parked at Area 51:

There you have it.  211 cars (or there abouts), presumably driven by people that work here. 

The area around Area 51, including the small town of Rachel on the “Extraterrestrial Highway”, is a popular tourist destination.

Here’s a GE shot of Rachel and the Extraterrestrial Highway:

So get this.  I was with my brother-in-law Peter a few weeks ago, and I heard him telling a story about taking a trip to check out Area 51 – I heard something about white SUVs and “camo dudes.”  I’ll admit that I didn’t pay close attention – I mean, after all – he’s just my brother-in-law.  But now that I’ve landed here, I thought I’d give him a call and get the lowdown.

This happened maybe 10 years ago when his wife Amy went to a professional conference in Las Vegas, and Peter decided to take a few days off and go out there with her.  So one day while she was conferencing, Peter decided to take a day trip and explore the Area 51 environs.

He headed north towards Rachel, and turned left on an unmarked dirt road that lead to the northern perimeter of Area 51.  There were no other vehicles on the road; he was driving a rental convertible, enjoying the scenery and solitude.

Here’s a GE Pano shot of “Groom Lake Road” (by foast2foast):

 

Suddenly, two white Chevy Suburbans blew past him.  They didn’t stop or bother him in any way.  According to Peter, the occupants were “camo dudes.”  Eventually (about 13 miles from the main drag), he came up to a plethora of warning signs.  Peter mentioned that one of the signs says “No Photography.”  Funny – there are about a dozen Pano pictures of the signs.  He also mentioned signs that say (of course) that trespassers are subject to arrest and imprisonment and that “deadly force” can be used. 

Here’s one of the signs (Pano by Tim Drivas):

And another from Wiki:

Peter said that he could see a white SUV on a nearby hill and he knew he was being watched. Here’s a Pano shot (by Andre/Tammy324) that’s maybe similar to what Peter saw:

He kept going until he saw a gate.  He snapped a quick picture (current status of the photo unknown).  Here’ a shot of the gate by Montes994:

He turned around, checked out Rachel, then headed back to Las Vegas. 

When we talked, Peter told me to Google “camo dudes,” so I did.  From a NY Daily News article by Laura Bult:

Thrill seekers and paranormal enthusiasts who have attempted to break into Nevada’s infamous Area 51 have almost all certainly been thwarted by armed men dressed in camouflage behind the wheel of a white unmarked pick-up truck.

These armed government contractors, dubbed “Camo Dudes” by Area 51 aficionados because of their military-style workwear, are shrouded in nearly as much secrecy as the 38,400-acre military testing site they protect.

Nearly all the trespassers are curious about the conspiracy theories that surround Area 51, which lies up to 10 miles within the base’s border.

“They’re there for pretty much one reason,” Lincoln County Sheriff Kerry Lee told the Daily News. “This is the middle of nowhere. It’s the middle of the desert. I see very few (trespasses) that are accidents,” he said.

The guards who patrol the site are alerted to intruders by sensors on the dirt roads and are authorized to detain them until sheriff’s deputies arrive. Roughly two to three people break into the area a month and get a $500 citation, Lee says.

Signs at the entrance to the Air Force base give the “Camo Dudes” authorization to use deadly force on trespassers, according to some who have attempted to break into the mysterious base.

“According to signs at the border, use of deadly force is authorized. They can shoot you,” Glenn Campbell, who lived near and researched Area 51 for 10 years in an attempt to spot extraterrestrial activity. He never saw a UFO, but he caught sight of the “Camo Dudes” on the occasions he entered the base, Campbell said.

Here’s a quick YouTube piece entitled “Arrest at Area 51,” posted by akexposures:

Time to move on to Indian Springs.  From Wiki:

In 1906 Indian Springs became a way station and watering place for the Las Vegas and Tonopah Railroad. The original rail line ran under what is now Highway 95. The LV&T ceased operation in 1918.

Here’s a GE shot of Indian Springs:

As you can see, the town is south of Route 95, and an air base N of 95.  But where are the springs?  I did a little poking around on GE Street View, and found this green section of town (near the word “Indian” on the above shot):

Wow.  Never guess Nevada, eh?  Anyway, less than half a mile away, just outside of town, here’s another Street View shot:

Back to Wiki:

Indian Springs Auxiliary Airfield also known as Indian Springs Field, was rapidly constructed in Nevada by the United States Army Air Forces the month after the Pearl Harbor attack. Indian Springs was immediately entered into service as a training camp for Army Air Force B-25 air-to-air gunnery training.

In 1947 Las Vegas AAF inactivated, and so did Indian Springs.

One year later, Indian Springs was reactivated as Indian Springs Air Force Base by the new United States Air Force.

Note:  B-25s were featured in the famous Doolittle Raid on Tokyo in April 1942, not long after Pearl Harbor.  I featured the raid in my April 2017 Ravenna MT post.  I’m sure that crew members from that raid trained right here. 

Moving along, I found an interesting story on LVStripHistory.com.  In their piece on the history of Indian Springs, they were featuring an early resident, a Mr. Lattimer.  Here’s an excerpt:

. . . in the summer of 1906, George & Belle Lattimer came to Indian Springs.

Mr. Lattimer was bitten on the arm by some poisonous insect, and the arm swelled badly and became very painful. His wife realized that he must have medical care so she made the best bed she could in the wagon, hitched up the team and started on the long ride to Las Vegas late in the afternoon of a fearfully hot day. The Lattimers had a young Indian boy living with them who helped with the ranch work. His name was Coachie Siegmuller and his parents lived at the Moapa Indian Reservation. Coachie was left in charge of things while the Lattimers were gone.

When Belle and her husband reached Vegas they came to me for help and I got the Railroad Physician to look after the suffering man. he sent them to Los Angeles on the evening train as blood poisoning had set in and he was afraid that the man might lose his arm. About a week later the Lattimers returned to Las Vegas, George being on the way of complete recovery.

