Volcanic Ash

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Volcanic Ash

 

 

Volcanic ash on SR 95 between Blanding, UT Natural Bridges National Monument

Volcanic ash on SR 95 between Blanding, UT Natural Bridges National Monument

 

 

 

 

 

 

We saw this volcanic ash on SR 95 west of Blanding, Utah when we were on our way to visit Natural Bridges National Monument. It is so unusual in this area that is dominated by sandstone.

 

Note that this volcanic ash has a greenish tint. I suspect it getting that green coloring from copper?

 

 

 

 

 

 

 

 

 

 

 

Volcanic ash visible in Arches National Park Moab, Utah

Volcanic ash visible in Arches National Park Moab, Utah

 

On the left is volcanic ash. I suspect this ash is part of the 150-million year old Morrison Formation. Specifically the Brushy Basin Member of the Morrison Formation (famous for dinosaur fossils) because it is visible as greenish mudstones, originating as volcanic ash that settled into a large alkaline lake.

One source says that the green tint is because of the iron content in the volcanic ash that has undergone a chemical process that creates that green tint.

I would have suspected copper not iron, but who am I?

 

 

 

 

 

 

 

 

Volcanic Ash along Colorado River in eastern Utah

Volcanic Ash

 

 

 

We were traveling between Moab, Utah and Grand Junction, Colorado along the Colorado River when we spotted this area of volcanic ash.

Once we cross over to the north side of the Colorado River we start to climb out of that sandstone canyon we had been in since Moab. The bright red cliffs of sandstone have given away to younger formations that are more grey in color and obviously volcanic ash.

 

 

 

 

 

 

 

 

 

 

Volcanic Ash along the Colorado River in eastern Utah

Volcanic Ash

 

 

 

As we start our climb away from the Colorado River we came upon this area of volcanic ash. I suppose it is part of the 150-million year old Morrison Formation where of volcanic ash was deposited in the large alkaline lake that covered this area. That would make sense since we are gaining elevation and would naturally be in much younger rock formations than the sandstone we were seeing downstream.

 

 

 

 

 

 

 

 

 

 

 

 

Volcanic ash that has aged into white claystone near Wheatland, Wyoming

Volcanic ash that has aged into white claystone

 

 

 

 

This is volcanic ash that has formed white claystone and is common around Wheatland, Wyoming. Geologist think that the ash was blown in on prevailing westerly winds from volcanic eruptions in Nevada. As thick as this stuff is there must have been some heavy volcanic action in Nevada. This volcanic ash appeared during the same time period as the volcanic action was occurring in Nevada.

 

 

 

 

 

 

 

 

 

More volcanic ash (now white claystone) that covers the open range around Wheatland, Wyoming

volcanic ash (now white claystone) that covers the open range around Wheatland, Wyoming

 

 

 

 

This is more of that white claystone that is made of compacted volcanic ash.

 

 

 

 

 

 

 

 

 

Volcanic ash caprock on this sandstone outcropping near Grants, New Mexico and Mt. Taylor

Volcanic ash caprock on this sandstone outcropping near Grants, New Mexico and Mt. Taylor

 

 

 

The gray rock is a layer of volcanic ash that at one time formed a layer of sediment. It is now crumbling and mixing with the much older sandstone sediments.

Volcanic ash also provides a bonding agent that holds the sandstone together.

Sandstone is actually a sedimentary rock formed by the consolidation and compaction of sand, which is held together by a natural cement, such as silica.

 

 

 

 

 

 

 

 

 

Volcanic ash visible in roadcut near Sandia Peak east of Albuquerque, New Mexico

Volcanic ash visible in roadcut near Sandia Peak east of Albuquerque, New Mexico

 

 

 

 

 

As we head north on SR-14 we are treated to a wondrous variety of roadcuts. The layer of sedimentary rock on the bottom is obviously very hard while the sediments on top are much softer. The soft layers contain a lot of volcanic ash.

 

 

 

 

 

 

 

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