Near shore, sedimentary. Deep ocean, extrusive igneous, mainly basalt.
The underlying rock beneath the ocean floor is primarily basalt, which is a mafic rock rich in iron and magnesium. Silica-rich rocks like granite are typically found in continental crust, not beneath the ocean floor.
the rock beneath the ocean is basalt
coral
Basalt
cream cheese
The plutonic igneous rock that forms beneath mid-ocean ridges is primarily gabbro. Gabbro is a coarse-grained rock that crystallizes from magma that cools slowly beneath the Earth's surface, typically associated with the upwelling of magma at mid-ocean ridges. This process contributes to the formation of new oceanic crust as tectonic plates diverge.
The two layers of Earth that are made of rock are the crust and the mantle. The crust is the outermost layer, consisting of solid rock that forms the continents and ocean floors. Beneath the crust, the mantle is composed of semi-solid rock that flows slowly over geological time. Together, these layers play a crucial role in tectonic activity and the Earth's geology.
continental crust.
The crust beneath the ocean is called oceanic crust. It is thinner and younger than continental crust, primarily composed of basaltic rock formed at mid-ocean ridges through volcanic activity.
Phosphorus is trapped in phosphate that makes up phodphate rock and the sediments of ocean floors.
Phosphorus is trapped in phosphate that makes up phodphate rock and the sediments of ocean floors.
The topsoil layer is typically least similar to the underlying rock, as it is a combination of organic matter, minerals, and microorganisms that have been weathered and broken down over time. This layer tends to have a different composition and structure compared to the solid rock beneath it.