While they were gone, a day or so after they had left the ranch for medical help, Coachie was sitting on the front steps. He noticed a small cloud of dust in the road to the ranch and kept a close watch on whatever it was. Later he was horrified when he identified the man approaching as ‘Wild Bill,’ a bad Indian of whom Coachie was very much afraid, so he quietly got out of sight as Wild Bill reached the porch, on the north side of the house, and sat down to rest.

From a sitting position Bill finally stretched out on his back and was soon sound asleep. Coachie was afraid to be alone with the visitor and also felt that it was his duty to protect the home of his friends so he slipped into the kitchen and took down the rifle from its nail behind the kitchen door. He crept noiselessly around the house, rested the muzzle of the rifle on the porch rail and shot Wild Bill through the head.

Then he started for his parent’s home at the Reservation where in about 10 days he was arrested for the murder of Wild Bill. He readily admitted the shooting, but seemed to think that it was a good deed and that he should be rewarded instead of punished.

When the Lattimers neared home they smelled Bill long before they reached the house and all that they could do was to shovel him into a gunnysack and bury him in the little burial plot.

A few days after the Lattimers had buried Wild Bill, Emmett Boyle, who was then the State Engineer, drove up to the ranch in the evening on his way from Reno to Vegas. He saw Belle in the lower part of the ranch tossing some good sized hogs back into the pen from which they had escaped. When she seemed to have finished this duty he asked her if he might have some supper and a bed for the night.

She invited him to stay with them for the night so they went up to the house. While she was preparing the meal he noticed she kept gong to the window to sniff the evening air. Finally, Emmett asked what the trouble was and she promptly answered, ‘Them damn dogs has dug up Wild Bill again.’

Post Script:  Coachie spent three years in the Carson City prison and after his release, lived a peaceful life.

Let’s finish off with this GE pano shot (by Hobgot) of the mountains just south of Indian Springs:

That’ll do it . . .

KS

Greg

 

© 2017 A Landing A Day

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Solomon Rapids, Beloit and Cawker City, Kansas

Posted by graywacke on June 28, 2017

First timer?  In this formerly once-a-day blog (and now pretty much a once-every-four-or-five days blog), I use an app that provides a random latitude and longitude that puts me somewhere in the continental United States (the lower 48).  I call this “landing.”

I keep track of the watersheds I land in, as well as the town or towns I land near.  I do some internet research to hopefully find something of interest about my landing location. 

To find out more about A Landing A Day (like who “Dan” is) please see “About Landing” above.  To check out some recent changes in how I do things, check out “About Landing (Revisited).”

Landing number 2353; A Landing A Day blog post number 784.

Dan:  Today’s lat/long (39o 28.482’N, 98o 12.548’W) puts me in N-Cen Kansas:

My local landing map shows two of three titular towns:

Glen Elder didn’t make the cut, and Solomon Rapids is nowhere to be seen.

You can see on the local landing map that I landed adjacent to the Solomon River (7th hit).  Here’s a zoomed-back streams-only shot:

The Solomon discharges to the Smoky Hill River (19th hit); on to the Kansas River (64th hit); on to the Missouri (422nd hit). 

And of course, the MM gets another one (its 915th).

It’s time to take a trip to the heart of the heartland.  Click HERE to watch as the Google Earth yellow pushpin settles gently into Kansas farmland.

So let’s check out the GE Street View coverage of my landing (and get our first look at Solomon Rapids):

Here’s what the Orange Dude sees:

Not far way, we can get a look at the Solomon River:

And check out the idyllic scene at the bridge (note the fishermen):

And note the minimal guard rail! No bridges look like this in NJ! 

 I zoomed in to get a little better look at the fishermen:

I think I’ll start with the town identified on Google Earth, Solomon Rapids.  Today, essentially 100% of Solomon Rapids is the Solomon Rapids Seed Company:

But there’s more to Solomon Rapids than Solomon Rapids Seed Company.  It took some effort, but I found excellent material on Solomon Rapids history.

Laura Thiessen had an article published under “Lost Kansas Communities,” put out by Kansas State University.  The title of her piece is “Killer Competition:  A Case Study of Solomon Rapids, Mitchel County Kansas, 1870 – Present.”

Here are some excerpts:

The town of Solomon Rapids was founded in 1870 with the construction of a water powered mill located along the Solomon River, about ¾ of a mile west of the present-day town.

[Interesting.  The town was right on the river, three-quarters of a mile from its current location.  More about that later.]

In the early years, business places were “a hotel, doctor, dentist, three general stores, a Presbyterian church and the grain elevator where the post office was.”  School District #11 was formed in October 1872, and Miss Mary Green was one of the first teachers.

With the establishment of the school, church and many small businesses Solomon Rapids appeared to be well on its way to being a successful town.

Willow Springs [later renamed Beloit] was founded at about the same time, and it, too was rapidly developing into a real town.

By the end of 1870, the area around Willow Springs and Solomon Rapids was well established.  Mitchel County was formed, and it was time to select a county seat.  Solomon Rapids, Willow Springs and Glen Elder were all in a race for county seat.

The founder of Willow Springs, Aaron Bell, knew that Willow Springs had the potential to be a successful town and county seat. He was able to get the people to realize the potential of Willow Springs as well and by the end of the campaign, despite Solomon Rapids having a larger population, [emphasis mine] Willow Springs won with 143 votes, Solomon Rapids had 43 votes and Glen Elder 36 votes.

The decline of Solomon Rapids (and the success of Willow Springs) began soon thereafter.

Most of the Solomon Rapids businesses were closed by 1940. The most dramatic period of decline occurred in the 50s. The post office which had been in operation since 1910 was discontinued in 1953.

Looking at GE, it’s apparent that all traces of the former town are gone, with the exception of the Solomon Rapids Seed Company.

Based on the information that the former town was ¾ of mile west of the current town (and was on the river), I figured it would have been here:

Note that there is a north-south road headed to the river at this point; likely a road that went to the former town.

