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The Gates of the Rocky Mountains

Captain Lewis wrote on July 19, 1805, ” … this evening we entered much the most remarkable clifts that we have yet seen. these clifts rise from the waters edge on either side perpendicularly to the height of 1200 feet. … the river appears to have forced its way through this immense body of solid rock for the distance of 5-3/4 Miles … I called it the gates of the rocky mountains.

Of all of the natural spectacles that Montana might have to offer, I think that the Gates of the Mountains on the Missouri River is probably one of the best. Captain Lewis wasn’t kidding when he described the canyon in his journal — It looks as if the river just “forced” it’s way through the rock.

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The boat tours through the gates have been going on for years. There have been millions of people since the times of Captain Lewis that have gazed up at the “most remarkable clifts“, and I’m pretty sure that over the future course of time there will be even millions more that will experience the Gates of the Rocky Mountains.

Gates of the Rocky Mountains rocky outcrops
Gates of the Rocky Mountains rocky outcrops

The day we experienced the gates was not too hot and not too cold. There was a slight breeze over the calm water and the clouds above just came and went at their leisure. There were plenty of boaters and folks fishing and camping along the way.

One of the things I was most interested in was the rock formations. I’ve always been interested in how Montana was made geologically, so I paid extra attention to how the river might have been able to make it’s way through the mountains. When I looked at the sharp rock cliffs, and of how the rock appeared to be folded in various places, I came away with the notion that the mountains might have given way to the river. I didn’t see the tell-tale cutting pattern of direct erosion like I saw on the Colorado River in the Grand Canyon. It appeared to me that some certain geological forces might have opened up a way for the river to pass through without the river having to put up much of an effort.

Gates of the Rocky Mountains cliffs
Gates of the Rocky Mountains cliffs

Captain Lewis had mentioned the “many springs” that were present coming out of the rock (I’m guessing at the water level he was at before the Holter dam was built) as he passed through and to me that might suggest that as the continent was moving westward, water was trapped in the area that might have undermined the base of the mountains in this particular area and caused a weak spot that opened up a way for the river to pass through without having to start the erosion at the surface like the Colorado River had done.

When I hear of the underground Madison River in the area of Great Falls, it’s not that much more of a leap to consider just how much water might be trapped all along the eastern side of the Continental Divide as a result of the North American tectonic plate movement ever grinding toward the west.

Gates of the Rocky Mountains sheer cliff
Gates of the Rocky Mountains sheer cliff

The boat tour through the gates was two hours well spent as far as I’m concerned. I didn’t get to see any Bears or Big Horn Sheep, but I did happen to see the Eagles and the Peregrine Falcons aloft. The canyon cliffs were the headliner however, with the wildlife being the added bonus … at least for me.

The only thing I might regret about our most recent tour of the gates, was the the fact that I didn’t bring the right camera. I’m thinking that next time I’ll bring the same camera that I used at the Petrified Forest National Park and at the Grand Canyon. The Gates of the Rocky Mountains deserve to have great photos taken of it because it’s imposing beauty is very difficult to put into words.

Schedule your own tour

For over 125 years guests have been following in the path of Lewis and Clark exploring the “Gates of the Mountains”. Today the marina and boat tour is operated by the Gates of the Mountains Inc, whose goal is to protect, educate, and allow visitors to explore one of the last best places.

Contacting the Gates

Phone: (406) 458-5241
Email: info@gatesofthemountains.com
Office: 9:00 AM – 5:00 PM

Welcome to Marysville, Montana

Welcome to Marysville, Montana

During one of our many road trips we recently had the opportunity to pay a visit to Marysville, Montana.

Marysville, primarily billed as a ghost town in the state, surprisingly has quite a number of people living there.

Though there are more occupied buildings than there are abandoned ones, the small town still boasts a few relics from the 1890’s that are in various stages of disrepair and decay.

Some of the old buildings have been or are in the process of being repurposed for modern use, like the old train station for instance, that houses the Marysville House Historic Restaurant. At very first glance, one might be hard pressed to imagine the building ever being a train station.

Many of the old buildings that once existed that are pictured across the internet on places like Pinterest and in articles about Montana ghost towns are gone — given way to grassy blank spots where they once stood.

1895 - Storefront - Marysville, Montana
1895 – Storefront – Marysville, Montana

Though I’m not a photographer by any stretch, I did manage to grab a few shots of some of what buildings were still there from the once bustling gold mining days of Marysville.

