Texture
The features that indicate how a sedimentary rock is layered include bedding planes, which represent the boundaries between different layers of sediment, and graded bedding, where grains are sorted by size within a layer. Additionally, cross-bedding can show inclined layers within a sedimentary rock, indicating the direction of sediment deposition.
PYROCLASTIC ROCKS AND TEPHRA, Pyroclasts .
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meterologists
Shadows can provide information about the depth and direction of geological features, such as mountain ranges or volcanic peaks, on the surface of the Earth. By studying the lengths and angles of shadows, geologists can infer the approximate shape and elevation of land formations, helping to better understand the Earth's interior composition and structure.
texture
The size of the grains in a sedimentary rock is primarily indicated by its texture, which can be described as coarse, medium, or fine. The presence of visible grains, their shape, and the degree of sorting (uniformity of grain size) are key features that help determine grain size. Additionally, the rock's composition and the method of deposition can provide insights into the grain size, as different environments produce distinct sediment characteristics.
Sedimentary rocks are often deposited in layers as strata. The feature that tells how a sedimentary rock is layered is called the bedding.
The features that indicate how a sedimentary rock is layered include bedding planes, which represent the boundaries between different layers of sediment, and graded bedding, where grains are sorted by size within a layer. Additionally, cross-bedding can show inclined layers within a sedimentary rock, indicating the direction of sediment deposition.
Sedimentary rocks are often deposited in layers as strata. The feature that tells how a sedimentary rock is layered is called the bedding.
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Talligator
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Grain size is more important for determining the classification of clastic sedimentary rocks, such as sandstone or shale. Composition is more important for determining the classification of chemical sedimentary rocks, such as limestone or rock salt. Layering is more important for identifying the structure of sedimentary rocks, such as bedding in sandstone or shale.
PYROCLASTIC ROCKS AND TEPHRA, Pyroclasts .
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Gerard tells his employees that the company website needs to be redesigned. He tells them what features it should have and when it's due, but let's them decide on the design.