And from a water-powered mill perspective, this location makes sense.  See the large meander in the river?  A mill race may have been constructed that cut across the neck of the two-mile long meander:

With a dam across the river at the upstream end of the mill race (now gone), river water would have been diverted into the gently-sloping mill race.  At the downstream end of the race, the water would have a fall of several feet down to the elevation of the Solomon (which, of course, was steadily getting lower over the course of the two-mile meander).

Of course, this is where the mill wheel would capture the water and harness the energy necessary to turn the wheel which then turned the millstone, and ground the grain into flour.

Check out this GE shot:

Could this be an old concrete structure that marks the beginning of the mill race?   If so, the dam is gone, and the river’s course has probably shifted to the east.

Alternatively, here’s a shot just a little ways downstream:

Note that the banks on either side of the river bulge in (due to some buried dam foundations preventing erosion?), and it looks like there could be a dam remnant in the middle of the river.

ALAD nation!  Especially those who live in north-central Kansas!  How about a trip to the Solomon River to conduct a little archeological investigation?

Odds are, what I’m looking at have other explanations, but one never knows . . .

On to Willow Springs – er, I mean Beloit. From Wiki:

The town site of Beloit was first settled by Aaron Bell in 1868 with the idea of utilizing water power from the Solomon River for a mill.  For some time, the town was known as Willow Springs.  Beloit is named after Beloit, Wisconsin.

Beloit’s old mill dam is still around:

And a closer view:

Here’s a picture from KansasTravel.org:

I found out that the water supply for the town comes from the river, and the intake is just above the dam.  I’m assuming that the building in the above picture has something to do with the intake.  I’m also assuming that the dam wasn’t built for water supply, but rather for the old mill (which might have been located on the concrete pad next to the dam . . .)

Anyway, I had to check out Beloit Wisconsin, just to see where the name came from.  Well, it turns out that some city father made up the name, more-or-less to sound like Detroit.  Consistent with this information, the only “Beloits” in the entire world are in the U.S.  Besides the two we already know about there are four others; all (I think) named after Beloit Wisconsin.

Time for a quick trip to Cawker City.  From Wiki:

It is one of several places claiming to be home of the largest ball of twine in the world.

It turns out that there are four ball of twine categories recognized by Wiki:

  • Largest ball of twine built by a community
  • Largest ball of twine built by a single individual
  • Heaviest ball of twine
  • Largest nylon ball of twine

Cawker City is the proud home of the largest ball of twine built by a community.  From Wiki:

In Cawker City, Kansas, Frank Stoeber created a ball that had 1.6 million feet of twine and 11-foot-diameter when he died in 1974. Cawker City built an open-air gazebo over Stoeber’s ball where every August a “Twine-a-thon” is held and more twine is added to the ball.

By 2006, the twine ball had reached 17,886 pounds, a circumference of 40 feet, and a length of 7,801,766 feet (almost 1500 miles).

In 2013, its weight was estimated at 19,973 pounds. In August 2014, the ball measures 41.42 feet in circumference, 8.06 feet in diameter and 10.83 feet in height, and it still growing.

For the record, the largest ball of twine built by a single individual is in Darwin MN.  From Wiki:

Darwin, Minnesota, is the home of a ball of baler twine rolled by Francis A. Johnson. It is 12 feet in diameter and weighs 21,140 pounds. Johnson began rolling the twine in March 1950, and wrapped four hours every day for 29 years.

OMG.  Four hours every day for 29 years!  And it’s larger than Cawker City’s ball.  Come on Cawker City!  You know what you have to do . . .

Weird Al Yankovich wrote a song about this Minnesota ball of twine.  For your listening and viewing pleasure:

 

If you listened to the whole thing, you realize what a long (and funny) song this is.  As always, Weird Al is very clever.  Here’s my favorite verse:

Oh, what on earth would make a man decide to do that kind of thing?
Oh, windin’ up twenty-one thousand, one hundred forty pounds of string.
What was he trying to prove, who was he trying to impress?
Why did he build it, how did he do, it was anybody’s guess.
Where did he get the twine, what was goin’ through his mind?
Did it just seem like a good idea at the time?

Speaking of time, it’s time for a couple of nearby GE Pano shots.  First this, by FischerFoto, from less than 2 miles S of my landing:

And then this, by Ape54321, taken between Beloit & my landing:

That’ll do it . . .

KS

Greg

 

© 2017 A Landing A Day

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Raeford and Dundarrach, North Carolina

Posted by graywacke on June 23, 2017

First timer?  In this formerly once-a-day blog (and now pretty much a once-every-four-or-five days blog), I use an app that provides a random latitude and longitude that puts me somewhere in the continental United States (the lower 48).  I call this “landing.”

I keep track of the watersheds I land in, as well as the town or towns I land near.  I do some internet research to hopefully find something of interest about my landing location. 

To find out more about A Landing A Day (like who “Dan” is) please see “About Landing” above.  To check out some recent changes in how I do things, check out “About Landing (Revisited).”

Landing number 2352; A Landing A Day blog post number 783.

Dan:  Today’s lat/long (34o 57.100’N, 79o 12.952’W) puts me in S-Cen North Carolina:

My local map shows my two titular towns:

My local streams-only map shows that I landed in the watershed of Toneys Creek, on to Raft Swamp. 

Zooming back:

Raft Swamp discharges to the Lumber River (first hit ever!); on the Little Pee Dee River (first hit ever!); on to the Pee Dee (11th hit).

I’ll open Google Earth (GE) and double click on the “landing 2352” pushpin (in the lengthy list of My Places).  Click HERE to see what happens.

You may have noted that I landed in the woods, so in spite of my close-by Street View coverage, there won’t be much to see:

Like I said:

I sent the Orange Dude a little ways south to get a look at Toneys Creek:

And here’s what he sees:

I went a little further south (I won’t bother showing you where) to get this look at Raft Swamp:

Kinda looks like a swamp, eh?

