A Landing a Day

Just another WordPress.com weblog

Posts Tagged ‘Bitterroot River’

The Bitterroot Mountains, Idaho

Posted by graywacke on February 2, 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 2323; A Landing A Day blog post number 754.

boxDan:  Today’s lat/long (46o 59.713’N, 115o 5.323’W) puts me right on the ID/MT border, but evidently in ID based on the title of this post:

landing-1

My local landing confirms my Idaho landing, and also validates the fact that no towns made it this post’s title:

landing-2

See?  Huge (pronounced yuge) area – no towns! 

Here’s my local streams-only watershed map:

landing-3a

You can see that I landed in the watershed of Graves Creek, on to the North Fork of the Clearwater River (2nd hit).  Zooming quite a ways back:

landing-3b

The N Fk discharges (of course) to the plain ol’ Clearwater (7th hit), and on to the Snake (80th hit).  Not shown (but you can trust me on this), the Snake makes its way to the Columbia (166th hit).

It’s time to strap yourself in, and climb on board the Google Earth (GE) yellow push-pin spacecraft for a short (but scintillating) trip in to Idaho from the outer fringes of the atmosphere.  Click HERE to partake.

Here’s an oblique shot of my landing, looking up Graves Creek towards the summit of the Bitterroots:

ge1

Given the boonie-esque nature of this landing, you might expect that there’s no decent Street View coverage of my landing.  You’d be correct in that expectation.

You might also suspect that I have to go quite some distance to get a look at one of my watershed streams.  You’d be correct there, as well:

ge-sv-n-fk-clearwater-map

Although I have no bridge upon which to place the Orange Dude, he does get a good look at the North Fork of the Clearwater River from the adjacent roadway:

ge-sv-n-fk-clearwater

Since I landed in an area forsaken by civilization, I felt compelled to feature the landscape, not a town for this post (especially after looking at a number of small towns between 35 and 50 miles distant, all hookless).

So – I landed in the Bitterroot Mountains, generally defined as the range that marks the boundary between the Idaho Panhandle and Montana.  The ridge of the Bitterroots, while marking the state border, does not mark the Continental Divide; rather it’s the distinctly-less-glamourous watershed boundary between the Snake to the west and the Clark Fork to the east.  Both, by the way, end up in the Columbia.

While typing the word Bitterroot, I realized that if it weren’t for that pesky “e,” Bitterroot could join “bookkeeper” in that most unique of letter groupings – three double letters in a row in a single word.

Anyway, being a geologist, I thought I’d do a little Bitterroot geology.  I found a short and succinct geologic summary from Cliff’s blogspot blog, “Somewhere in the Middle of (Western) Montana.”  Here are some of his words (slightly edited by yours truly):

About 100 million years ago, the west coast of North America ran through western Idaho. The North American plate was moving west (as it still is today), colliding with the plate holding the floor of the Pacific Ocean (as it still is today).

This causes the heavier Pacific plate to sink under the North American plate, creating a subduction zone. The compression crinkled (not a geologic term) and thickened/elevated the western edge of the North American plate.  It also drove the oceanic plate down into the hot mantle, where the granite melted and created a large mass of magma.

The magma rose into the existing rock near the Earth’s surface and formed the Idaho batholith, a huge mass of granite that covers about 10,000 square miles in central Idaho and includes the southern half of the Bitterroot Mountains.

So here’s my take. The subduction going on off the west coast today creates hot magma that rises up, creating the volcanoes of the Sierra Nevada.  Back 100 million years ago, when the coast was about where western Idaho is today, the hot magma didn’t rise all the way to surface; instead, it created a huge subsurface magma pool that migrated upward, cooled very slowly and created the Idaho granite batholith. 

Here’s a cross section (from Idaho State University):

subduction

“Plutons” are simply huge blobs of magma (rather than a single mass).  The “Moho” is the Mohorovicic Discontinuity, otherwise known as the boundary between the solid crustal rocks and the more plastic rocks of the mantle.

