"Belt of Venus" NE Wyoming
Here is a 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 of the complex as it’s closer to the interstate. The other three peaks were emplace around the same time as the towers rocks cooled in the neck of an ancient volcano. Title: “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. The Tower was formed from the same type of rock that the Missouri Buttes is called “phonolite porphyry”. (PP). There is some agreement among geologist 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:
It makes sense that the rocks leading to these erosional remnants (mountains) were emplaced the same general closely related volcanic timeline. 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.
"Belt of Venus" NE Wyoming
Here is a 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 of the complex as it’s closer to the interstate. The other three peaks were emplace around the same time as the towers rocks cooled in the neck of an ancient volcano. Title: “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. The Tower was formed from the same type of rock that the Missouri Buttes is called “phonolite porphyry”. (PP). There is some agreement among geologist 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:
It makes sense that the rocks leading to these erosional remnants (mountains) were emplaced the same general closely related volcanic timeline. 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.