The consensus is that several factors are important: atmospheric composition (the concentrations of carbon dioxide, methane); changes in the Earth's orbit around the Sun known as Milankovitch cycles (and possibly the Sun's orbit around the galaxy); the motion of tectonic plates resulting in changes in the relative location and amount of continental and
oceanic crust on the Earth's surface, which could affect wind and ocean currents; variations in solar output; the orbital dynamics of the Earth - Moon system; and the impact of relatively large meteorites, and volcanism including eruptions of supervolcanoes.
The relatively low - density continental crust of the North Island, which sits on the Australian plate, is forcing the dense
oceanic crust on the Pacific plate beneath it in a process called subduction.
Not exact matches
Plate tectonics has shaped the Earth's surface for billions of years: Continents and
oceanic crust have pushed and pulled
on each other, continually rearranging the planet's façade.
Generally speaking, there are two types of
crust on Earth: a lighter continental
crust that is rich in silicon and constitutes the dry land above sea level, and a denser
oceanic crust where water gathers in the form of large oceans.
Its strength resulted from the abrupt release of plate tectonic forces, a process known as subduction, centered
on an area beneath Honshu where it slides over the top of
oceanic crust.
If the melt erupts quickly, it forms basalt, which makes up the
crust beneath the oceans
on Earth; but there are still questions about how continental
crust, which is more buoyant than
oceanic crust, is formed.
Sediment - covered basalt
on the flanks of mid-ocean ridges constitutes most of Earth's
oceanic crust, but the composition and metabolic function of its microbial ecosystem are largely unknown.
The northwest Pacific
crust that is subducting in this area is some of the oldest, coldest
oceanic crust subducting
on Earth.
As long as rapid continental weathering continued, carbonate was deposited
on the
oceanic crust and subducted into what Lowe calls «a big storage facility... that kept most of the carbon dioxide out of the atmosphere.»
Researchers from the Centre for Arctic Gas Hydrate, Environment and Climate (CAGE) at the Arctic University of Norway have discovered a growing Arctic abiotic methane - and methane hydrate — charged sediment drift
on oceanic crust in the deep Fram Strait of the Arctic Ocean.
While I'm comfortable with the heat flow measurements
on land, I doubt that the measurements of
oceanic crust are as reliable.