And a more local cross section from Carnegie Melon University:

x-section-carnegie-museum

Back to Cliff:

With so many forces at work, the Earth’s surface is thought to have bulged and heaved, becoming higher in elevation (mountain building) but also unstable. In southwestern Montana, a large piece of the Idaho batholith broke off and moved east, forming the Sapphire Mountains. The gap created between the Idaho batholith (i.e., the Bitterroot Mountains) and the Sapphire Mountains is the Bitterroot Valley.

The Bitterroot River (3 hits!) flows northward in this valley and discharges to the Clark Fork.

And then, the most recent glacial epoch (which ended about 15,000 years ago), resulted in glacial sculpting of the landscape.  By perusing GE, I could see that the Bitterroots were obviously so sculpted (but then again, I am a geologist). 

Here’s what I would consider an obvious glacially-carved area (the Oregon Lakes, less than 4 miles to the northwest):

ge-oregon-lakes

Here’s an academic figure (from slideshare.net), showing mountain glacial features.

geo-1-glacial-environments-20-638

I’ll return to the Oregon Lakes, with many of those same features labeled:

ge-oregon-lakes-2

By the way:  “Pater noster lakes?”  Say what?  From Wiki:

A paternoster lake is one of a series of glacial lakes connected by a single stream. The name comes from the word Paternoster, another name for the Lord’s Prayer derived from the Latin words for the prayer’s opening words, “Our Father.”

Paternoster lakes are so called because of their resemblance to rosary beads, with prayer beads connected by a string or fine chain.

So the Bitterroots, eh?  From whence cometh the name?  From Wiki:

The Bitterroot Mountains are named after the bitterroot, a small white/pink flower that is the state flower of Montana.

Here are the white variety (from Wiki, by Walter Siegmund) and the pink variety (from AuntieDogmasGardenSpot):

lewisia_rediviva_lg1024px-lewisia_rediviva_9789

Back to Wiki:

The bitterroot (Lewisia rediviva) is a low-growing perennial plant with a fleshy taproot.  The flower stems are leafless, with a single flower on each stem.

French trappers knew the plant as racine amère (bitter root).  Native American names included spetlum or spetlem, meaning “bitter.”

The roots were consumed by tribes such as the Shoshone and the Flathead Indians as an infrequent delicacy. The Lemhi Shoshone believed the small red core found in the upper taproot had special powers, notably being able to stop a bear attack.

[I could see how it could happen that someone ate some bitterroot, and apparently miraculously was spared a bear attack.  But I have trouble imagining the special powers legend continuing any length of time.  But hey – what do I know?]

The bitterroot was selected as the Montana state flower on February 27, 1895.

Three major geographic features, the Bitterroot Mountains (running north-south and forming the divide between Idaho and Montana), the Bitterroot Valley, and the Bitterroot River (which flows south-north, terminating in the Clark Fork river in the city of Missoula), owe the origins of their names to this flower.

Here’s some more, from the St. Mary’s Mission & Museum:

Lewis and Clark are credited with the “discovery” of the bitterroot plant (Lewisia Rediviva) in the Montana valley which was eventually named after it. It was an important part of the Native American diet for unknown generations. Tribes’ spring migrations were timed to coincide with the blooming of the bitterroot flower and often scouts would be sent out to alert the tribe to the readiness of the plant for harvesting.

Indian women dug, cleaned and boiled the root of the plant and then mixed it with meat or berries. Hunting expeditions and war parties often carried patties made from a mixture of pulverized root, deer fat and moss. At trading centers a sackful of bitterroot commanded a high price and could often be traded for a horse.

The species name rediviva refers to the hardiness of the plant.  A bitterroot can live for over a year without water and is usually found growing in gravelly, dry soil.  It is low-growing perennial with a fleshy taproot and has a branched base. In May and June a single flower will appear on each stem ranging in color from white to a deep pink or rose.

