Fossils are formed from the buried remains of marine organisms. These organisms are under a tremendous amount of pressure and, over time, they fossilize.
The broad flat part of the ocean basins consisting of sand, mud, and the remains of marine organisms is called the continental shelf.
The cemented shells of marine organisms form limestone, which is a type of sedimentary rock. Limestone is predominantly composed of the mineral calcite and can contain fossilized remains of shells and other marine organisms.
No, it is formed when forests die and are covered with layers of rock which compress it and over time turns it into coal. Buried remains of marine organisms formed oil, following mass extinctions,where the oceans have stagnated.
Two types of biogenous sediments are calcareous ooze and siliceous ooze.
No, petroleum is not considered a rock. It is a naturally occurring liquid found underground that is extracted and used as a source of energy. Petroleum is formed from the remains of ancient marine organisms over millions of years.
Fossil fuel
oil
Crude oil comes from these remains but it takes a very long time for them to form.
Crude oil comes from these remains but it takes a very long time for them to form.
Fossil fuel
oil
Crude oil is a liquid, not a plasma. It is a naturally occurring hydrocarbon mixture that is formed from the remains of ancient marine organisms. It is widely used as a source of energy and in the production of various products.
Liquid petroleum is formed from the remains of marine organisms that lived millions of years ago. Over time, these organisms were buried under layers of sediment, which subjected them to heat and pressure. This process transformed the organic material into liquid petroleum through a process called thermal maturation.
The broad flat part of the ocean basins consisting of sand, mud, and the remains of marine organisms is called the continental shelf.
The dead marine organisms are oil and gas now and the people used them for gas and fuel cost companies.
Coal
Ooze on the ocean floor is formed from the remains of marine organisms like phytoplankton and zooplankton, as well as shells and skeletons of marine animals. Over time, these organic materials accumulate and form sediment on the ocean floor.