Of course, I checked out Raeford.  From Wiki:

John McRae and A.A. Williford operated a turpentine distillery and general store, respectively. Each took a syllable from his name and came up with the name Raeford for the post office they established. The McRae family, was made up primarily of old Highland Scot families. Note that in the 18th and 19th centuries, the nearby Upper Cape Fear Valley of North Carolina was the largest settlement of Gaelic-speaking Highland Scots in North America.

I’ve featured the Welsh language in a previous post (in an April 2015 post featuring Carnarvon IA), so I thought I’d feature Scottish Gaelic this time.  Here’s a Scottish weather forecast presented by Sarah Cruickshank in Scots Gaelic on BBC Alba, uploaded by money2tight2mention:

 

While perusing my local Street Atlas landing map, I noticed Dundarrach, and thought to myself “that certainly sounds Scottish!”  I embarked on a rather meandering but intense search for the name origin.  Google said next-to-nothing about the town, let alone its name origin.

Because there’s a Dundarrach Street in Charlotte (and I no longer  cared about any references to North Carolina), I had to do the following Google search:  “Dundarrach -NC -North Carolina -Charlotte.”  The minus signs tell Google to ignore any hits that contained NC, North Carolina or Charlotte.

After three pages of unhelpful entries, I found a picture entitled “Colintraive – Rhubodach ferry from Dundarrach.” 

With some research, I found the towns of Colintraive & Rhubodach, and the route of the ferry that connects the two towns. Looking at the photo, I surmised where Dundarrach must be.  Here’s the photo (with the ferry boat docked on the far shore):

And here’s where I figured Dundarrach must be (and I put a yellow push pin there):

Zooming back a little:

But then, I scrolled down from the photograph, and found a map:

Bingo!  Zooming way back, I’ll put Dundarrach into the larger Scottish scene (it’s not far west of Glasgow):

I checked out GE Street View, and son-of-a-gun if there wasn’t coverage right next to downtown Dundarrach:

The Orange Dude noticed a young mother (from Dundarrach?) out for a stroll with her wee one on a lovely day in Dundarrach Scotland:

I nudged the OD a little further south:

So he looked north to get this look of Dundarrach:

I sent him just north of Dundarrach to find this lovely shot:

And a little further north:

The Isle of Bute is right across the Kyles of Bute (the waterway) from Dundarrach:

From Wiki:  The Isle of Bute (Scottish Gaelic: Eilean Bhòid), or simply Bute, is an island in the Firth of Clyde in Scotland. It is divided into highland and lowland areas by the Highland Boundary Fault.

More about the fault in a bit.

It turns out that there’s a 13th-century castle in the Bute capital “city” of Rothesay.  Here’s a GE shot showing that the castle is right in the middle of town:

Here’s a Wiki picture of the castle:

I put the OD on a street next to the castle:

Wow.  An incredibly scenic and historic castle (with a moat!) right in the middle of town.  Very cool.

Another item of interest from Wiki:

The human occupation of Bute dates from prehistoric times. The Queen of the Inch necklace is an article of jewelry made of jet found in a tomb on the adjacent island of Inchmarnock that dates from circa 2000 BC.

Here’s a map showing the Queen’s little island:

I found a Blogpot (“Bensozia”) post about the necklace and the Queen, entitled “The Queen of the Inch,” which begins with this picture of the 4000-year old necklace:

Quoting from the post:

In the 1950s a tenant farmer on the tiny Scottish island of Inchmarnock hit a stone slab with his plow. This turned out to be the cover of a 4,000-year-old, stone-lined tomb.

Within was a single burial, a middle aged woman who became known as the Queen of the Inch. She had only a few grave goods, but among them was a spectacular jet necklace (above). The queen was dug up, examined by archaeologists, then (in the 1960s) reburied. In 2006 she was dug up again so her bones could be studied using modern techniques, and last year she was reburied again.

This time a reconstruction was made of her face, by the usual forensic method. Isotope analysis of the bones showed that she ate a mostly land-based diet, and that she probably grew up in the Scottish Isles.

She looks like she could be the lady next door!

Lord Smith of Kelvin, who owns the whole island, had this to say about the investigation and the reburial:

It is right that she goes back. When you speak with the researchers and scientists, obviously they wanted her for a period of time. But I was always clear that once they had actually looked at her properly, because we all need to understand what her forebears were like and what they did and so on, she had to go back. It’s where she belongs and it’s where she was buried and that’s where she’s going back to, to rest for ever.

Bravo for him.

For the record, note that the necklace is made of “jet.”  What’s jet?  From Wiki:

Jet is a type of lignite, a precursor to coal, and is a gemstone. It has an organic origin, being derived from ancient deposits of decaying wood under extreme pressure.

A particularly famous jet deposit from Whitby, England was laid down approximately 180 million years ago.  Jet has been mined from this location since 4,000 B.C., and perhaps earlier.

The English noun “jet” derives from the French word for the same material: jaiet.  The adjective “jet-black”, meaning as dark a black as possible, derives from this material.

Moving right along – I mentioned earlier that the “Highlands Boundary Fault” goes through the Isle of Bute.  Indeed it does:

Note on the above map that the  rock formation shown in green to the northwest of the fault is Precambrian metamorphic rock (in the very general vicinity of one billion years old).  Southeast of the fault (the beige rock formation), the rocks are Devonian sedimentary rocks (a mere 400 million years old).

How do very two completely different rock formations of completely different composition and age come to be right next to each other?  It’s the faults fault. 

Here’s a cartoonish cross-section (from the Scottish Natural Heritage website) showing the fault:

The green is the ancient metamorphic rock, and the orange is the less-ancient sedimentary rock (sandstone).

It turns out that the ancient metamorphic rocks are much more resistant to erosion than the younger sedimentary rocks.  So, the “Scottish Highlands” are northwest of the fault and the “Scottish Lowlands” are southeast of the fault.  Can you pick out the fault on this GE shot?

