The product of the mechanically weathered rock would be identical to the original rock. The product of the chemically weathered rock would be dissimilar to the original rock.
Weathering is the breakdown of rocks and minerals at or near the Earth's surface, while erosion is the transportation of the weathered material. Weathering physically and chemically breaks down rocks, whereas erosion involves the movement of the weathered material by wind, water, or ice. Both processes work together to shape the Earth's surface over time.
Zircon is the mineral that typically crystallizes last in igneous rocks and is known for its resistance to weathering. It has a high melting point and is chemically stable, making it a durable mineral that can persist long after other minerals have weathered away.
oxidation. Oxygen combines with minerals like iron in the rock, causing it to rust and turn reddish brown.
Erosion is the process of moving weathered material from one place to another, while weathering is the breakdown of rocks and minerals in place. Erosion involves transportation of the weathered material by agents like water, wind, or ice, which weathering does not.
It is when hot & wet climates produce a thin layer of chemically weathered soil.
Sedimentary rocks can be both chemically and mechanically weathered.
Weathering is the breakdown of rocks and minerals at or near the Earth's surface, while erosion is the transportation of the weathered material. Weathering physically and chemically breaks down rocks, whereas erosion involves the movement of the weathered material by wind, water, or ice. Both processes work together to shape the Earth's surface over time.
Clay, silt, and sand are the three types of weathered rock particles found in soil.
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Rainwater is naturally slightly acidic. The acid in rainwater reacts chemically with the calcium carbonate of limestone, dissolving it. The result is chemically weathered limestone, karst terrains, and cave structures.
Zircon is the mineral that typically crystallizes last in igneous rocks and is known for its resistance to weathering. It has a high melting point and is chemically stable, making it a durable mineral that can persist long after other minerals have weathered away.
air oxidation, groundwater, and acid precipitation
Weathered rock provides the material for soil.
oxidation. Oxygen combines with minerals like iron in the rock, causing it to rust and turn reddish brown.
Most surface rock is weathered by water. Naturally acidic rain and groundwater can react chemically with rock, causing dissolution and oxidation. Freezing water can also act on the rock mechanically, forcing open gaps and faults for further weathering attack by liquid water.
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Erosion is the process of moving weathered material from one place to another, while weathering is the breakdown of rocks and minerals in place. Erosion involves transportation of the weathered material by agents like water, wind, or ice, which weathering does not.