Sinkhole and a cavern
The two features formed by underground weathering are caves and caverns. Caves are natural underground chambers typically formed in limestone, while caverns are larger caves that often have unique formations such as stalactites and stalagmites.
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.
No, litter is typically formed by humans leaving behind waste materials such as plastic bags, wrappers, and bottles in public areas or nature. Weathering refers to the breaking down of rocks and other materials through processes like wind, rain, and temperature changes. These two concepts are not directly related.
Bedrock is formed from the consolidation of solid rock materials, such as granite or basalt, through processes like cooling and pressure. Subsoil is formed from the weathering and decomposition of bedrock, which creates a layer of material composed of minerals and organic matter.
The two main types of weathering are mechanical weathering and chemical weathering. Mechanical weathering involves physically breaking down rocks into smaller pieces, while chemical weathering involves the alteration of rock composition through chemical reactions.
The two features formed by underground weathering are caves and caverns. Caves are natural underground chambers typically formed in limestone, while caverns are larger caves that often have unique formations such as stalactites and stalagmites.
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.
holy shift
Stalagmites and stalactites are two features formed by underground deposition. Stalactites hang from the ceiling of caves and are formed as mineral-rich water drips down and leaves behind deposits of minerals. Stalagmites, on the other hand, form on the cave floor as the dripping water deposits minerals and builds up over time.
In a region with karst topography, you would typically find features such as sinkholes, which are depressions or holes formed when underlying limestone dissolves and collapses. Additionally, you might encounter limestone caves, created by the erosion of soluble rock by water, leading to intricate underground systems. These features result from the chemical weathering process that characterizes karst landscapes.
Two features formed by underground deposition are stalactites, which hang from the ceiling of caves, and stalagmites, which grow up from the floor of caves. These formations are created as mineral-rich water drips from the ceiling and leaves behind deposits of minerals like calcite or gypsum.
Extrusive-formed on surfaceIntrusive-formed underground
The two features formed by wave deposition are islands and beaches.
physical & change weathering climate
The 2 kinds of weathering are the Mechanical or Physical Weathering and the Mechanical Weathering.
The two primary requirements for karst topography are soluble rock, typically limestone, and sufficient rainfall to facilitate the chemical weathering process. The dissolution of the rock occurs as acidic water seeps through the soil, creating unique landforms such as sinkholes, caves, and underground rivers. These processes lead to the characteristic features of karst landscapes.
The London Underground began operation in 1863. A group was first formed in the 1850's to build the underground transportation system. The Underground stations were used in World War Two as shelters from German bombing, and many Londoners spend the night in the Underground to survive the bombs.