WebA novel method of exploring the uppermost few hundred kilometres of the Earth was proposed in 2005, consisting of a small, dense, heat-generating probe which melts its … WebMantle convection is the main way heat from Earth’s interior is transported to its surface, and this heat escapes principally through mid-ocean ridges. In fact, the connected mid-ocean ridge system is in essence a 80,000 km long volcano. Escaping heat along these ridges causes hot water to circulate through the crust in a “hydrothermal ...
Plate tectonics - Seafloor spreading Britannica
WebJul 27, 2024 · Continental crust is less dense than oceanic crust and does not get forced into the mantle. The crumpling of the continental crust is similar to two cars colliding, as … WebAnswer (1 of 6): Is it true that convection only moves in oceanic crust? Not true. Convection occurs in fluids or semi-fluids. The oceanic crust is solid. It does not flow like a fluid under convection. The fact is that the oceanic crust is carried along on mantle convection cells, much like ... jasper ga zip code and county
The deepest hole we have ever dug - BBC Future
Webwarm mantle material sinks, cools, and eventually rises upb. cool mantle material sinks, heats up, and eventually rises upc. cool mantle material rises, heats up, and eventually sinks downd. warm mantle material rises and eventually breaks out to the crust Answer: b. Explanation: The mantle is heated from below (the core), and in areas that are ... WebAnswer (1 of 4): Well, without the material diving back into the mantle at the seams, where would the material come from to make more crust ? After all, the planet certainly won’t be getting any bigger and it’s a zero-sum game. It seems like the only alternative is to collapse the continents, eve... Subduction zones are important for several reasons: • Subduction zone physics: Sinking of the oceanic lithosphere (sediments, crust, mantle), by the contrast of density between the cold and old lithosphere and the hot asthenospheric mantle wedge, is the strongest force (but not the only one) needed to drive plate motion and is the dominant mode of mantle convection. jasper goldberg scoring scale