Two features formed by underground weathering are caves and sinkholes. Caves are formed through the dissolution of limestone by groundwater, while sinkholes are created when the roof of a cave collapses, causing a depression on the surface.
Two features formed by underground weathering are caves and sinkholes. Caves are formed by the dissolution of limestone or other soluble rocks, creating underground chambers and passages. Sinkholes are depressions in the ground that form when the roof of an underground cavern collapses.
The dominant type of weathering in areas with karst topography is chemical weathering, specifically carbonation. This type of weathering occurs when rainwater combines with carbon dioxide to form a weak carbonic acid that dissolves the limestone bedrock, creating features like sinkholes, caverns, and underground drainage systems.
Lava forms underground in magma chambers. When it erupts onto the Earth's surface through volcanic activity, it becomes lava.
Spheroidal weathering is the process that tends to form spherical boulders. This type of weathering occurs on rocks with varying resistance to weathering, resulting in the development of rounded shapes over time due to the uneven weathering of the rock surfaces.
Erosion typically has a greater impact on the formation of sinkholes than weathering. This is because erosion refers to the wearing away of rock and soil, which can create voids in the ground where sinkholes may form. Weathering, on the other hand, breaks down rocks and minerals but does not necessarily result in the formation of sinkholes.
Two features formed by underground weathering are caves and sinkholes. Caves are formed by the dissolution of limestone or other soluble rocks, creating underground chambers and passages. Sinkholes are depressions in the ground that form when the roof of an underground cavern collapses.
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Igneous rocks form because, magma cools under the ground, or magma erupts, then cools on the ground forming these rocks.
The main form of weathering in a desert is decomposition.
Biological weathering
because of weathering
Rocks form soils due to weathering by wind, sun, rain and ice.
they form by the igneous rock cooling both under and above the ground
The dominant type of weathering in areas with karst topography is chemical weathering, specifically carbonation. This type of weathering occurs when rainwater combines with carbon dioxide to form a weak carbonic acid that dissolves the limestone bedrock, creating features like sinkholes, caverns, and underground drainage systems.