Here’s a cheat-sheet:

Of course, there is much geologic information about the fault, but most of it is very dry and over my head.  And I’m a geologist!

I’ll close my Dundarrach segment with two GE Pano shots of the waterway around the Isle of Bute (the Kyles of Bute).

First this, of the small islands (the Burnt Islands) just west of Dundarrach (photo by Stavrosspb):

And this, by Rainbow Chaser:

Heading back to NC, I looked and looked, but couldn’t find much in the way of decent Pano shots to close out the post.  I’ll have to settle for this, by MikeBike, of the Lumber River a few miles west of my landing:

That’ll do it . . .

KS

Greg

 

© 2017 A Landing A Day

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Post, Texas

Posted by graywacke on June 18, 2017

First timer?  In this formerly once-a-day blog (and now pretty much a once-every-four-or-five days blog), I use an app that provides a random latitude and longitude that puts me somewhere in the continental United States (the lower 48).  I call this “landing.”

I keep track of the watersheds I land in, as well as the town or towns I land near.  I do some internet research to hopefully find something of interest about my landing location. 

To find out more about A Landing A Day (like who “Dan” is) please see “About Landing” above.  To check out some recent changes in how I do things, check out “About Landing (Revisited).”

Landing number 2351; A Landing A Day blog post number 782.

Dan:  Today’s lat/long (32o 56.846’N, 101o 12.669’W) puts me in Cen-NW Texas:

This was my second Texas landing in a row, making this my 62nd double (and my 10th TX double).  As you’d expect, TX leads the pack in doubles, with CA (the second-largest-state) in second place with 9.

My local landing map shows that I landed closer to a whole passel of towns  than I landed to titular Post:

As you can readily guess, those non-titular towns are totally:

My close-in streams-only map shows that I landed in the watershed of Sand Creek:

Perhaps you can tell that I labeled the creek myself.  That’s because StreetAtlas gave me no information about the identity of the stippled blue linear splotch.  As you’ll see, good ol’ Google Earth in conjunction with the Texas DOT let me know the name of the creek.

Anyway, zooming back:

Sand Creek discharges to Double Mountain Fork of the Brazos River (8th hit); on to the Brazos (32nd hit). 

JFTHOI, I thought I’d zoom back one more time so you can see how the Brazos makes its way to the G of M:

I’ve already mentioned Google Earth, which I try not to do before my yellow pushpin flight.  Speaking of which, click HERE to check it out.

Moving right to the Google Earth connection to Sand Creek, here’s a shot showing where the creek passes a road with Street View coverage:

And here’s what the Orange Dude sees:

As mentioned previously, I can always count on the Texas DOT to label even small streams:

My Street View coverage ain’t great; I simply had the OD move down the road a little:

Note that I showed two topographically-elevated mesas, cut by the Sand Creek (with my landing in the Sand Creek valley).  Here’s what the OD sees:

It’s time for me to post a little Post in this post (from Wiki):

Post (pop 5,400) is located on the edge of the caprock escarpment of the Llano Estacado, the southeastern edge of the Great Plains.

[More about the Llano Estacado in a bit.  Continuing:]

In 1906, Charles William (C. W.) Post, the breakfast cereal manufacturer, bought 200,000 acres of ranchland and established the Double U Company to build and manage houses and commercial structures.

[AYKM?  200,000 acres?  That’s 312.5 square miles!  That’s a huge hunk of real estate that takes a lot of bowls of Grape Nuts!]

They planted trees along every street and prohibited alcoholic beverages and brothels. The Double U Company rented and sold farms and houses to settlers.

Two years later, the town had a school, a bank, and a newspaper, the Post City Post. The railroad reached the town in 1910. The town changed its name to “Post” when it incorporated in 1914, the year of C. W. Post’s death. By then, Post had a population of 1000, 10 retail businesses, a dentist, a physician, a sanitarium, and three churches (Baptist, Methodist, and Presbyterian0.

So here’s a little more about C.W. (from Wiki):

Post suffered a mental breakdown in November 1885, the result of the stress and overwork which accompanied his job as a farm implement manufacturer.  Post made a break with his previous life, moving to the state of Texas in 1886.  Post began a real estate development in Fort Worth on 200 acres that he had obtained, platting the land for streets and homes and constructing two mills.

The stress of this work again proved too much for Post’s constitution, and a second breakdown followed in 1891.  Post began a period of extensive travels in search of a cure, coming to take particular interest in the chemistry of digestion.  After a period traversing Europe, Post visited the Battle Creek Sanitarium of Battle Creek, Michigan, a facility operated by John Harvey Kellogg. He was inspired to start his own company based upon the dietary products used there.

In 1895, Post founded Postum Cereal Co., with his first product, Postum cereal beverage. Post’s first breakfast cereal premiered in 1897, and he named the product Grape-Nuts cereal because of the fruity aroma noticed during the manufacturing process and the nutty crunch of the finished product. In 1904, he followed up the Grape Nuts label with a brand of corn flakes, which was first called Elijah’s Manna before being renamed Post Toasties in 1908.

[He must have been making some big bucks, as he founded Post City in 1906-1907.]

At the end of 1913, the chronically ill Post’s health deteriorated to the point that he canceled public appearances, which prompted speculation in the press regarding his well-being.

In early March 1914, Post was believed to be suffering from appendicitis and was rushed via a nonstop train from California to Rochester, Minnesota to be operated on by William and Charles Mayo, regarded as the preeminent surgeons of the day.

Although there is some historical uncertainty about whether Post actually underwent surgery, there is no doubt that his health did not substantially improve.  On May 9, 1914, despondent over his ongoing stomach illness, Post took his own life with a self-inflicted gunshot.

His 27-year-old daughter, Marjorie Merriweather Post, inherited his company along with most of his vast fortune, one of the largest of the early 20th century .

A quick aside about Marjorie Merriweather.  From Wiki:

Mar-a-Lago is an estate and National Historic Landmark in Palm Beach, Florida, built from 1924 to 1927 by cereal-company heiress and socialite Marjorie Merriweather Post.

