crust
it's mantle
it's mantle
Mantle.Earth's largest layer is the mantle.
It depends on the surface status of the silicon. Bare silicon surface without any chemical termination is 'hydrophobic'. But this is very unstable status and it is very easily oxidized forming native SiO2 layer in the air which is 'hydrophilic'. Chemical treatment to make silicon surface hydrogen terminated will make it hydrophobic; while surface with OH termination will make it hydrophilic.
about 30km-40km on the continental crust and about 10km on oceanic.Depth varies with location.
it's mantle
it's mantle
Oceanic crust.
Mantle.Earth's largest layer is the mantle.
The surface of the moon is primarily made of rocky material, specifically a type of rock called basalt. It also contains other elements and minerals such as silicon, iron, magnesium, and calcium. The surface is covered in a layer of dust and rocky debris called regolith.
The surface of the moon is characterized by impact craters, their ejecta, volcanoes, hills, lava flows and depressions filled with magma. Known elements to be present on the surface are oxygen, silicon, iron, magnesium, calcium, aluminum, manganese and titanium.
43% of lunar soil is oxygen, 21% silicon, 13% iron, 8% calcium, 6% aluminum, 5% magnesium, and 4% other elements...
Nunavut has the largest surface area, but it also composed of islands. As far as "solid" land mass, it would probably be Quebec.
By mass, the Earth is composed of mostly iron (35 percent), oxygen (30 percent), silicon (15 percent), and magnesium (13 percent). It is made of distinct layers: a thin crust, upper mantle, lower mantle, outer core, and inner core, as well as transition zones. The crust is thinner under the oceans but thicker under the continents. While the inner core and crust are solid, the outer core and mantle layers are semi-fluid. Most of the mass of the Earth is in the mantle, which is mostly made of the minerals olivene and pyroxene (iron and magnesium silicates). The elements calcium and aluminum are abundant in the upper mantle and while silicon, magnesium, and oxygen are major components of the lower mantle. The core is probably composed mostly of iron (perhaps with some nickel), where the temperature may be as high as 7227 °C (13,040 °F) at the center -- which is hotter than the surface of the Sun
It depends on the surface status of the silicon. Bare silicon surface without any chemical termination is 'hydrophobic'. But this is very unstable status and it is very easily oxidized forming native SiO2 layer in the air which is 'hydrophilic'. Chemical treatment to make silicon surface hydrogen terminated will make it hydrophobic; while surface with OH termination will make it hydrophilic.
The Earth is rocky, mainly iron, oxygen, silicon and magnesium, still molten internally, a thin atmosphere largely of nitrogen and oxygen, and liquid water oceans over two thirds of its surface.
This has many answers, like there's molten rock which we call "magma" under the earth. Then there is Sima- silicon and magnesium and Sial- silicon and aluminum and Nife- nickel and ferrum(iron) together. Mostly there is aluminum in the rocks below the crust.