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∙ 13y agoCoarse particles are heavier and settle quickly due to gravity, leading to deposition near the shore where energy from waves and currents is lower. Finer particles are lighter and are carried further offshore by the water flow before settling, resulting in deposition at greater distances from the shore.
extrusive
mars
A slowly cooled magma is likely to result in a rock with a coarse-grained texture because the crystals have more time to grow larger. Examples of rocks with coarse-grained textures from slowly cooled magma include granite and diorite.
Seaweed, coral, and corps
They were deposited horizontally and then shifted by a geologic event.
The deposit is most likely transported and deposited by a glacier. Glaciers are massive sheets of ice that can carry rock particles long distances and leave behind unsorted and scratched deposits as they melt and retreat. This process is known as glacial deposition.
The river's velocity is much slower on the inside bend of a meander, so any material being transported in the river is deposited.
extrusive
It is most likely formed underground.
mars
The mass of the sediment covering the US varies greatly depending on location, but it amounts to billions of tons in total. This sediment was primarily deposited by glaciers, rivers, and wind over millions of years, forming the diverse landscapes we see today.
conglomerate
conglomerate
Big Foot
Sedimentary rocks, such as sandstone, shale, and limestone, are most likely to result from the compaction and cementation of particles. These rocks form through the accumulation and lithification of sediments that have been weathered and eroded from pre-existing rocks.
The texture of an igneous rock formed from cooling magma deep beneath the earth is typically coarse-grained. This is because the slower cooling process allows larger mineral crystals to form within the rock.
Sedimentary rock, such as sandstone, is most likely formed from the compaction and cementing of particles together. As layers of sediment accumulate and are compressed over time, the particles are gradually cemented together by minerals, creating a solid rock.