Skeletal and plant remains.
Clastic and organic sedimentary rocks like conglomerate, coal, some limestones, and shale, are formed under pressure from overlying sediments.
Sedimentary rocks form when sediments such as sand, mud, and organic material are compacted and cemented together over time. These sediments can accumulate in various environments such as rivers, lakes, oceans, and even on land. After burial and compaction, the sediments undergo lithification to become sedimentary rocks.
Sedimentary rocks are formed through the accumulation and compression of sediments, such as sand, mud, and organic matter, over time. The short answer explanation for their formation is that sediments are deposited, compacted, and cemented together to create sedimentary rocks.
Sedimentary rocks are formed through the accumulation and cementation of sediments or organic materials over time. These sediments can come from the erosion of pre-existing rocks, the remains of plants and animals, or chemical precipitation. Through processes like compaction and cementation, these sediments are eventually lithified into sedimentary rocks.
Sediments in sedimentary rocks may be made of fragments of other rocks, minerals, and organic material like remains of plants and animals. These sediments are typically transported and deposited by processes such as erosion, weathering, and deposition.
Sedimentary rocks form when sediments like sand, mud, and organic material are compressed and cemented together over time. These sediments can come from the erosion of pre-existing rocks or the accumulation of organic material. Common examples of sedimentary rocks include sandstone, limestone, and shale.
They are called clastic sedimentary rocks.
Sedimentary rocks.
Sedimentary rocks.
by sediments
Sedimentary rocks are made from the accumulation and compression of weathered and eroded pieces of other rocks, minerals, and organic material such as plant and animal remains. Examples of sedimentary rocks include sandstone, limestone, and shale.
Sedimentary rock.