Limestone is a sedimentary rock that can be formed both chemically and organically. It can form through the accumulation of marine organisms' shells and skeletons (organically) or through the precipitation of calcium carbonate from water (chemically), such as in caves or hot springs.
Limestone is a rock that forms both chemically and organically. It is primarily composed of the mineral calcite, which can precipitate out of water or form from the remains of marine organisms like coral and shells. Over time, these accumulations can build up and harden into limestone rock.
Both are: composed of minerals, subject to weathering and erosion, can be visible on the surface, are derived from natural processes, and are solid. Some sedimentary rocks can be composed almost completely of sediments derived from igneous rock.
When sedimentary rocks are physically changed, their size and shape may be altered through processes like weathering and erosion. When they are chemically changed, minerals within the rocks may be dissolved or precipitated, leading to the formation of new minerals and the alteration of the rock's composition. Both physical and chemical changes can result in the transformation of sedimentary rocks into new rock types through processes like metamorphism.
Sedimentary rock is most similar to metamorphic rock as both types are formed through processes that involve heat and pressure. However, sedimentary rock is distinct in that it is made up of solid fragments of pre-existing rocks or minerals that have been compacted and cemented together over time.
Limestone is a sedimentary rock that can be formed both chemically and organically. It can form through the accumulation of marine organisms' shells and skeletons (organically) or through the precipitation of calcium carbonate from water (chemically), such as in caves or hot springs.
Sedimentary rocks can be both chemically and mechanically weathered.
Limestone is a rock that forms both chemically and organically. It is primarily composed of the mineral calcite, which can precipitate out of water or form from the remains of marine organisms like coral and shells. Over time, these accumulations can build up and harden into limestone rock.
Thunder eggs are technically both sedimentary and igneous rocks. They are formed when gas bubbles in volcanic lava solidify and are later filled with various minerals, such as quartz. So, they have characteristics of both sedimentary (formed through deposition) and igneous (formed through cooling of magma or lava) rocks.
They both are mixed together but compounds are mixed chemically and mixtures are mixed phisically.
Both are: composed of minerals, subject to weathering and erosion, can be visible on the surface, are derived from natural processes, and are solid. Some sedimentary rocks can be composed almost completely of sediments derived from igneous rock.
Physical change. Example: ice melting into water. They're both H2O, so chemically speaking, no new substance is formed.
Both are composed of minerals. Some sedimentary rocks contain pieces of igneous rocks.
Igneous rocks, which come in many different forms.
Sedimentary and conglomerate, as igneous and metamorphic are both formed underground where there is a high pressure and temperature.
Limestone is a chemical sedimentary rock formed from the precipitation of calcium carbonate. It is primarily composed of mineral calcite, which is organic in origin but can also form through inorganic processes. So, limestone is considered both a chemical and organic sedimentary rock.
Both sedimentary rocks of chemical and organic origin are formed through the accumulation and solidification of particles or materials. They can both contain fossils, have distinct layers, and are influenced by environmental conditions during their formation. Additionally, both types of rocks can undergo processes like compaction and cementation.