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16-Mar-2020 05:46

During the glacial advances of the Pleistocene ice sheets covered large areas of North America, Europe, and Asia. Wedge-shaped, ice body composed of vertically oriented ground ice that extends into the top of a permafrost layer.These features are approximately 2 to 3 meters wide at their top and extend into the soil about 8 to 10 meters.The flood model can explain this as contortion induced in soft material during an earthquake or upheaval of a portion of the earth.

If the layers are soft at the time of formation and then subjected to pressure through geological disturbances, a circular column of liquid mud can be squeezed up through the overlying areas.To form, this type of precipitation requires an environment where raindrops develop in an atmosphere where air temperature is above freezing.These raindrops then fall into a lower layer of air with freezing temperatures.In some cases, there is evidence of a bottom layer being whipped up into the layer above, and the two layers solidifying together.Clastic intrusions are further evidence of plasticity in the geological column.

If the layers are soft at the time of formation and then subjected to pressure through geological disturbances, a circular column of liquid mud can be squeezed up through the overlying areas.

To form, this type of precipitation requires an environment where raindrops develop in an atmosphere where air temperature is above freezing.

These raindrops then fall into a lower layer of air with freezing temperatures.

In some cases, there is evidence of a bottom layer being whipped up into the layer above, and the two layers solidifying together.

Clastic intrusions are further evidence of plasticity in the geological column.

A mass of ice found floating in the ocean or a lake.