The 126-room house contains the Mar-a-Lago Club, a members-only club with guest rooms, a spa, and other hotel-style amenities.

At the time of her death in 1973, Post bequeathed the property to the National Park Service, hoping it could be used for state visits or as a Winter White House. However, due to the costs of maintaining the property exceeding the funds provided by Post, and the difficulty in securing the facility in the flight path of Palm Beach Airport, the property was returned to the Post Foundation by an Act of Congress in 1981.

In 1985, Mar-a-Lago was purchased by businessman Donald Trump and his then-wife Ivana Trump was put in charge of running the property.  The Trump family maintains private quarters in a separate, closed-off area of the house and grounds and since becoming President, Trump has frequently stayed there, referring to it as his “Southern White House”.

As promised, I’ll talk a little about the Llano Estacada, which is a large plateau.  Here’s a map by Meredith McClain:

I landed just off the Llano, southeast of Lubbock.

From MySite.du.edu (University of Denver):

The Llano is a very flat, semiarid plateau, ranging in elevation from 5000′ on the northwest to less than 3000′ on the southeast, sloping more or less uniformly to the east-southeast at a rate of at least 10′ per mile. The slope is imperceptible to an observer on the plateau. The Llano is dry and treeless, the prevailing wind is from the southwest, and mirages are a frequent occurrence under the hot sun.

The surface of the Llano is remarkably flat, reminding one of the sea, and it is conceivable that the curvature of the earth could be perceived as it is on the sea. The area around Levelland, Texas, would be a good place to look for grain elevators sinking beneath the horizon.

[Levelland!  More about that later.]

A sequence of sediments that eroded from the Rocky Mountains underlie the Llano Estacada; (known amongst geologists as the Ogallala Group).  These sediments were deposited by streams carrying eroded material away from the Rockies during uplift that began about 5 million years ago (during the Pliocene).  This is why the Llano slopes away from the Rockies.

What causes the Llana is the “caprock” that overlies the Ogallala.  The caprock is a hard caliche layer formed when surface drying of the sediments caused mineral-laden water to rise by capillary action to the surface. Evaporating, the minerals were left behind to cement the otherwise fairly loose sandy sediments of the Ogallala Group.

This very hard caprock is more resistant to erosion than similar sediments located in surrounding areas; thus the Llana is elevated by an average of 300’ causing the Llana Estacada escarpment.  (An escarpment is a steep slope or cliff that defines the edge of a plateau.)

Let’s take a look at the escarpment on Google Earth:

As you can tell, the escarpment is the boundary between the brown/orange region to the west from the ill-defined grayish area to the east.

I sent the Orange Dude to take a look at the escarpment just south of Post:

And here’s what he sees:

So, I mentioned the town of Levelland earlier; obviously an aptly-named town on the Llana Estacada.  I featured Levelland not long ago (in a January 2017 post).  In that non-Post post, I featured the song “Levelland” by singer-songwriter James McMurtry.  Here’s an excerpt from that post:

Moving right along.  The Levelland TX Wiki article also mentioned that a singer named James McMurtry recorded a song about the town, appropriately entitled “Levelland.”  For the record, James McMurtry is the son of famous Texas novelist Larry McMurtry, author of the well known novel Lonesome Dove, which spawned a TV mini-series of the same name.

Well, here we go.  ALAD Nation!  I love this song!  If you like good ol’ straight ahead story-telling back beat country rock ‘n roll (which is my sweet spot), this song is for you.  I highly recommend that you listen to it twice.  Once, following the words, and then, enjoying the video.

And if you’re like me, you’ll be listening again and again.  In fact, I just bought tickets to see James McMurtry in concert in Alexandria VA . . .

[Update:  I lied.  I almost bought tickets for his Alexandria show, but ended up going to his show in Blairstown NJ.  Jody and I went and absolutely loved it.  And yes, he sang “Levelland.”  And what the heck; for those of you who missed my Levelland post (or want to hear the song again), here goes, with the words below:]

 

Flatter than a tabletop
Makes you wonder why they stopped here
Wagon must have lost a wheel or they lacked ambition one
In the great migration west
Separated from the rest
Though they might have tried their best
They never caught the sun
So they sunk some roots down in this dirt
To keep from blowin’ off the earth
Built a town right here
And when the dust had all but cleared
They called it Levelland, the pride of man
Levelland.

Granddad grew dryland wheat
Stood on his own two feet
His mind got incomplete and they put in the home
Daddy’s cotton grows so high
Sucks the water table dry
As rolling sprinklers circle by
Bleedin’ it to the bone
And I won’t be here when it comes a day
It all dries up and blows away
I’d hang around just to see
But they never had much use for me in Levelland, Levelland
They don’t understand me out in Levelland, Levelland

And I watch those jet trails carving up that big blue sky
Coast to coasters – watch ’em go
And I never would blame ’em one damn bit
If they never looked down on this
Not much down here they’d wanna know
Just Levelland
Far as you can point your hand
Nothin’ but Levelland

Mama used to roll her hair
Back before the central air
We’d sit outside and watch the stars at night
She’d tell me to make a wish
I’d wish we both could fly
Don’t think she’s seen the sky
Since we got the satellite dish and
I can hear the marching band
Doin’ the best they can
They’re playing “Smoke on the Water”, “Joy to the World”
I’ve paid off all my debts
Got some change left over yet and I’m
Gettin’ on a whisper jet
I’m gonna fly as far as I can get from
Levelland, doin’ the best I can
Out in Levelland

Footnote:  In March this year, the NY Times magazine had an article entitled “25 Songs That Tell Us Where the Music is Going,” and yes, James McMurtry was one of the 25 featured artists.  The featured song is “Copper Canteen.”

