Oceanic ooze is soft mud that is calcareous or siliceous on they ocean floor. It is far beneath the surface of the ocean and is deposited by waves, contains the shells of one celled organisms.
Radiolarian ooze is formed by the accumulation of silica skeletons of tiny marine organisms called radiolarians. These skeletons sink to the ocean floor after the radiolarians die, creating a sediment known as ooze. Over time, the ooze can accumulate and compact to form layers and eventually turn into rock.
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.
The island-arc volcanoes are formed from the subduction of an oceanic tectonic plate under another tectonic plate, and often parallel an oceanic trench.
The island-arc volcanoes are formed from the subduction of an oceanic tectonic plate under another tectonic plate, and often parallel an oceanic trench.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Radiolarian ooze is formed by the accumulation of silica skeletons of tiny marine organisms called radiolarians. These skeletons sink to the ocean floor after the radiolarians die, creating a sediment known as ooze. Over time, the ooze can accumulate and compact to form layers and eventually turn into rock.
a trench is formed when 2 oceanic plates collide
it becomes part of the oceanic crust
Island arc mountains are formed when one oceanic plate is subducted beneath another oceanic plate, creating a volcanic island arc.
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.
The island-arc volcanoes are formed from the subduction of an oceanic tectonic plate under another tectonic plate, and often parallel an oceanic trench.
The island-arc volcanoes are formed from the subduction of an oceanic tectonic plate under another tectonic plate, and often parallel an oceanic trench.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Magma leaking in from the mantle.
subduction zones
When an oceanic plate and a continental plate collide, it forms a volcano. The oceanic plate subducts underneath the continental plate. As the oceanic plate slides underneath, a magma chamber is formed. This magma chamber is what feeds the volcano.
because stuff goes and hits some other stuff and.........BOOM..... oceanic lithosphere