Azov Films Sun And Sand Part 1

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Azov Films Sun And Sand Part 1

as the drift moves down the grand canyon it is deposited until the amount of material accumulated reaches the level where it becomes no longer erodible and forms a mountain range. a sand hill is one such accumulation. the sand hill in the grand canyon is wupatki national monument.

sponheim, a huge block of limestone, is oriented northwest to southeast in the geological map on the left. the map of the geologic state of the area is based on rocks, fossils, and well-sorted sediments. since the sedimentary layers in the area are found at different elevations, the rocks and fossils vary in age. the rise of the rocks on the rocks shown on the left helps identify the particular layers in the sequence of sedimentary rocks. in the map the thickness of layers is shown. the color of the layers correspond to the lithology of the rocks (type of sedimentary rock) that composes the geological map.

because the rock bed is spread over such a large area of land, it is possible that a lot of time has passed between the formation of the rock and the final deposition, so that the rocks have been re-worked or tilted, resulting in a change in rock type. the map on the left shows the sequence of rocks in the area. it is apparent that sponheim is made up of many different rocks, but the total thickness of the layers varies. kupferschiefe, a thick layer of white crystals of quartzite, is found in the south in the sponheim rock series, which have a musgästen or mussel-bearing calcareous sandstone. it is quite possible that the beach sand in this area is formed today by wave action, and not by the slow transportation of sand by currents. gespannschiefe, a thin layer of loam, is shown at the top of the map. gespannschiefe is very well sorted, indicating that it is transported. this well-sorted loam is often reworked by wind erosion, resulting in some coarsening of the material. this may indicate that the loam was deposited by current erosion, which would be transporting the material much faster than wind erosion, or that the wind erosion process was very active over time and shaped the loam into its current form.

as the drift moves down the grand canyon it is deposited until the amount of material accumulated reaches the level where it becomes no longer erodible and forms a mountain range. a sand hill is one such accumulation. the sand hill in the grand canyon is wupatki national monument.
sponheim, a huge block of limestone, is oriented northwest to southeast in the geological map on the left. the map of the geologic state of the area is based on rocks, fossils, and well-sorted sediments. since the sedimentary layers in the area are found at different elevations, the rocks and fossils vary in age. the rise of the rocks on the rocks shown on the left helps identify the particular layers in the sequence of sedimentary rocks. in the map the thickness of layers is shown. the color of the layers correspond to the lithology of the rocks (type of sedimentary rock) that composes the geological map.
because the rock bed is spread over such a large area of land, it is possible that a lot of time has passed between the formation of the rock and the final deposition, so that the rocks have been re-worked or tilted, resulting in a change in rock type. the map on the left shows the sequence of rocks in the area. it is apparent that sponheim is made up of many different rocks, but the total thickness of the layers varies. kupferschiefe, a thick layer of white crystals of quartzite, is found in the south in the sponheim rock series, which have a musgästen or mussel-bearing calcareous sandstone. it is quite possible that the beach sand in this area is formed today by wave action, and not by the slow transportation of sand by currents. gespannschiefe, a thin layer of loam, is shown at the top of the map. gespannschiefe is very well sorted, indicating that it is transported. this well-sorted loam is often reworked by wind erosion, resulting in some coarsening of the material. this may indicate that the loam was deposited by current erosion, which would be transporting the material much faster than wind erosion, or that the wind erosion process was very active over time and shaped the loam into its current form.
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