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Missouri Buttes Snowy Squalls

Missouri Buttes Snowy Squalls
Missouri Buttes Snowy Squalls

Missouri Buttes Snowy Squalls (I see the Devil’s Tower’s outline on the left but it’s pretty far out in the snow to show up here lol. )

I’m a photorealist who preaches against “blue snow”. I maintain the practice of maintaining a blue snow free zone in my gallery, except when it was really blue. This was blue sky and hills distant but the snow was white.

So much of the deeply blue snow you see in forum photos is bad or excessive color enhancement or improper setting for white balance in that camera. It drives me crazy lolol. I’ve always argued that blue snow doesn’t exist in nature but for a few, very few mornings, early in twilight. This color is as I experienced it. Think about it, have you ever seen electric blue snow?

I do sunrises and sunsets almost every day photographically. This twilight was a rmisty one indeed. This is a view looking to the south east from near the Montana/Wyoming border. This is very far northeastern Wyoming.

Remember that those 4 hills are all related volcanic necks. Being made of hard rock, they stick up above the softer rock the volcanic neck melted through to the surface. Much sediment has been removed around this volcanic pipes now more than a 1000 feet in the air. They used to be miles deep. Everybody known about the Devils Tower but also part of the same “Volcanic neck” complex formed around the same time as the MIssouri Buttes. This is the Non tourist angle from the north east .. Devils tower had more time to cool slowly and the columns formed much better

Location: near the Bliss Dinosaur Ranch, Wyoming/Montana borderlands

Title: Missouri Buttes Snowy Squalls

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Missouri Buttes + Devil’s Tower

Missouri Buttes + Devil's Tower
Missouri Buttes + Devil's Tower

Missouri Buttes + Devil’s Tower

The Exposed Volcanic Necks in this image are all related in space and time. Once deeply buried volcanic conduits to the surface. Each of the 4 peaks stands eroded at the surface. These pipes carried magma to the surface as lava/ash in four volcanos popping off at the surface . The rock we see here froze solid in that neck and cooled. We know this was deep as the column of rock in the Devils Tower cooled very slowly allowing the columns of rock the National Monument is famous for. Being our nations first national Monument is the moniker that Devil’s Tower and surround area carry. Wyoming and all that

Being 40 miles away from the tow and the buttes somewhat closer, this becomes a terribly long shot to actually be able to resolve the columns on the tower. There is SOME columnar jointing in the Missouri Buttes. Emplaced closely in time and space does not say they were coterminous in their eruptions. . We don’t know their exact schedule.

Phenolitic Porphyry is the name of the rock. It cooled into big 6 foot in diameter crystals up the length of the tower. I used one of several possibilities all related to volcanic activity to describe the tower as volcanic necks. There are multiple configurations and possible variations in this discussion I won’t get into here but feel free to google devils tower origin to discover more.

Location: The Pass at Rockypoint Wyoming, Trail Creek Road, NE Campbell Country

Title: Missouri Buttes + Devil’s Tower

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Missouri Buttes and Devil’s Tower

Missouri Buttes and Devil's Tower

Missouri Buttes and Devil’s Tower

This is one of those RARE times when the colorcast from the twilight was so intensely orange, that the reflections on the snow was very noticeable. I’m a photorealist who preaches against “blue snow”. I maintain the practice of maintaining a blue snow free zone in my gallery, except when it was really blue.

So much of the blue snow you see in forum photos is bad color correction or improper setting for white balance in your camera. I’ve always argued that blue snow doesn’t exist in nature but for a few, very few mornings like this extreme one. This color is as I experienced it. I could easily drop out the bark blue in the snow and make it white but that isn’t how it was. Early morning colorcast twilight is the only times I have ever seen this phenomena. Even then, I’ve only seen this one other time 2 winters ago. That time the colorcast was WAY red. This one is a very pervasive colorcast covering every object in it’s glow.

I do sunrises and sunsets almost every day photographically. This twilight was a rare one indeed. This is a view looking to the south east from near the Montana/Wyoming border. This is very far northeastern Wyoming.

