NO
Rocks become weathered through a combination of physical and chemical processes. Physical weathering occurs when rocks are broken down into smaller pieces by forces such as wind, water, and temperature changes. Chemical weathering happens when the minerals in rocks react with substances like water and oxygen, leading to their breakdown and dissolution. Over time, these processes can cause rocks to wear away and change their appearance.
Weathered pieces of rock are called sediment. As rocks are broken down by physical or chemical processes, they form sediment that can be transported and eventually deposited elsewhere.
The type of erosion that causes weathered cliffs is typically a combination of mechanical weathering (breaking down of rocks through physical processes like freeze-thaw cycles and abrasion) and chemical weathering (breaking down of rocks through chemical reactions with water and air). Over time, these processes weaken the rock and lead to the formation of cliffs.
Examples of rocks that are easily weathered include limestone, sandstone, and shale, which are sedimentary rocks. Rocks that are resistant to weathering include granite, basalt, and quartzite, which are igneous and metamorphic rocks that have a more crystalline structure and are less prone to chemical breakdown from weathering processes.
Chemical weathered because volcanos occur and avenue lava and when lava cools down it forms a rock or rocks.
A mineral is a solid inorganic matter found in the earth that can break down when weathered. Minerals can be chemically altered or physically broken down through processes like erosion, temperature changes, and chemical reactions with water.
Deposited weathered rocks can form sedimentary rocks through processes like compaction and cementation. These rocks are made up of fragments of pre-existing rocks that have undergone weathering and erosion before ultimately being deposited and lithified to form a new rock.
Weathered rocks with rust streaks are likely to contain iron minerals that oxidize when exposed to air and water, forming iron oxide, or rust. This process occurs over time through a series of chemical reactions, giving the rocks their characteristic rusty appearance.
Rocks buried deep underground must be uplifted to the surface before they can be weathered or eroded. This uplift can happen through tectonic movements, erosion of overlying rocks, or other geological processes that bring the rocks closer to the Earth's surface. Once at the surface, rocks are exposed to weathering processes such as wind, water, and ice that break them down over time.
The rate of chemical weathering increases when a rock becomes more mechanically weathered, also called abrasion.
Mountain rocks can undergo both chemical and mechanical weathering. Mechanical weathering breaks rocks into smaller pieces through physical processes like frost wedging and abrasion. Chemical weathering involves the breakdown of rocks through chemical reactions, such as oxidation or dissolution, which can alter the composition of the rock.
Sedimentary rocks form through processes such as compaction and cementation of sediments, precipitation of minerals from solutions, and accumulation of organic materials. Key ways include clastic formation from weathered rock fragments, chemical sedimentation from dissolved minerals, and biochemical processes involving organisms. However, sedimentary rocks do not form from volcanic activity or directly from molten magma, which are processes associated with igneous rocks.