 

Honey, don’t you be yelling at me when I’m cleaning my gun
I’ll wash the blood off the tailgate when deer season’s done
We got one more weekend to go
And I’d like to kill one more doe

So I’ll shovel the sidewalk again ’cause you’re still in a stew
I bet the bridge tender’s widow* won’t mind that I can’t please you
She’s sure got the run of the men
Out here where the pickin’s are thin and there’s not much to do

I woke up last night in the grip of a fright scared to breathe for I might make a noise
This life that we craved so little we saved between the grandparents graves and the grandchildren’s toys

We grew up hard and our children don’t know what that means
We turned into our parents before we were out of our teens
Through a series of Chevys and Fords
The occasional spin round the floor at the Copper Canteen

Now the big boxes out on the bypass are shaving us thin
I guess we’ll hold on a couple more years ’til the pension kicks in
Then we’ll sell all the stock in the store
Leave only the lock on the door
And wonder what then

When I wake up at night in the grip of a fright
And you hold me so tight to your chest
Then your breath on my skin still pulls me back in
‘Til I’m weightless and then I can rest

So if Monsignor should pull you aside as you’re leaving the church
And I’m out on the ice, dropping lines for the walleye and perch
Tell him it’s not your job to bring me to the fold
And I’d rather stand out in the cold

And honey I know that the woodpile’s low and you can’t close the flue
So I’ll split up a couple more cords ‘fore the winter time’s through
Hold on to your rosary beads
Leave me to my mischievous deeds like we always do

*The Bridge Tender is a 2014 novel by Marybeth Whalen as well as a 2012 novel by Gary Landry.  Both books involve a widow.  Hmmmm . . . I wonder what McMurtry is talking about?  Maybe it has nothing to do with either book, but maybe it does. . . .

I found a Slant Magazine review of the song (by Jeremy Winograd) that speculates on the bridge tender’s widow:

Complicated Game [album title] starts off with its most vivid vignette, “Copper Canteen.” The opening descending arpeggios set the album’s contemplative mood effectively, but it’s McMurtry’s couplets that do the heavy lifting. He employs a few small details to acquaint the listener with the setting: references to ice fishing for walleye and perch place the song clearly in the rural upper Midwest, “where the pickings are thin and there’s not much to do.” The song captures a boredom, even a dread, underlying the stillness and monotony of the characters’ lives. The narrator tells his wife to “hang onto your rosary beads and leave me to my mischievous deeds” (which may or may not include sleeping with “the bridge tender’s widow”).

Interesting that the NY Times reviewer said that after the election, she (Ruth Graham from Slate) was drawn back to this song – she doesn’t say, but maybe she sees it as a portrait of a voter both candidates wanted (and Trump got).

Well, it’s time for me to take a spin around my landing, checking out GE Pano shots.  I couldn’t find much, but I did find this striking sunset shot taken by John Drew a few miles west of my landing:

That’ll do it . . .

KS

Greg

 

© 2017 A Landing A Day

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Magasco, Texas

Posted by graywacke on June 13, 2017

First timer?  In this formerly once-a-day blog (and now pretty much a once-every-four-or-five days blog), I use an app that provides a random latitude and longitude that puts me somewhere in the continental United States (the lower 48).  I call this “landing.”

I keep track of the watersheds I land in, as well as the town or towns I land near.  I do some internet research to hopefully find something of interest about my landing location. 

To find out more about A Landing A Day (like who “Dan” is) please see “About Landing” above.  To check out some recent changes in how I do things, check out “About Landing (Revisited).”

Landing number 2350; A Landing A Day blog post number 781.

Dan:  Today’s lat/long (31o 16.086’N, 94o 4.587’W) puts me in SE Texas:

My local landing map shows a number of small towns close to the Sam Rayburn reservoir:

My streams-only map shows that I landed in the watershed of the Briar Branch:

As you can see, the Briar Branch’s more formal name is likely Briar Branch of the Ayish Bayou (2nd hit). 

However, upon zooming back a little further, I suppose it’s possible that the Briar was a branch of the Angelina River.  Regardless, this is the 5th hit for the Angelina, making it the 170th river on my list of rivers with 5 or more hits. 

But that damn reservoir (or I should say dam reservoir) covered up the evidence . . .

You can also see that the Angelina lost out to the Neches (11th hit) for naming rights after the two rivers combine.  See the Sabine off to the east?  Trust me on this – the Neches ends up as part of the Sabine watershed (21st hit).

It’s Google Earth (GE) free fall time!  Strap on your parachute, but don’t hit the ripcord until you’re close to landing (otherwise, the video will take way too long).  Click HERE for the experience.

As you can see, I landed in the woods, so there will be no bare-naked street view shots of my landing.  But there will be a look from here:

And here’s what the Orange Dude sees:

I instructed the OD to move west on the same road just a little ways to get a look at the Briar Branch:

And here’s what the he sees:

And JFTHOI, I told the OD to head south of Sam Rayburn reservoir on the Angelina until he could get a look.  Here’s what he saw:

It looks like a nice RV campground in the background . . .

Real quick quiz: Who’s Sam Rayburn?  I didn’t know any specifics, but his name was familiar to me as a politician, so I guessed a Texas politician.  From Wiki:

Samuel Taliaferro Rayburn (1882 – 1961) was an American politician who served as the 43rd Speaker of the United States House of Representatives from 1940 to 1947, 1949 to 1953, and 1955 to 1961, the longest-serving speaker in American history. He represented Texas’ 4th congressional district as a Democrat from 1913 to 1961.

So I was only 11 when he died, but I was already watching the Huntley-Brinkley report by that age (my family didn’t watch Walter Cronkite).

How about Sam’s cool middle name?  Taliaferro means “ironcutter” in Italian.

With 6 towns to choose from (based on my local landing map), I obviously just chose one. Of course, I checked them all out, and all (including Magasco) were totally:

Wait a minute (you might be saying) – you must have found a hook for Magasco!  Well, sort of . . .

All I could learn about Magasco, is that it is the only place in the entire world called Magasco!  Here’s a screen shot from GeoTarget.com:

If GeoTarget says it, it must be true!!!!

