An ophiolite is a piece of the oceanic crust which has be obducted onto the continental mass. It generally consists of a 4 layer makeup. The bottom layer includes peridotites, the next layer gabbro, then basalt and on top is a thin layer of microorganisms. The ophiolites are rare and generally small in nature.
It would necessarily be sedimentary rock, formed in a saltwater or freshwater environment, depending on the type of clam.
Erosion..... As wind, water, and glaciers move rock debris, they relentlessly disintegrate the rock further.
magma is a mixture of several different types of rock.
A rock that is formed when magma cools is called a igneous rock.
Sedimentary rock is where we look for fossils.
Or they get subducted and re-enter the mantle or they get obducted onto continent (the latter being called an ophiolite).
Or they get subducted and re-enter the mantle or they get obducted onto continent (the latter being called an ophiolite).
Serpentine parent rock refers to a type of metamorphic rock that is primarily composed of serpentine minerals, which are formed from the alteration of ultramafic rocks, such as peridotite. This process, known as serpentinization, typically occurs under high-pressure and low-temperature conditions, often in the presence of water. Serpentine rocks are characterized by their green color and can be associated with geological settings such as ophiolite complexes and subduction zones. They are also significant in mineralogy and are often studied for their potential role in carbon sequestration.
The rock cycle is how one type of rock can be changed into another type of rock.
this mt. has a rock type of rock
Rock
granite is a type of igneous rock.
The type of rock that can be foliated and/or non-foliated is the Igneous rock.
All rock types can be formed from any other rock type.
Magma IS made of melted rock and minerals. Not what type of rock. All types of rock.
Igneus is a type of rock. Metamorphic, too. Sedimentary.
I. L. Abbotts has written: 'A field petrological and geochemical study of the Masirah ophiolite, Oman'