I did a quick search to see if there are medicinal uses for bitterroot, and was not surprised to find the following (from NaturalMedicinalHerbs.net):

Medicinal use of Bitter-Root: The root is cardiac (promotes heart health) and galactogogue (promotes lactation). An infusion of the root has been used to increase the milk flow in nursing mothers, to relieve heart pain and the pain of pleurisy and also as a blood purifier. The root has been eaten raw to counteract the effects of poison ivy rash and as a treatment for diabetes. The pounded dry root has been chewed in the treatment of sore throats. A poultice of the raw roots has been applied to sores.

Likely, not all true; likely, not all false . . .

Time for some GE Pano shots, all within about 7 miles of my landing.  First this, of Upper Oregon Lake (a tarn), by Blackbear91:

pano-blackbear91

And this, by DHOlano:

pano-dholano

Also, by DHO:

pano-dholano2

A lovely meadow by Glacierman:

pano-glacierman

And mountain goats by Raymond Gardner:

pano-raymond-gardner

And I’ll close with this award-winner, also by Mr. Gardner:

pano-raymond-gardner2

 That’ll do it . . .

KS

Greg

 

© 2017 A Landing A Day

 

 

Advertisements

Posted in Uncategorized | Tagged: , , , , , | Leave a Comment »

Missoula, Montana

Posted by graywacke on March 11, 2013

First timer?  In this formerly once-a-day blog (and now pretty much a once-every-time-I-get-around-to-it blog), I have my computer select 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 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 and what the various numbers and abbreviations mean in the first paragraph), please see “About Landing,” (and “Abbreviations” and “Cryptic Numbers”) above.

 Dan –  After three USers in a row; of course, I follow up with three OSers in a row, thanks to this landing in the granddady of OSers . . . MT; 117/96; 4/10; 1; 155.3.   Here’s my regional landing map, showing that I didn’t land far from that long-time USer Idaho:

 miss - landing1

My closer-in landing map shows that I landed within easy commuting distance of Missoula:

 miss - landing2

You can see that I landed along a road that runs east-west in what looks like the boonies.  
Here’s an even-closer-in landing map, which shows that I landed right along O’Brien Creek and O’Brien Creek Road:

miss - landing3

O’Brien Creek flows east towards the tangle of rivers that you can see in the greater Missoula area.  Specifically, the creek flows into the river that comes up from the south – and curls around Route 12 – the Bitterroot R (3rd hit).  The Bitterroot flows just a little over a mile after accepting the waters of the O’Brien when it flows into Clark Fork (17th hit, the river that flows right through Missoula); on to the Pend Oreille (19th hit); to the grand ol’ Columbia (139th hit).

 Here’s my Google Earth (GE) shot that shows what the O’Brien Creek valley looks like:

 miss - GE1

I decided to zoom in at a low elevation (using GE, of course), looking west up the valley past my landing:

 miss - GE2

Stepping back some (er, I should say flying back some), here’s a GE view over the Missoula Valley (with a little of the city in the foreground), still looking west past my landing:

 miss - GE3

I was surprised and happy to see that GE StreetView coverage extends up O’Brien Creek road.  It doesn’t make it all the up to my landing, but it comes close.  Here’s a shot looking up the valley.  My landing is about 1.5 miles ahead.

 miss - GE4 obrien creek road .5 mi from landing

Here’s a Panoramio shot by J. Belote, taken from the top of the mountain about 1.5 miles due south of where I landed, looking east towards Missoula:

 miss pano towards missoula from 1.5 mi s of landing by j. belote

Checking into the history of Missoula, I found out that the area was originally known as Hell Gate.  Catchy name, eh?  From Wiki:

Hell Gate (sometimes known as Hell’s Gate or Hellgate) is a ghost town at the western end of the Missoula Valley.  The town was located on the banks of the Clark Fork River roughly five miles downstream from present-day Missoula near what is today Frenchtown.