There is nothing else – nada, rien, zero – on the internet about Magasco TX (not including numerous automatically-generated sites like “Auto Glass Repair in Magasco TX.” There’s also a “Magasco Drive” in nearby Pineland and Magasco Lake – a 7-acre lake in (of all places) Magasco.

So.  Like I did, you should go to Google and search for “Magasco.”  Not Magasco TX, just Magasco.  And what do you see?  Page after page devoted to a Cameroonian pop star who goes by the name of (what else?) Magasco.

From Wiki:

Tohnain Anthony Nguo better known as Magasco aka “Bamenda Boy” is a Cameroonian Afro-pop/afro-beats artist, born in 1988 in Bamenda, Northwest Cameroon.

Although his music is not my style, I found myself really enjoying several of his videos.  Because I’m ignorant of modern music genres, I won’t even attempt to classify his music. 

I’ll start with his Kumba Market song (Kumba is a city in Cameroon)

 

I took a GE trip to Kumba and started checking out Panoramio shots.  And lo and behold, I found one of the Kumba Market (by Ronio):

Here’s another Magasco video (with “Pit Baccardi”), entitled “One by One.”  Magasco sings in English (the “one by one” part), while Pit Baccardi raps in French.  There are a lot of cool shots of kids in this (although there are some PG-13 dance scenes towards the end of the video).  By the way, English and French are both official languages in Cameroon.

 

I wasn’t paying attention to You Tube after watching a Magasco video when I realized a video from another Cameroonian artist, “Mr. Leo” was playing.

This appears to be a love song to a pregnant sweetheart – in French, entitled “On Va Gerer” (we will manage):

 

If you like the music, there’s plenty more where that came from.  And watch out about “Love It” by Magasco — it goes a little beyond PG-13.  But don’t worry, everybody keeps their clothes on, and it’s just dancing . . .

So, I thought I’d check out Cameroon, at least a little.

From Wiki, some early Colonial history:

Portuguese sailors reached the coast in 1472. They noted an abundance of shrimp in the Wouri River and named it Rio dos Camarões (Shrimp River), which became Cameroon in English.  Over the following few centuries, European interests regularized trade with the coastal peoples, and Christian missionaries pushed inland.

In 1884, the territory was colonized by Germany as Kamerun.  With the defeat of Germany in WW I, the territory was split into British Cameroon and French Cameroon.

Independence was gained in 1960, and the French & English colonies were united.

Strangely, the Wiki article never mentions slavery.  I thought that the west coast of equatorial Africa was the nexus of the slave trade. 

So, I did a little research, and found this from History.com:

Though exact totals will never be known, the transatlantic slave trade is believed to have forcibly displaced some 12.5 million Africans between the 17th and 19th centuries; some 10.6 million survived the infamous Middle Passage across the Atlantic.

[Oh my.  About 2 million Africans didn’t survive the journey.]

Though descendants of these enslaved Africans now make up considerable segments of the population in the United States, Brazil and many Caribbean islands, written records of their ancestors’ origins are difficult—if not impossible—to find. Through extensive research, however, scholars have been able to make educated guesses about where many of the slaves brought to the New World originated.

It should be noted that slaves brought to the United States represented only about 3.6 percent of the total number of Africans transported to the New World, or around 388,000 people—considerably less than the number transported to colonies in the Caribbean (including more than 1.2 million to Jamaica alone) or to Brazil (4.8 million).

Here’s a graphic from SlaveVoyages.org (note that the Cameroon coast is on the Bight of Biafra Bight, confirming that Cameroon was indeed part of the slave trade):

And check out a mesmerizing interactive map graphic (from History.com) that shows the slave trade year by year.  Click HERE.

One other bit about Cameroon.  There’s a large volcanic mountain right on the coast, Mt. Cameroon.  Mt. Cameroon is an active volcano that last erupted in 2012.

Here’ a shot of the mountain from TheCultureTrip.com:

Wiki notes that Cameroon’s Lake Nyos is part of the same volcanically active area (known as the Cameroon Line), and that the lake was the site of a disaster in 1986.

I made a little Google Earth video that shows Mt. Cameroon (I circled it with the cursor) and the volcanic Cameroon Line (highlighted by the cursor), leading towards Lake Nyos).  I then zoomed in to get a look at the lake. Click HERE for the quick trip.

From Wiki, about the disaster:

Lake Nyos [a little less than a square mile in area] is a deep crater lake in Cameroon, located on the flank of an inactive volcano. A volcanic dam impounds the lake waters.

A pocket of magma lies beneath the lake and leaks carbon dioxide (CO2) into the water, changing it into carbonic acid.

In 1986, possibly as the result of a landslide, Lake Nyos suddenly emitted a huge cloud of CO2 (estimated to be nearly a third of a cubic mile) which suffocated 1,746 people and 3,500 livestock in nearby towns and villages. The cloud was heavier than the surrounding air, so hugged the ground and flowed down two valleys leading away from the lake.

Nyos is one of only three known exploding lakes to be saturated with carbon dioxide in this way, the others being Lake Monoun, also in Cameroon, and Lake Kivu in Democratic Republic of Congo.

Though not completely unprecedented, it was the first known large-scale asphyxiation caused by a natural event.

To prevent a recurrence, a degassing tube that siphons water from the bottom layers of water to the top allowing the carbon dioxide to leak in safe quantities was installed in 2001, and two additional tubes were installed in 2011.

Today, the lake also poses a threat because its natural volcanic dam is weakening. A geological tremor could cause this natural levée to give way, allowing water to rush into downstream villages all the way into Nigeria and allowing large amounts of carbon dioxide to escape.

Here’s a shot of the volcanic dam that holds back the lake (Pano shot by Ledeclau):

It looks tenuous, eh?

Let’s head back to good ol’ Texas, and finish off with a quick sunrise shot Pano on Lake Rayburn by Rob Keith:

That’ll do it . . .

KS

Greg

 

© 2017 A Landing A Day

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