At an ocean-ocean convergent boundary, one of the plates (oceanic crust and lithospheric mantle) is pushed, or subducted, under the other (Figure 4.6. 1). … It mixes with the overlying mantle, and the addition of water to the hot mantle lowers the crust’s melting point and leads to the formation of magma (flux melting).

How does magma form at a mid-ocean ridge quizlet?

Basaltic melt, due to decompression melting, forms magma chamber below mid-ocean ridge crust. Some magma rises through narrow cracks that open as plates separates and form basaltic pillow lavas. Some magma solidifies in cracks as vertical dikes of gabbro. Any remaining magma solidifies as massive intrusions of gabbro.

What two types of igneous rocks are formed at the mid-ocean ridge?

Igneous rock is formed by the cooling and crystallization of molten magma at volcanoes and mid-ocean ridges, where new crust is generated. Examples of igneous rock are basalt, granite, and andesite (Fig.

Why is so much mafic magma erupted along mid-ocean ridges quizlet?

As the asthenosphere rises, pressure decreases and the rock partially melts (decompression melting). The buoyant, mafic magma rises away from the unmelted residue in the mantle and accumulates in magma chambers in the crust and upper mantle. … Mafic rocks are the main type of rocks that form along mid-ocean ridges.

Which type of volcanoes are formed by hotspots quizlet?

Hotspot volcanoes are technically always shield volcanoes, so that it what they look like. They can form island chains.

What are hotspots in the ocean?

Summary. Oceanic hotspots are the surface expression of rising mantle plumes from the Earth’s interior and are responsible for much of the intraplate volcanism observed in the ocean basins.

What is the magma chamber of a volcano?

The location beneath the vent of a volcano where molten rock (magma) is stored prior to eruption. Also known as a magma storage zone or magma reservoir.

What is a magma plume geography?

Magma plumes are areas of hot, upwelling mantle.

A hot spot develops above the plume in the crust. Magma generated by the hot spot rises through the rigid plates of the lithosphere and produces active low viscosity volcanoes at the Earth’s surface.

What are hotspots and mantle plumes?

A hot spot is an area on Earth that exists over a mantle plume. A mantle plume is an area under the rocky outer layer of Earth, called the crust, where magma is hotter than surrounding magma. … While most volcanoes form along tectonic plate boundaries, mantle plumes and hot spots lead to their development as well.

What forms on the surface of the plate when the lava erupts?

This molten rock can erupt when it reaches Earth’s surface. At convergent plate boundaries, one plate can be pushed under another plate. When this happens, the plate can melt and turn into magma. This molten rock can rise up to the surface, forming a volcano, and causing volcanic eruptions.

How magma is formed?

Magma forms from partial melting of mantle rocks. As the rocks move upward (or have water added to them), they start to melt a little bit. … Eventually the pressure from these bubbles is stronger than the surrounding solid rock and this surrounding rock fractures, allowing the magma to get to the surface.

What is molten magma?

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