shale
Shale is a sedimentary rock formed from the compaction of fine-grained sediment such as mud or clay.
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.
Chalk is a type of sedimentary rock that is primarily composed of organic material, specifically the calcareous remains of marine microorganisms such as coccolithophores. It is not considered clastic, as it does not consist of fragments of pre-existing rock like clastic sedimentary rocks.
Sedimentary Rocks are classified based on some criterials, such as Origin and Mode of formation. Sedimentary Rocks can be classified into 3 as follows; 1. Clastic Sedimentary Rock. eg. Sandstone. 2. Organic Sedimentary Rock. eg. Limestone. 3. Chemical Sedimentary Rock. eg. Gypsum.
Clastic sedimentary rocks: Formed from the accumulation of mineral and rock fragments that are cemented together. Chemical sedimentary rocks: Formed from precipitation of minerals dissolved in water. Organic sedimentary rocks: Formed from the accumulation of organic material, such as plants or animals.
Clastic sedimentary rock.
Shale is a sedimentary rock formed from the compaction of fine-grained sediment such as mud or clay.
Shale is clastic sedimentary rock.
Breccias are a relatively common clastic sedimentary rock.
sedimentary rock
non clastic sedimentary rock :)
Shale is clastic sedimentary rock.
Fragmentation clastic sedimentary rock is formed by the lithification of inorganic and/or organic sediments.
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.
Shale, sandstone, and conglomerate are examples of clastic sedimentary rock.
None of the above. These terms describe sedimentary rocks. Granite is igneous.
Chalk is a type of sedimentary rock that is primarily composed of organic material, specifically the calcareous remains of marine microorganisms such as coccolithophores. It is not considered clastic, as it does not consist of fragments of pre-existing rock like clastic sedimentary rocks.