A sedimentary rock made up of rock fragments or particles of other rocks is called 'clastic'.
Breccia refers to a rock that is composed of the broken fragments of the rocks or minerals that have been cemented together. The broken fragments of the rocks or minerals are usually cemented together to form a fine grained matrix.
Breccia is a clastic sedimentary rock with large angular fragments cemented in a finer matrix.
Breccia is an inorganic land-derived sedimentary rock. It is clastic (fragmental), but not foliated. Breccia is composed of mostly quartz, feldspar, and clay minerals; it may contain fragments of other rocks and minerals.
Breccia is a clastic sedimentary rock composed of various sized visible pieces of other rock, cemented together by the processes of lithification.The pieces of rock that are visible are angular fragments, meaning they have somewhat jagged edges. This means that the fragments in the breccia did not travel far before they were deposited. If they had traveled longer and further they would have become rounded, in which case the resulting sedimentary rock would have been called conglomerate.
Breccia is a sedimentary rock that is composed of large angular fragments of various rocks cemented together by a fine-grained matrix. These fragments are typically a mix of different minerals and rock types, giving breccia a diverse appearance.
Conglomerate or Breccia. You'd have to specify the shape of the fragments and types of minerals.
Breccia refers to a rock that is composed of the broken fragments of the rocks or minerals that have been cemented together. The broken fragments of the rocks or minerals are usually cemented together to form a fine grained matrix.
Breccia is a clastic sedimentary rock with large angular fragments cemented in a finer matrix.
Breccia is a clastic sedimentary rock.
Breccia is the type of sedimentary rock that is made of other fragmented rocks. The mineral that holds the fragments together can be made from the same rock material as the larger fragments, or from a different type of rock entirely.
Classic sedimentary rocks are made up a minerals, grains, and rock fragments from older rocks. Some examples of this kind of rock are sandstone, breccia, and shale.
Breccia is an inorganic land-derived sedimentary rock. It is clastic (fragmental), but not foliated. Breccia is composed of mostly quartz, feldspar, and clay minerals; it may contain fragments of other rocks and minerals.
Breccia is a clastic sedimentary rock composed of various sized visible pieces of other rock, cemented together by the processes of lithification.The pieces of rock that are visible are angular fragments, meaning they have somewhat jagged edges. This means that the fragments in the breccia did not travel far before they were deposited. If they had traveled longer and further they would have become rounded, in which case the resulting sedimentary rock would have been called conglomerate.
Breccia is a sedimentary rock that is composed of large angular fragments of various rocks cemented together by a fine-grained matrix. These fragments are typically a mix of different minerals and rock types, giving breccia a diverse appearance.
Sedimentary rocks composed of older rocks are called "conglomerate" or "breccia." These rocks form when fragments of older rocks are compacted and cemented together to create a new rock.
Clastic sedimentary rocks are formed from the accumulation of fragments of pre-existing rocks that have been transported and deposited by water, wind, or ice. These fragments, called clasts, are typically cemented together by mineral material to create the rock.
No, sedimentary rocks formed from fragments of other rocks are called clastic sedimentary rocks. Chemical sedimentary rocks form from minerals that are dissolved in water and precipitate out to form rocks like limestone or halite.