Sandstone, conglomerate, and breccia are examples of clastic sedimentary rock, composed of particles of other rocks.
Chat with our AI personalities
Examples of clastic sedimentary rocks include sandstone, conglomerate, and shale. Sandstone is made up of sand-sized grains, conglomerate is composed of rounded gravel-sized particles, and shale is formed from clay-sized particles.
Two examples of clastic rocks include: breccia and sandstone. Also, siltstone, shale, chert, and limestone are other examples of clastic rocks.
Sandstone, claystone, mudstone, conglomerate, and breccia are all examples of detrital sedimentary rocks - those composed of particles of pre-existing rock.
Examples of Clastic Sedimentary Rock are;
1. Sandstone.
2. Shale.
3. Clay.
4. Conglomerate.
5. Mudrock/Mudstone.
The class of sedimentary rocks made of fragments of rock minerals and shells is known as clastic sedimentary rocks. These rocks form from the accumulation and lithification of sediments such as sand, silt, clay, and sometimes organic material. Examples include sandstone, shale, and conglomerate.
Sedimentary rock formed from rock fragments is called clastic sedimentary rock. These rocks are made up of pieces of other rocks that have been weathered, transported, and then deposited and cemented together. Examples include sandstone, shale, and conglomerate.
The type of sedimentary rock formed from deposits carried away from their source by water, wind, or ice is called clastic sedimentary rock. Clastic sedimentary rocks are made up of pieces of other rocks or minerals that have been transported and deposited by erosion processes before being lithified into solid rock. Examples of clastic sedimentary rocks include sandstone, shale, and conglomerate.
No, conglomerate is a sedimentary rock composed of rounded rock fragments cemented together. Clastic rocks are composed of individual grains or fragments of minerals or rocks that have been compacted and cemented together.
Bituminous is not clastic, as clastic refers to sedimentary rocks composed of fragments of pre-existing rocks. Bituminous, on the other hand, is a type of coal formed from the compression and heating of organic matter.