Devils Tower National Monument

Wonders of the world Devils Tower National Monument Do you feel the wonders ? Devil's Tower in Wyoming state. It is a stone that was hand-ground pop up a screen similar to the excision of a large tree stump of a mammoth. W here this happens because the melting of volcanic rock. When they catch cold. And the heat and sun, wind and rain erosion, blow it up. The layers of rock are in the clear. And looks very unnatural. These layers of rock to stabilize the fracture by a square around it. I almost can not believe that nature is a wonderful thing to be like this.

The landscape surrounding Devils Tower is composed mostly of sedimentary rocks. The oldest rocks visible in Devils Tower National Monument were laid down in a shallow sea during the Triassic period, 225 to 195 million years ago. This dark red sandstone and maroon siltstone, interbedded with shale, can be seen along the Belle Fourche River. Oxidation of iron minerals causes the redness of the rocks. This rock layer is known as the Spearfish Formation.

Above the Spearfish formation is a thin band of white gypsum, called the Gypsum Springs Formation. This layer of gypsum was deposited during the Jurassic period, 195 to 136 million years ago.

Created as sea levels and climates repeatedly changed, gray-green shales (deposited in low-oxygen environments such as marshes) were interbedded with fine-grained sandstones, limestones, and sometimes thin beds of red mudstone. This composition, called the Stockade Beaver member, is part of the Sundance Formation. The Hulett Sandstone member, also part of the Sundance formation, is composed of yellow fine-grained sandstone. Resistant to weathering, it forms the nearly vertical cliffs which encircle the Tower itself.

About 65 million years ago, during the Tertiary period, the Rocky Mountains and the Black Hills were uplifted. Magma rose through the crust, intruding into the existing sedimentary rock layers.


Wonders of the world Devils Tower National Monument Do you feel the wonders ?
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