Sedimentary rocks are formed when bits of existing rocks get stuck together
Clastic Sedimentary Rocks.
Some examples of clastic sedimentary rocks include sandstone, conglomerate, shale, and breccia. These rocks are formed from the accumulation of fragments of pre-existing rocks and minerals, which are then compacted and cemented together over time.
Sedimentary rocks are formed from the weathering and erosion of pre-existing rocks. This process involves the breakdown of rocks into small particles that are then compacted and cemented together to form sedimentary rocks such as sandstone, shale, and limestone.
Detrital sedimentary rocks are made up of particles that have been weathered and eroded from pre-existing rocks. These particles are transported and deposited by water, wind, or ice, and then compacted and cemented together to form rocks like sandstone, shale, and conglomerate. They are characterized by their grain size and composition, reflecting the source rocks from which they originated.
A rock formed from grains stuck together would be Porous
If existing bits of rock become attached through the process of lithification, a clastic sedimentary rock is formed.
morpheus rock is formed i think
metamorphic rocks.
Clastic sedimentary rocks are formed from particles of pre-existing sedimentary, metamorphic, or igneous rock that are deposited, compacted, and cemented together by natural processes.Clastic sedimentary rock is made of fragments of rocks cemented together by a mineral such as calcite or quartz.
They are rocks formed from pieces of pre-existing rocks or organic debris.
Clastic Sedimentary Rocks.
Sedimentary rock is formed from pieces of other rocks, minerals, and organic materials that have been compacted and cemented together over time. Examples of sedimentary rocks include sandstone, shale, and limestone.
No. Metamorphic rocks are formed from existing rocks by the action of heat and pressure. Igneous rocks are formed when liquid magma (or lava) cools and sets. Sedimentary rocks are formed when solid particles sink to the bottom of bodies of water, and gradually get compressed together by later sediments.
Some examples of clastic sedimentary rocks include sandstone, conglomerate, shale, and breccia. These rocks are formed from the accumulation of fragments of pre-existing rocks and minerals, which are then compacted and cemented together over time.
Metamorphic rocks are formed by the alteration of pre-existing rocks due to high heat and pressure deep within the Earth's crust. Examples of metamorphic rocks include marble, slate, and schist.
Sedimentary rocks are formed from the weathering and erosion of pre-existing rocks. This process involves the breakdown of rocks into small particles that are then compacted and cemented together to form sedimentary rocks such as sandstone, shale, and limestone.
Gniess is formed from pre-existing rocks that are subjected intense derectional pressure.