Remember that those 4 hills are all related volcanic necks. Being made of hard rock, they stick up above the softer rock the volcanic neck melted through to the surface. Much sediment has been removed around this volcanic pipes now more than a 1000 feet in the air. They used to be miles deep. Everybody known about the Devils Tower but also part of the same “Volcanic neck” complex formed around the same time as the MIssouri Buttes. This is the Non tourist angle from the north east .. Devils tower had more time to cool slowly and the columns formed much better

Location: near the Bliss Dinosaur Ranch, Wyoming/Montana borderlands

Title: Missouri Buttes and Devil’s Tower

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“Belt of Venus” NE Wyoming

"Belt of Venus" NE Wyoming
"Belt of Venus" NE Wyoming

Here I have posted a very well developed “Belt of Venus” . NE Wyoming version. Lots of Ice in the air…..Backshow from the sun that just went down over my shoulder.

This is the view from the Pass at RockyPoint Wyoming showing the 4 volcanic necks. The debris from them being eroded (sediments) are draping off them making an apron of debris to the relatively hard peaks. The Devil’s Tower (left) is the best known volcanic neck in this complex

. The other three peaks were emplace around the same time as the towers rocks were cooling in the deeply buried neck of an ancient volcano.

“Belt of Venus” NE Wyoming

The Missouri Buttes AKA the Three sisters are in fact 4 buttes. Hard to see all 4 unless your on the top of Devils Tower though or in a plane. Two of the buttes rise slightly lower topographically than the Tower, while the remaining two are actually higher. Devil’s Tower was formed from the same type of rock type as the Missouri Buttes. Rocks there are classified as “phonolite porphyry” by geologists.

There is some agreement among geologist (rare thing lol) that these volcanic necks were from the same intrusion of magma. That event created the hard magmatic origin rocks that obviously later resisted erosion better than the surrounding sediments. Thus they stick out of the surrounding landscape that washed away.

Erosional Remnants:

Geologists think magmatic injection, lead to these erosional remnants (mountains). All these peaks rocks were formed during closely related volcanic timelines it appears. Although some columnar jointing is evident in the Little Missouri Buttes, they lack the distinctive appearance and magnificent grandeur of Devils Tower which cooled over a longer period of time allow the giant columnar crystals of Dark Porphyry. These eroded exposed volcanic necks dominate the landscape with their presence here in the NorthEastern Corner of the state. This is almost entirely in Crook County but I’m standing in Campbell County Wyoming.

Location: Bliss Dinosaur Ranch, Wyoming/Montana borderlands.

Title “Belt of Venus” NE Wyoming

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Pink “Belt of Venus” Alpenglow Crack of Dawn on the “Red Hills”

Pink "Belt of Venus" Alpenglow Crack of Dawn on the "Red Hills"
Pink "Belt of Venus" Alpenglow Crack of Dawn on the "Red Hills"

In taking this image Pink “Belt of Venus” Alpenglow Crack of Dawn on the “Red Hills”, I was at around the same elevation as the saddle to the left of the peak off in the “Red Hills” 40 miles away from the camera.

I wonder why they call them the “Red Hills”? hummm.🤔

The Science of this.

The Light Stuff: The Pink Alpenglow known as “The Belt of Venus” is literally the back show of a sunrise over my shoulder that was s a stunning clear sky yellow Alpenglow scene saturated by an orange and yellow gradient sunrise THROUGH the atmospheric ice present. You’ve seen other photos of that in the wetlands around here just recently posted this morning perhaps elsewhere. This is the back show where only the longer more penetrative red/pink rays of light make it through to the relatively light grey atmospheric ice present and reflects even more red. The red rocks on the hills are also adding to the effect of just the tip of the Mountain is exposed to the sun over the shadow of the horizon behind me. Technically the sun has risen for some places and not for others.

Geology: That is the Little Powder River Valley with the Montana/Wyoming border somewhere in there. That little 6 foot wide river removed all the sediment between here and those mountains all by itself. No kidding. I wonder how long that took a spring flood and yearly freeze thaw cycles to break up the bedrock so the river can haul sand/silt/clay most of the time? 🤔 Cobbles only move during floods. Quartz cobbles are common down in the river valley where they eventually make their way. Being harder they resist erosion, being heavy, they don’t travel very fast and tend to concentrate in the river down there. Quartzite cobbles up here in pure fine grained sandstone country are rare. When I find them, they are affiliated with Dinosaur Bone Deposits and are probably “gastroliths” or stomach stones (like chickens swallowing gravel). Dinosaurs moved literally small boulders around in their stomachs and left them here mixed in randomly where you find dinosaur bones. the same river concentrated both just like it does gold.

This has been an alpenglow day……3 posts in a row anyway… Change up is in order I think📸

Location: Bliss DInosaur Ranch, Wyoming/Montana borderlands