Skeletons of ocean organisms and broken rock particles
Breccia is a sedimentary rock composed of angular fragments of other rocks cemented together. It forms when fragments are compacted and cemented together by minerals, creating a mosaic-like appearance. Breccia can consist of a variety of rock types depending on the environment in which it formed.
Conglomerate is a sedimentary rock made up of rock fragments with sharp edges, typically larger than 2 millimeters in size. These fragments are bound together by a matrix of finer-grained material, such as sand or clay.
This type of sedimentary rock is called breccia. Breccia is characterized by its angular-shaped pebbles and fragments that are cemented together by a matrix of smaller particles. It is commonly found in areas where there has been significant tectonic activity or mass wasting processes.
called clastic sedimentary rocks. These rocks are made up of different sizes of rock fragments that have been eroded, transported, and then deposited in layers. Over time, these layers are compressed and cemented together to form solid rock.
Sandstone, conglomerate, and breccia are examples of clastic sedimentary rock, composed of particles of other rocks.
Breccia is a sedimentary rock composed of angular fragments of other rocks cemented together. It forms when fragments are compacted and cemented together by minerals, creating a mosaic-like appearance. Breccia can consist of a variety of rock types depending on the environment in which it formed.
Large, pointy-edged rocks and minerals cemented together.
a clastic sedimentary rock. That's because organic are made up of remains, and chemical are made up of the water cycle, like precipitation etc. research what's a clastic rock and you'll find out. research some info about breccia and you'll se why. I guess you don't wanna research, but its better so that you understand it better than me telling you. hope that's right. luck.
Conglomerate is a sedimentary rock made up of rock fragments with sharp edges, typically larger than 2 millimeters in size. These fragments are bound together by a matrix of finer-grained material, such as sand or clay.
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.
Firstly, a breccia is itself a kind of sedimentary rock. It consists mainly of large (pea sized and up), angular sediment grains. For an existing sedimentary rock to become a breccia, it must be weathered into fragments, redeposited elsewhere, and buried to sufficient pressure for the sediment to become rock.
This type of sedimentary rock is called breccia. Breccia is characterized by its angular-shaped pebbles and fragments that are cemented together by a matrix of smaller particles. It is commonly found in areas where there has been significant tectonic activity or mass wasting processes.
Yes, coarse sedimentary rock can be made up of pebbles or boulders. Coarse sedimentary rocks are formed from the accumulation and cementation of larger grains, such as pebbles and boulders, that are transported by water, ice, or wind. These larger grains are typically found in rocks like conglomerate or breccia.
A sedimentary rock called "breccia". The sharp angular pebbles making up the breccia could be igneous, sedimentary, or metamorphic. Breccias generally form close to the point of origin of the clast rock, having less time to round those sharp angular edges.
There are lots of seDimentary rocks. Limestone, coquina, sandstone, conglomerate, breccia, gypsum, halite, shale, coal...anything that has been formed from layers of sediment piling up, getting smushed together, and forming chemical bonds is a sedimentary rock.
A sedimentary rock called "breccia". The sharp angular pebbles making up the breccia could be igneous, sedimentary, or metamorphic. Breccias generally form close to the point of origin of the clast rock, having less time to round those sharp angular edges.
called clastic sedimentary rocks. These rocks are made up of different sizes of rock fragments that have been eroded, transported, and then deposited in layers. Over time, these layers are compressed and cemented together to form solid rock.