Igneous rock becomes sediment due to exposure to chemical and mechanical weathering at or near the surface.
Igneous rock can become sedimentary if it is weathered into sediment and then lithified.
The pressure is from the weight of rock and sediment layered on top of the rock in question.
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It must erode into sediment and then be compressed to form sedimentary rock.
Sediment and rock move to lower elevations primarily due to the force of gravity acting on them. This process, known as erosion, is facilitated by various agents such as water, wind, ice, and gravity itself. Over time, the movement of sediment and rock contributes to the formation of landforms and reshapes the Earth's surface.
Well, first before the sediment can become to a metamorphic rock, it has to create into a sedimentary rock or an igneous rock, Then the rocks go under the ground and is under tons and tons of pressure, which fosters heat build up, and this causes them to change.
Well, first before the sediment can become to a metamorphic rock, it has to create into a sedimentary rock or an igneous rock, Then the rocks go under the ground and is under tons and tons of pressure, which fosters heat build up, and this causes them to change.
The Metamorphic Rock must undergo a process called Weathering and Erosion. Once it has become sediments it goes under another process called Cementing and Compacting. Now it has become a sedimentary rock. Trust Point me if this helped! Thanks!
Igneous rock can become sedimentary if it is weathered into sediment and then lithified.
The pressure is from the weight of rock and sediment layered on top of the rock in question.
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erosion
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It must erode into sediment and then be compressed to form sedimentary rock.
Rain causes rock and sediment to be loosened, and gravity does the rest
Firstly, a breccia is itself a kind of sedimentary rock. It consists mainly of large (pea sized and up), angular sediment grains. For an existing sedimentary rock to become a breccia, it must be weathered into fragments, redeposited elsewhere, and buried to sufficient pressure for the sediment to become rock.
When sediment is deposited in layers and undergoes compaction due to the weight of overlying sediments, it squeezes out water and air, causing the sediment grains to become tightly packed. With time and pressure, this compacted sediment can undergo lithification to become sedimentary rock, such as sandstone or shale.