Rock fragments can be either round or jagged, depending on their origin and the processes they have undergone. Round fragments are typically produced by prolonged weathering and erosion, which smooths their edges as they are transported by water or wind. In contrast, jagged fragments often originate from processes like fracturing or breaking, where the rocks have not been subjected to extensive transport or erosion. The shape of the fragments provides insights into their geological history and the environmental conditions they experienced.
A sedimentary rock that forms when rock fragments are squeezed together is called a conglomerate. This rock is composed of rounded fragments that have been cemented together by a finer material, such as sand or mud.
Sedimentary rocks contain particles of minerals, organic material, and fragments of pre-existing rocks, which have been compacted and cemented together over time. These rocks often include fossils and can be categorized into three main types: clastic, chemical, and organic sedimentary rocks.
Sedimentary rock
Solid rocks
Wind erosion is a type of physical weathering where the force of wind transports and deposits rock fragments, leading to the breakdown and wearing away of rocks over time.
Conglomerate
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 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.
A sedimentary rock that forms when rock fragments are squeezed together is called a conglomerate. This rock is composed of rounded fragments that have been cemented together by a finer material, such as sand or mud.
A sedimentary rock is formed when rock fragments are compacted and cemented together by pressure and minerals. Examples of sedimentary rocks include sandstone, shale, and conglomerate.
Grapefruit spoon.
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 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.
dagger
Depends on what kind of conditions it has been under.
jagged coastlines and many harbors
Sedimentary rocks contain particles of minerals, organic material, and fragments of pre-existing rocks, which have been compacted and cemented together over time. These rocks often include fossils and can be categorized into three main types: clastic, chemical, and organic sedimentary rocks.