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.
Root wedging is a form of mechanical weathering, not chemical weathering. It occurs when tree roots grow into cracks in rocks, applying pressure that causes the rock to break apart over time. Chemical weathering involves the breakdown of rocks through chemical reactions, such as oxidation or dissolving.
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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The main form of weathering in a desert is decomposition.
Igneous rocks form because, magma cools under the ground, or magma erupts, then cools on the ground forming these rocks.
Biological weathering
because of weathering
they form by the igneous rock cooling both under and above the ground
Rocks form soils due to weathering by wind, sun, rain and ice.
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.