Our drive over to Marysville was sort of a bonus because we had a 3 hour gap in our schedule between Gates of the Mountains and an Astronomy lecture over at Canyon Ferry. During our late lunch at the Grub Stake Restaurant we decided to visit Marysville which was just a few miles or so up Lincoln Road. If you’re in the area and have a few hours to kill, I’d recommend driving over to Marysville for a look.

1895 - 2023 - Old commercial district building - Marysville, Montana
1895 – 2023 – Old commercial district building – Marysville, Montana

It’s somewhat unfortunate that these old buildings are crumbling away like they are. I’m guessing that the march of time is pretty much outpacing the availability of much needed talent and money. Soon I think, what’s left of some of these relics from the 1890’s are going to have to be totally demolished on account of the safety risk they pose. Some of these buildings are so far gone that no amount of money could probably ever save them.

Another interesting thing that I’ve discovered while visiting Marysville is that this old car never goes away.

Old car posing for a picture
Old car posing for a picture

Looking at other Marysville photos on the internet shows this car in different locations, in front of or beside other buildings. It’s almost as if this is the only car left in town from a known bygone era and it’s placed as if it might be posing exclusively for the tourists that happen to roll through. Another thing I might have to consider here is that this car lost it’s garage to the wiles of time and is forever orphaned — subjected to a never ending search for a new garage that it can call home.

The history of Marysville somewhat parallels the history of many other small gold mining towns in the state. Every town has a similar but no less colorful story of how someone came into the gulch, gully, canyon, or flat, and struck it rich with their own lode.

Marysville, Montana
Marysville, Montana

Stories of how Martha Jane Canary was literally everywhere back in the day, including Marysville, Montana. Some Scotsman, Norwegian, or Irishman came to Montana and set about to make history, most times not even realizing it — We do well to revisit that history as often as we can, because if we don’t, our history, not too unlike some of the old buildings in Marysville, will fade away into oblivion.

Thomas Cruse was no exception, as far as stories go.
In 1876 he discovered the vein and named it after his native town of Drumlummon, Ireland.
He named the town after Mary Ralston, the first woman to arrive.
During the 1880’s and 90’s, Marysville was Montana’s leading gold producer and had a population of 3,000 people.

Our Son loved Marysville — We tell the stories and show the places to our kids just like our parents did for us, and theirs before them. Montana history won’t ever die as long as we choose to keep it alive.

Sounds of the ’70’s

I never really ever got into Rock music much in the 1970’s.

I guess the ’60’s were so tumultuous and busy that everybody just decided to take the ’70’s off. I kind of liked the laid back take it easy sort of thing back in the day.

When I look back at the ’70’s, what with all of the plaid pants, bell bottoms, Puka shells, fly-away shirt collars, black light posters, and turtle neck sweaters that no one could ever quite get their head into or out of, I’ll have to say that the ’70’s music pretty much got through the decade none the worse for the wear.

Below is a small playlist of some of the stuff I liked to listen to back then.

Otters, Beavers, and other things that might go Bump in the woods

I was looking at a story recently in the news about how a small group of people were accosted by a small group of Otters on a float trip down the Jefferson River.

It’s an unfortunate incident that may or may not have been avoidable given the conditions of the day on the river and the proximity of the territory of the Otters themselves. Either way it appears, these animals saw what they deemed was a potential threat to their area and responded how wild animals might often do … with aggression.

Animals like Otters, Beavers, Snakes, Deer, and even Elk aren’t real known for their aggressive tendencies. We usually don’t hear of the aggression until the warning signs are ignored.

Every one of these animals have a set of warning signs that are designed to let you know that they are there. A rattle snake for instance, doesn’t rattle his tail to tell all of his buddies that you are there — he rattles his tail to let “you” know that “he” is there. Beavers are much the same as that. A sharp slap on the water with his tail might do well to give you a clue as to his presence.

Most of these animals would prefer to not have a confrontation, but if the boundaries are pushed far enough, they are more than ready to meet the challenge at hand in order to restore their own perceived notions of personal space, safety, and peace.

My encounter with a Beaver one year when I was young up the West Fork of the Bitterroot at Pierce Creek taught me a thing or two. I ignored the warning signs and as a result, played hell getting out of there. Beavers, not too unlike any other form of our Montana wildlife, can be forces to be reckoned with if you ignore the warning signs.

