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Field Trip Analysis: Marietta Topographic Quadrangle - Essay Example

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"Field Trip Analysis: Marietta Topographic Quadrangle" paper focuses on the geographical position of the area, an analysis of the general geological information in addition to any other notable geological characteristics. The selected outcrop is within the Marietta Topographic Quadrangle…
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Field Trip Analysis: Marietta Topographic Quadrangle
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In terms of the coordinates, it is within Sec. 2, T2N, R9W. The outcrop exists within an elevation of 640, which is from its base. The Bedrock Geology of Washington County rates the outcrop as of the Pennsylvanian age. The rock formation is of the Monongahela group. The general rock types that exist in this outcrop are shale, siltstone, red shale, and greywacke. Consequently, the following breakdown describes the various compositions that make up the basal layers:

            Layer 1 is made up of 0.5m shale which is moss green. It also has plenty of fern fossils and has a covered basal contact. This layer lies at a lateral intersection with siltstone. Layer 2 consists of 1.5m siltstone. This is greenish-grey in color and exists as a composite. It is also covered in fern fossils and has a covered basal contact. It lies at a lateral intersection with red shale. Layer 3 consists of 3.0m of red shale that is largely reddish in color. This also has covered basal contact and fern fossils. Layer 4 has 1.7m of greywacke that is grey in color. This layer tapers laterally and lacks the ferns. Its basal contact is irregular. Layer 5 is 2.2m of grey siltstone made up of larger lateral grains. There are no ferns and the basal contact is uneven. Layer 6 has 3.5m of greywacke with larger grains. Layer 7 is made up of 1.5m of laterally layered greywacke. The final layer 8 is made up of 1.5m of grey granulated siltstone.

From such a study, various inferences can be drawn from the results, and the corresponding analysis can be compared to the pre-existing theory. This is important in understanding the landscape of such a region due to its dynamic nature it has. The hilltops are predominantly made of greywacke sandstones due to their resistance to weathering. The valleys are otherwise made up of sandstones and shale that erode very easily. As a follow-up, a subsequent essay on the interpretations regarding the depositional surroundings of the sandstones and shale can sufficiently shed more light.

 

 

 

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