Detrital sedimentary layers.
Sedimentary rocks made of weathered rock fragments are called clastic sedimentary rocks. These rocks are formed from the accumulation and cementation of fragments that have been weathered, eroded, and transported from their original source. Examples include sandstone, shale, and conglomerate.
They are called clastic sedimentary rocks.
Detrital sedimentary rocks are composed of particles or fragments of pre-existing rocks, minerals, or organic material that have been weathered, transported, and deposited by erosion. These particles are typically deposited in layers and can accumulate to form rocks such as sandstone, shale, and conglomerate. Their composition and texture depend on the source material, the distance of transport, and the conditions of deposition.
Sedimentary rock
Sandstone is the sedimentary rock formed from weathered rock.
Clastic sedimentary rock is formed from weathered particles of rocks and minerals that have been eroded, transported, and deposited. Examples include sandstone, shale, and conglomerate.
Sandstone is the sedimentary rock formed from weathered rock.
Detrital sedimentary layers.
Sedimentary rocks can be both chemically and mechanically weathered.
Clay is formed from rocks by those rocks being weathered to minute particles, those particles being washed in a river and then deposited. As clay is formed of these "sediments" it is sedimentary.
Clastic sedimentary rocks are composed of particles of weathered and eroded or fragmented in situ rocks of varying mineralogy.
When sedimentary rock is weathered in nature by chemical or mechanical means, the particles that are produced can be eroded and deposited, becoming sediments.
Sedimentary rocks made of weathered rock fragments are called clastic sedimentary rocks. These rocks are formed from the accumulation and cementation of fragments that have been weathered, eroded, and transported from their original source. Examples include sandstone, shale, and conglomerate.
When sedimentary rock is weathered in nature by chemical or mechanical means, the particles that are produced can be eroded and deposited, becoming sediments.
Detrital rocks are sedimentary rocks that are composed of particles of weathered and eroded igneous, metamorphic, or other sedimentary rocks that have been deposited, compacted, and cemented together. Sandstone, conglomerate, shale, and breccia are examples of detrital sedimentary rocks.
They are called clastic sedimentary rocks.