1.Abrasion occurs when two rocks grind together and break up.
2.The repeated heating and cooling of a rock causes heat effects; the expansion and contraction
eventually cracks the rock.
3.The physical activity of plants and animals around rocks can contribute to weathering.
4.Oxidation causes weathering by changing a rock's chemical composition. This occurs when
oxygen reacts with a mineral; it requires only the presence of oxygen, not water.
Four types of weathering that can occur without water include mechanical weathering caused by temperature changes, chemical weathering due to oxygen in the air, biological weathering from plant roots and burrowing animals, and physical weathering caused by wind abrasion.
Weathering can occur over both short and long time scales, from a few days to thousands of years, depending on factors such as the type of rock or material being weathered, climate conditions, and the presence of vegetation or water. Chemical weathering can be a slow process, whereas physical weathering can happen more rapidly in response to factors like temperature changes and mechanical stress.
Weathering can happen at varying rates depending on factors such as the type of rock or minerals involved, the climate, and the presence of biological activity. In general, the process of weathering is slow and occurs over long periods of time. However, some types of weathering, like chemical weathering in tropical environments or physical weathering in areas with freeze-thaw cycles, can be more rapid.
The speed of weathering can vary depending on factors such as climate, type of rock, and presence of vegetation. In general, physical weathering processes like frost action or abrasion tend to happen more quickly than chemical weathering processes like oxidation or hydration. Weathering is typically a slow process that occurs over thousands to millions of years.
Weathering is the process of rocks breaking down. Erosion is what moves the broken down rocks. There are four factors wind, moving water, wind, and gravity. Without weathering there would would be nothing for the Earth to erode.
Four types of weathering that can occur without water include mechanical weathering caused by temperature changes, chemical weathering due to oxygen in the air, biological weathering from plant roots and burrowing animals, and physical weathering caused by wind abrasion.
they get dryno weathering
why does chemical weathering happen?
Weathering can occur over both short and long time scales, from a few days to thousands of years, depending on factors such as the type of rock or material being weathered, climate conditions, and the presence of vegetation or water. Chemical weathering can be a slow process, whereas physical weathering can happen more rapidly in response to factors like temperature changes and mechanical stress.
Weathering can happen at varying rates depending on factors such as the type of rock or minerals involved, the climate, and the presence of biological activity. In general, the process of weathering is slow and occurs over long periods of time. However, some types of weathering, like chemical weathering in tropical environments or physical weathering in areas with freeze-thaw cycles, can be more rapid.
The speed of weathering can vary depending on factors such as climate, type of rock, and presence of vegetation. In general, physical weathering processes like frost action or abrasion tend to happen more quickly than chemical weathering processes like oxidation or hydration. Weathering is typically a slow process that occurs over thousands to millions of years.
Mechanical and chemical weathering both occur.
Weathering is the process of rocks breaking down. Erosion is what moves the broken down rocks. There are four factors wind, moving water, wind, and gravity. Without weathering there would would be nothing for the Earth to erode.
SOMEWHERE
the next landform that will happen? the next landform that will happen is by weathering
Weathering and erosion are related processes that often occur simultaneously. Weathering breaks down rocks into smaller pieces, while erosion transports these pieces to a different location. Both processes work together to shape the Earth's surface over time.
The most common form of weathering is mechanical weathering, which breaks down rocks into smaller pieces without changing their chemical composition. This can happen through processes like frost wedging, root wedging, and abrasion from wind and water.