Members of the Bitterroot Salish (or Flathead) Native American tribe often traveled through the Missoula Valley on their way east to bison hunting grounds.  As the Salish passed through the valley’s narrow eastern and western mouths, members of the Blackfeet tribe would often attack and kill them.  The Salish called the valley lm-i-sul-étiku, which means “by the cold, chilling waters” but which the Salish used metaphorically to mean “the place chilled with fear.”  The entire valley was heavily wooded, and ideal for ambush.

French trappers passing through the valley in the 1820s were horrified to see so many remains of Salish in the deep canyons which formed the valley’s entrances, and called the valley “Porte de l’Enfer,” or the “Hell Gate.”

Hell Gate collapsed as a settlement in 1865. The settlement had reached a grand total of 20 residents.  But a sawmill, flour mill, and new store were built at the site of present-day Missoula, and all the residents of Hell Gate moved to the new town practically overnight.

Rather than take the town name with them, they adopted as the new name of their town the (garbled) Indian word for the valley, “Missoula.” The county seat was moved from Hell Gate to Missoula in 1866.  By 1913, little was left of the town (which was now part of a privately owned ranch) except for a few buildings.

Hell Gate has lent its name to several natural and man-made features in the area, including the valley itself, which became known in the 1800s as the Hell Gate Valley.   Hell Gate was also the original name of the Clark Fork River.

Although the river and valley would be renamed, the steep gorge cut by the Clark Fork to the east of the Missoula Valley is still known as Hellgate Canyon.  The U.S. Postal Service maintains a Hell Gate Station in downtown Missoula, and the Missoula County Public School System operates Hellgate High School, one of the oldest and largest high schools in the state of Montana.

There you have it.  By the way, Hellgate is such a cool name for a high school.  Let me guess, they are either the “Red Devils” or the “Blue Devils.”  I’ll go check in with Google . . .

Doh!  This is one of those rare occasions that my hunch was wrong.  They are the Hellgate Knights:

 Missoula-Hellgate-Knights-2

FYI, I went to Zanesville High School in Ohio.  We are the Blue Devils, and this is our logo (although this wasn’t our logo the many eons ago that I went there):

 miss - ZHS logo

By the way, ZHS  went 19-5 in boy’s basketball this year, suffering a tough loss in the second round of the state tournament.  Not a bad season when the two tallest kids on the team are both only 6′ 3″ . . .

Ahem.  Sorry about the diversion.  Moving right along – Missoula is the home of the University of Montana.  Perusing GE, I could easily find the big “M” on the mountainside that overlooks the campus:

miss - M over Univ of mt

As a geologist, I’ve been itching to get on to the next topic:  References to the Missoula Valley are replete with discussions of  “Glacial Lake Missoula.”  I know, I know, it wasn’t so long ago that I gave a robust geological treatment to Glacial Lake Wisconsin (my Mauston WI post).  But I couldn’t look myself in the eye (in the mirror) if I didn’t include some discussion about Glacial Lake Missoula, because it’s so cool.  I can hardly think of a geological story more compelling . . .

Here’s the nuts & bolts (from ForMontana.net, starting with this picture of relic shorelines):

miss don hyndman, u of mt

One of the most fascinating events of the last ice age was a series of cataclysmic floods associated with Glacial Lake Missoula. The shorelines of the ancient lake can be seen along mountainsides around Missoula. In the photo shown above, the light snow on Mt. Jumbo makes it easier to see these ancient shorelines.  At times the lake was 950 feet deep where Missoula sits today.

Here’s what happened . . .
As the glacial ice moved south and reached its maximum about 18,000 years ago, it extended into western Montana and Idaho and it blocked the flow of the Clark Fork River.  The water began to build up behind (south of) the ice dam. This formed a huge lake that geologists have named “Glacial Lake Missoula.”

