Volcanoes do not only occur in oceanic crust; they can also be found in continental crust. While many volcanic eruptions happen at mid-ocean ridges or subduction zones associated with oceanic plates, continental volcanoes can form due to rifting, hotspots, or tectonic activity in continental regions. For example, the Cascade Range in the Pacific Northwest of the U.S. features volcanoes formed on continental crust. Thus, both oceanic and continental crust can host volcanic activity.
The simple answer: Oceanic crust is more dense than the continental crust, so it goes under as the two plates ram into each other. (This is called subduction) This submerged crust melts into magma, and collects into a large pool under the continental plate where it went under. The pool of magma forces its way up to form a volcano, which sits in front of us and blows when least expected. The whole process takes a very long time. Also, it only happens in convergent boundaries.
yes but oceanic crust is younger than continental crust because of deep sea trenches
Hot spots can occur in both oceanic and continental crust, not just in oceanic crust. They are caused by plumes of hot material rising from deep within the Earth's mantle, which can create volcanic activity. While many well-known hot spots, like the Hawaiian Islands, are located in oceanic regions, others, such as the Yellowstone hotspot, are found beneath continental crust. Therefore, hot spots are not limited to oceanic crust alone.
The correct answers are - B. Where oceanic crust meets continental crust, and C. Earthquakes.Subduction zones appear only on places where a crust of lower density (oceanic crust) meets a crust of higher density (continental crust).On the places where the oceanic crust meets the continental crust, the oceanic crust goes beneath the continental crust, this makes changes and readjustments in the inner part of the crust, and plus there's significant pressure from the mantle layer from beneath, so earthquakes are a very common occurrence.Check all that apply. A. Broad river deltas B. Where oceanic crust meets continental crust C. Earthquakes D. Two continents collide
Volcanic eruptions occur only in certain places and do not occur randomly. ... Volcanoes occur most frequently at plate boundaries
It occurs in the oceanic crust!!!
The simple answer: Oceanic crust is more dense than the continental crust, so it goes under as the two plates ram into each other. (This is called subduction) This submerged crust melts into magma, and collects into a large pool under the continental plate where it went under. The pool of magma forces its way up to form a volcano, which sits in front of us and blows when least expected. The whole process takes a very long time. Also, it only happens in convergent boundaries.
yes but oceanic crust is younger than continental crust because of deep sea trenches
No, earthquakes can occur anywhere in the crust, oceanic crust or continental crust. An earthquake occurs when the hard brittle solid material of the crust fractures under stress. Earthquakes cannot occur deeper than the crust (the mantle is plastic and flows slowly under stress instead of fracturing, the outer core is liquid and flows even easier than the mantle).
They do not pop up everywhere. they only occur along the fault lines (where the plates that form the earth's crust meet). Volcanoes have been occurring along fault lines since the creation of the earth's crust (billions of years)
The correct answers are - B. Where oceanic crust meets continental crust, and C. Earthquakes.Subduction zones appear only on places where a crust of lower density (oceanic crust) meets a crust of higher density (continental crust).On the places where the oceanic crust meets the continental crust, the oceanic crust goes beneath the continental crust, this makes changes and readjustments in the inner part of the crust, and plus there's significant pressure from the mantle layer from beneath, so earthquakes are a very common occurrence.Check all that apply. A. Broad river deltas B. Where oceanic crust meets continental crust C. Earthquakes D. Two continents collide
Two differences are that the oceanic crust is more dense than continental, and continental crust is composed mostly of granite, while oceanic is mostly basalt
The plates that include only oceanic crust with no continents are the Pacific Plate, Nazca Plate and the Juan de Fuca Plate. These plates are mainly composed of basaltic oceanic crust and are located in the ocean basin areas.
Volcanic eruptions occur only in certain places and do not occur randomly. ... Volcanoes occur most frequently at plate boundaries
The continental crust is about 35 to 40 kilometers thick, while the oceanic crust averages at about 7-10 kilometers thick. This means that the continental crust is about 3.5 to 4 times the thickness of the oceanic crust.
If you meant thicker, the answer is no: Continental crust is much thicker than Oceanic crust. This is because the oceanic crust is formed very quickly, at an ocean ridge, for example, where the lava gradually erupts. The continental crust, on the other hand, is like a river delta: over time, it grows in height as more material is added on top (by volcanoes and other intrusions, as well as other uplifting processes). The reason why we can't touch the Moon is because uplift and eruptions are balanced by weathering and erosion. Therefore, the thickness is regulated by an equilibrium, and this causes the crust to be thick. The thickness of the oceanic crust is not regulated in such a way, but additions to its thickness are irrelevant as the oceanic crust is very quickly subducted again. Millions of years ago, there was a small sea between Britain and the Laurentine continent. This consisted of Oceanic crust. It was then very quickly consumed again when the plates changed their direction. The same could happen, in theory, to the Atlantic Ocean. Only time will tell...
No, hot spots can form in both oceanic and continental crust. Hot spots are areas of high volcanic activity that are thought to be caused by a deep-seated mantle plume that rises to the surface, creating a localized area of magma upwelling. These hot spots can create volcanic islands, such as the Hawaiian Islands, regardless of whether they are in oceanic or continental crust.