clastic sedimentary
Volcanic eruptions are most likely to produce fragmental sedimentary rocks due to the rapid cooling and subsequent deposition of ejected volcanic material, such as ash, lava fragments, and rocks. These materials can accumulate, compact, and cement together to form rocks like tuff or volcanic breccia.
The main types of rock texture are crystalline, fragmental, glassy, and vesicular. Crystalline rocks have interlocking mineral grains, fragmental rocks are made up of broken fragments of pre-existing rocks, glassy rocks have no crystal structure due to rapid cooling, and vesicular rocks have cavities or bubbles caused by gas escaping during solidification.
Yes, a rock can be classified as sedimentary, igneous, or metamorphic based on its method of formation. Sedimentary rocks form from the accumulation and cementation of sediments, igneous rocks form from the solidification of magma or lava, and metamorphic rocks form from the alteration of existing rocks due to heat and pressure.
Igneous rocks are the category of rocks that contain diamonds. The two types of igneous rocks that form diamonds are kimberlites and lamproites.
Sedimentary rocks can be classified based on their composition, texture, and the way they were formed. Common classifications include clastic, chemical, and organic sedimentary rocks. Clastic rocks are made of fragments of other rocks, while chemical rocks form from dissolved minerals. Organic rocks are made from the remains of plants and animals. Texture can also help classify sedimentary rocks, such as fine-grained, coarse-grained, or conglomerate.
Volcanic eruptions are most likely to produce fragmental sedimentary rocks due to the rapid cooling and subsequent deposition of ejected volcanic material, such as ash, lava fragments, and rocks. These materials can accumulate, compact, and cement together to form rocks like tuff or volcanic breccia.
Fragmental sedimentary rocks are formed from rock fragments, such as sand, gravel or clay. These fragments become cemented together because of pressure and other chemical reactions.
A fragmental sedimentary rock is composed of fragments of pre-existing rocks or minerals that have been eroded, transported, and deposited. These fragments, known as clasts, can vary in size and are typically held together by a cementing material. Examples of fragmental sedimentary rocks include sandstone, conglomerate, and breccia.
The main types of rock texture are crystalline, fragmental, glassy, and vesicular. Crystalline rocks have interlocking mineral grains, fragmental rocks are made up of broken fragments of pre-existing rocks, glassy rocks have no crystal structure due to rapid cooling, and vesicular rocks have cavities or bubbles caused by gas escaping during solidification.
Yes, a rock can be classified as sedimentary, igneous, or metamorphic based on its method of formation. Sedimentary rocks form from the accumulation and cementation of sediments, igneous rocks form from the solidification of magma or lava, and metamorphic rocks form from the alteration of existing rocks due to heat and pressure.
Sedimentary rocks are classified based on their mineral composition, grain size, texture, and the way they were formed. The three main types of sedimentary rocks are clastic, chemical, and organic. Clastic rocks are made up of broken fragments of other rocks, chemical rocks form from precipitation of minerals from water, and organic rocks are formed from the accumulation of plant and animal remains.
they are classified into 3 major kinds of rocksthey are the ;IGNEOUS ROCKS,SEDIMENTARY ROCKS,AND METAMORPHIC ROCKS
sedimentary rocks can be classified by detrial, chemical ,or organic
Igneous rocks are classified based on their mineral composition, texture, and origin. They can be divided into two main categories: intrusive rocks, which form from magma cooling beneath the Earth's surface, and extrusive rocks, which form from lava cooling on the Earth's surface or in the air. Within these categories, igneous rocks can then be further classified into specific types based on their mineral content and texture.
Igneous rocks are classified as either extrusive or intrusive. Extrusive rocks form from lava at or above the ground, and intrusive rocks form from magma below the ground. Granite is intrusive, pumice is extrusive.
No, igneous rocks are not classified by their shape. They are primarily classified based on their origin (either intrusive or extrusive) and their texture (coarse-grained, fine-grained, glassy, etc.). Shape or form is not a major factor in the classification of igneous rocks.
They are classified by their composition.