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Divergent boundaries by submarine eruptions and intrusions of rhyolitic magma will form new crusts of the ocean. This commonly takes place in the hydrosphere.
Beneath the Earth's crust is a lot of magma. Thus as the plates pull apart, it leaves a gap through which the magma can travel and erupt as lava. For example at the Mid Atlantic Ridge, there are divergent plate boundaries. The 'gap' between the divorcing plates allows magma to boil through, building up the ridge in the process.
decompression melting
Divergent boundaries form ocean ridges.
There are two places that divergent boundaries occur. Under the sea where magma pushes up to form lava ridges and at the divergence at the Red Sea near the Suez canal.
Divergent boundaries by submarine eruptions and intrusions of rhyolitic magma will form new crusts of the ocean. This commonly takes place in the hydrosphere.
Beneath the Earth's crust is a lot of magma. Thus as the plates pull apart, it leaves a gap through which the magma can travel and erupt as lava. For example at the Mid Atlantic Ridge, there are divergent plate boundaries. The 'gap' between the divorcing plates allows magma to boil through, building up the ridge in the process.
divergent boundaries
Plates are moved at a divergent boundary by the magma pushing upwards.
decompression melting
divergent boundaries happen when 2 plates move apart or divide
At divergent boundaries, two plates move apart from each other and the space that this creates is filled with new crustal material sourced from molten magma that forms below.
Usually a dense basaltic magma with low water content.
Divergent boundaries form ocean ridges.
There are two places that divergent boundaries occur. Under the sea where magma pushes up to form lava ridges and at the divergence at the Red Sea near the Suez canal.
Hot mantle rock rises to fill rift zones. When rock rises, a decrease in pressure causes hot mantle rock to melt and form magma.
At divergent boundaries, two plates move apart from each other and the space that this creates is filled with new crustal material sourced from molten magma that forms below.