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Partial melting of a large region of anomalously hot, upwelling mantle is required to explain these huge volumes of pre- and syn-rift basaltic magma. The uplift associated with a shallow region of hot mantle is often invoked as a cause of the "rift-push" force that may drive the observed...
To answer this, we must go 200 million years in the past. When the supercontinent Pangea broke up into continents we have today, the rift between the Pacific and North American plates run roughly along what is today the US west coast. These two plates are still setting in, creatingmany fa...
The plates move towards one another and this movement can cause earthquakes. ... This happens becausethe oceanic plate is denser (heavier) than the continental plate. When the plate sinks into the mantle it melts to form magma. The pressure of the magma builds up beneath the Earth's surface...
Tectonic Plates: Tectonic plates are the independently moving pieces of the Earth's crust. When they collide, they can form mountains or push one of them down to form a subduction zone. When they spread apart, they create a rift for magma to rise and create new surface rock. ...
upon the migration of a magma batch: in these cases, strike-slip earthquakes can first be triggered along a zone of weakness ahead of the dike’s tip (Fig.2a, blue strike-slip mechanism) and then with reverse motions of the same structure when the dike grows or propagates forward (Fig....
Michon L, Ferrazini V, Di Muro A, Villeneuve N, Famin V (2015) Rift zones and magma plumbing system of Piton de la Fournaise: how do they differ from Hawaii and Etna? J Volcanol Geotherm Res 303:112-129Michon L, Ferrazzini V, Di Muro A, Villeneuve N, Famin V (2015) Rift zones...
Immersive virtual reality can potentially open up interesting geological sites to students, academics and others who may not have had the opportunity to visit such sites previously. We study how users perceive the usefulness of an immersive virtual reali