When the Lake Missoula was at its highest, the water was about 2,000 feet deep and contained about as much water as Lake Erie.  Once the water filled in the area behind the ice dam, the lake didn’t last for long.  Since ice floats, it doesn’t make for a very durable dam. Consequently,  it was only a matter of time before the lake dislodged its ice dam. With the dam displaced, the 480 cubic miles of water impounded behind it would have been unleashed in a cataclysmic flash flood of incredible proportions.  The water would have thundered through present-day Spokane and continued across eastern Washington to the Columbia River, scouring the land as it swept through.

Geologists think that this happened many times. Once the front of the glacier was swept away by the water it had impounded, the lobe of ice grew back into the area and re-dammed the river. Geologists believe that at Lake Missoula formed and flooded at least 41 times between 15,500 and 13,200 years ago.

Below: On this map of Montana, Glacial Lake Missoula is the lake in the far west.  It wasn’t the only glacial lake – several others existed along the southern edge of the ice.

glakesmontana

As one might expect, these cataclysmic floods left their mark.  But it took quite a bit of sleuthing and piecing together many clues to put the whole story together.  A geologist named Harlen Bretz was the first to have a clue.  This, from Wiki:

J Harlen Bretz (1882 – 1981) was an American geologist, best known for his research that led to the acceptance of the Missoula Floods.

In the summer of 1922, and for the next seven years, Bretz conducted field research of the Columbia River Plateau.  He was interested in unusual erosion features, where massive erosion had cut through basalt deposits (the Channeled Scablands).  The area was a desert, but Bretz’s theories required cataclysmic water flows to form the landscape.

Bretz published a paper in 1923, arguing that the erosion features were caused by massive flooding (that he termed the Spokane Floods) in the distant past.

Bretz encountered resistance to his theories from the geology establishment of the day.  The geology establishment was resistant to such a sweeping theory for the origin of a broad landscape for a variety of reasons, including the lack of status and reputation of Bretz in the eyes of the largely Ivy League-based geology elites.

Bretz defended his theories (along with another geologist, J.T. Pardee, who focused on evidence for Glacial Lake Missoula), kicking off an acrimonious 40 year debate over the origin of the Channeled Scablands. As he wrote in 1928, “Ideas without precedent are generally looked upon with disfavour and men are shocked if their conceptions of an orderly world are challenged.”

Pardee’s and Bretz’s theories were accepted only after decades of painstaking work and fierce scientific debate.   In 1979 Bretz received the highest medal of the Geological Society of America, the Penrose Medal, to recognize that he had developed one of the great ideas in the earth sciences.

I found a great website that is all about the huge floods.  It is called (appropriately enough) HugeFloods.com.  Click HERE to go to it.  I strongly recommend that you do.  When you’re at the site, click on the following tabs, and peruse:

The Mystery

Lake Missoula

The Scablands (includes a cool BBC video)

Lake Lewis –  Wait until you read about Lake Lewis!

If you think that this whole colossal flood thing is worth learning more about, may I recommend this book:

miss book

My friend Cheryl showed me the book.  She has a new-found passion for geology, in spite of an artsy life that included designing and producing her own line of clothing.  She spent some time out west checking out the evidence for the big flood and knows way more about this than I do . . .  

Phew.  Heading’ on back to Missoula . . . you may have noticed that the picture of the relic shorelines is on “Mount Jumbo.”  Of course, I was curious as to how it go its name.  Well, this from Wiki:

Mount Jumbo (Salish: ‘Sin Min Koos,’ which translates into ‘obstacle’ or ‘thing in the way’)  is an iconic mountain that overlooks the city of Missoula, Montana.  Early settlers thought Mount Jumbo looked like a sleeping elephant and the round grassy mountain became known as Elephant Hill.

Coincidently, miners christened a nearby copper mine ‘Jumbo Lode’ in honor of Jumbo the elephant, famously with the Barnum and Bailey circus.  Eventually, “Elephant Hill” became “Mount Jumbo.”

