A rock can conceivably erode indefinitely. So long as it can be made into smaller and smaller pieces, perhaps into the element or molecule that composed that rock, it could be considered to have eroded. To truly answer this question, one would have to know precisely how much matter was present and a standard by which to erode the object. Such a standard may be removal of a set amount of matter or a binary fission or said matter.
Long answer short, It could "erode" nearly infinitely, or at least until it reached the smallest division by which it could still be considered the rock in question.
Metamorphic rock can change into igneous rock through melting and solidification, or into sedimentary rock through weathering, erosion, and lithification.
Erosion can break down rock by wearing away particles through processes like wind, water, or ice. This can cause rocks to gradually be weathered and worn down into smaller pieces, eventually leading to their erosion and transportation to different locations.
Water erosion is caused by the action of flowing water, which can wear away or transport soil and rock particles. This erosion can occur through processes such as sheet erosion, rill erosion, and gully erosion, depending on the amount and intensity of water flow.
Sedimentary rock forms through the process of weathering, erosion, and deposition. Weathering breaks down existing rocks into smaller pieces, which are then transported and deposited in layers. Over time, these layers are compacted and cemented together to form sedimentary rock.
Rock erosion is caused by a combination of factors such as wind, water, ice, and gravity. These external forces gradually break down rocks into smaller pieces through processes like abrasion, freeze-thaw cycles, and chemical weathering. Over time, this wearing away of rock surfaces leads to erosion.
Erosion.
through erosion and cementation
Metamorphic rock can change into igneous rock through melting and solidification, or into sedimentary rock through weathering, erosion, and lithification.
it turns into sediment
That's when the rocks it goes through the process of erosion.
Erosion can break down rock by wearing away particles through processes like wind, water, or ice. This can cause rocks to gradually be weathered and worn down into smaller pieces, eventually leading to their erosion and transportation to different locations.
The type of rock which makes the grand canyon - sedimentary which causes all of the visible banding. The occurring erosion: -Wind erosion -Water erosion from the river which cuts through it -Erosion from repeat heating and cooling which weakens the rock
The river will break down rock into sediment through the process of erosion, which involves the mechanical wearing away of rock by the force of the flowing water and the chemical breakdown of rock through processes like weathering. These processes result in the transportation of sediment downstream where it can be deposited in a new location.
Metamorphic rock can be transformed into sediments through the processes of weathering, erosion, and deposition. Weathering breaks down the rock into smaller pieces, erosion transports these pieces to new locations, and deposition settles the sediments in layers. Over time, these sediment layers can be compacted and cemented together to form sedimentary rock.
Three landforms shaped by weathering and erosion are canyons, arches, and hoodoos. Canyons form through the erosion of rock by rivers, arches are created by the gradual wearing away of softer rock underneath harder layers, and hoodoos are tall, thin spires of rock formed through erosion of sedimentary rock layers.
Coombe rock is typically formed through a process called weathering and erosion, where softer rocks are gradually worn away by elements such as wind, water, and ice. This erosion leaves behind the more resistant rock formations like coombe rock. Over time, continuous weathering and erosion shape the coombe rock into its characteristic features.
Erosion of igneous and metamorphic rock