I saw a video a month or so ago of a Bear stuck between two groups of people hiking a trail up at Glacier National Park and the Bear ultimately chose an alternate route down the mountain side in order to avoid having a run-in with either group. Though the Bear might not have preferred to take the route that he did, I’m pretty sure that he chose that route so that he might maintain his own personal space and peace.

Sometimes we wander off into an animals personal range and space without even realizing it and as a result we are confronted with the unexpected and seemingly out of the blue responses from the animals themselves. Situational awareness is pretty important if you’re in the woods or on the river because sometimes we might miss the warning signs.

These animals, in their own way, speak to us — The clicking, chirping, whistling, and rattling are all forms of communication they use for not only their own protection, but for our protection as well … we all might do well to be better focused and tuned in to what these animals might be trying to tell us.

Being aware of our surroundings can help greatly when we consider the Otters, Beavers, and other things that might go Bump in the woods.

Montana Fish, Wildlife and Parks posted a response with regard to this incident:

FWP advises recreationists to keep a wide distance, giving all wildlife plenty of space. In drought conditions, low water levels can bring recreationists closer to water-dwelling wildlife. Being aware and keeping your distance can help avoid dangerous encounters, reduce stress for wildlife, and promote healthy animal behavior. If you are attacked by an otter, fight back, get away and out of the water, and seek medical attention.

Read the entire press release here:

https://fwp.mt.gov/homepage/news/2023/aug/0803-3-women-injured-by-otter-on-jefferson-river

Thrust faults of the Rocky Mountain Front

Thrust faults of the Rocky Mountain Front — Living and working and playing on Montana’s Rocky Mountain Front is pretty epic when you stop to consider just exactly how wonderfully the entire area is built.

Geologists have spent a great deal of time over the years working out just how the Rocky Mountain Front came to be, from mapping the numerous fault zones to determining the types and kinds of strata involved with all of the uplift.

The Rocky Mountain Front is characterized by the fold-and-thrust belt system (see Geologic Map of Choteau Quadrangle; thrust faults are mapped with the ‘sawteeth’ on the upper block (hanging wall) of the thrust fault. Generally, the thrust faults run northwest-southeast and dip (point) to the southwest (propagating the formations towards the east-northeast).

Thrust faults often have a deep-seated sole thrust (a decollement), and as the upper plate is transported, a series of subsidiary thrust faults “ramp up” through the stratigraphic section. This creates an imbricate thrust zone. The thrust faults propagate through the system repeating the stratigraphic units as shortening continues. The youngest movement will occur along the front edge of the thrust system.

To get a better view of how the Rocky Mountain Front was and is being built even today you can view this animation created by Paul Karabinos, Department of Geosciences, Williams College below:

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This 3D block diagram was made using Trimble SketchUp.

2,395 earthquakes recorded in Montana during 2018
2,395 earthquakes recorded in Montana during 2018

Western Montana is riddled with a great number of faults as a result of this fold-and-thrust belt system.

2,000 to 3,000 Northern Rocky Mountain earthquakes happen in a typical year. Most of these earthquakes did not cause significant ground shaking but even still, the Northern Rocky Mountains are definitely still on-the-move.

Intermountain Seismic Belt and the Centennial Tectonic Belt
Intermountain Seismic Belt and the Centennial Tectonic Belt

 

Our Montana home is a seismically active state. Large historical earthquakes as well as modern frequent small and moderate-sized earthquakes demonstrate the very real possibility of future damaging earthquakes. Seismologists as of yet, still can’t predict the specific times, locations, and magnitudes of future earthquakes, but past experience says that future seismic activity is most likely to occur in regions where previous earthquakes were common.

In Montana, most—but not all—earthquakes occur in the western one-third of the state along two related zones named the Intermountain Seismic Belt and the Centennial Tectonic Belt.

The Rocky Mountain Front has a rugged beauty all it’s own — A rugged beauty that couldn’t exist if it weren’t for the tectonic forces involved.

Knowing the science behind the creation of our Rocky Mountain Front just makes it even more beautiful than it ever was before.

sourced:
Sarah Anne Devaney, Department of Earth Sciences, Montana State University
Paul Karabinos, Department of Geosciences, Williams College