Here’s a lovely shot of Mount Jumbo at sunset (from Wiki):

miss mt jumbo  wiki

I thought I’d do a little research on Jumbo himself (the elephant).  From Wiki:

Jumbo was born in 1861 in the French Sudan, whence he was imported to France and kept in the old zoo Jardin des Plantes in Paris. In 1865 he was transferred to the London Zoo, where he became famous for giving rides to visitors, especially children. The London zookeeper association leader Anoshan Anathajeyasri gave Jumbo his name; it is likely a variation of one of two Swahili words: jambo, which means “hello” or jumbe, which means “chief”.

Jumbo was sold in 1881 to P. T. Barnum, owner of the Barnum & Bailey Circus,for 10,000 dollars ($241 thousand today).  In New York, Barnum exhibited the elephant at Madison Square Garden, earning enough from the enormous crowds to recoup the money he spent to buy the animal.  Jumbo became a major attraction in the traveling “Greatest Show on Earth.”

Jumbo died in 1885 at a railway yard in St. Thomas, Ontario, Canada, where he was hit and fatally wounded by a locomotive. Barnum afterwards told the story that Jumbo died saving a young circus elephant, Tom Thumb, from being hit by the locomotive, but other witnesses did not support this.

Here’s a picture, from Wiki, of the sad occurrence:

miss jumbo death wiki

Jumbo’s hide was stuffed, and I’ll borrow from the Tufts University webpage for the following information:

Tufts’ official mascot, Jumbo the elephant, has been ranked among the most singular in college athletics by The Sporting News and Sports Illustrated and is the only college mascot found in Webster’s Dictionary.

The elephant’s tale dates back to 1885, when P.T. Barnum, the circus showman who was an early trustee and benefactor of Tufts, donated the stuffed hide of Jumbo to the university after he was killed by a train in Ontario, Canada. The pachyderm was eventually put on display in the Barnum Museum of Natural History (now Barnum Hall) at Tufts. He was a big hit with the college’s athletes, who adopted him as their mascot, while their coaches invoked his strength and bravery in pre-game pep talks.

For 86 years, Jumbo was a veritable mecca for students, their parents and other campus visitors. Students would pop pennies in his trunk or give a tug on his tail to bring luck for an upcoming exam or athletics competition. But Jumbo mania came to a fiery end on April 14, 1975, when Barnum Hall, and the beloved elephant, were consumed in a blaze caused by faulty wiring in a refrigeration unit. All that remained were a piece of his tail (now neatly wrapped and stored in the university archives) and some ashes. Phyllis Byrne, the administrative assistant in the athletics department, dispatched a colleague to the ruins to collect some of Jumbo’s ashes in an empty peanut butter jar.

Jumbo’s spirit lives on in his hybrid container (a Peter Pan Crunchy lid on a Skippy jar), and since 1975, university athletes have rubbed the jar for good luck. And when a new athletics director is named, there is a ceremonial “passing of the ashes” to the successor.

If you started to skim, make sure that you read the last paragraph.  Anyway, back to Wiki: 

In time the elephant’s name came to be a household word, with “jumbo” meaning “very large”.

[How about that!  The word “jumbo” came from the elephant’s name!]

A life-size statue of the elephant was erected in 1985 in St. Thomas to commemorate the centennial of the elephant’s death:

miss jumbo statue

Railway City Brewing Company in St. Thomas, Ontario, Canada brews “Dead Elephant Ale,” an IPA, in recognition of Jumbo’s connection to St. Thomas’s railway history.

I’ll close with a couple of great Panaoramio shots, taken along the Bitterroot River just east of my landing.  First, this one by John Krempel:

 miss mt sentinel john krempel pano landing to left

And this, by J. Edmonds:

miss pano j edmonds bitterroot just upstream

Phew.  Long post, eh?  This may well be my longest-ever . . .

That’ll do it.

KS

Greg

 

© 2013 A Landing A Day

Posted in Uncategorized | Tagged: , , , , , , , , , , , , , , | 2 Comments »