subbduction zones
The relationship between depth and sunlight is that sunlight penetration decreases as depth increases in water. This is due to the absorption and scattering of light by water molecules and particles. Consequently, less sunlight reaches deeper parts of the water column, affecting the availability of light for photosynthesis and primary production.
pressure of liquid on bottom=density*gravitational force*depth :)
The Moho, or Mohorovičić discontinuity, is typically found at a depth of about 5-70 kilometers (3-43 miles) below the Earth's surface. It marks the boundary between the Earth's crust and the underlying mantle.
The boundary between the asthenosphere and the lithosphere is normally below the Moho (which marks the boundary between the crust and the mantle). The exception to this is below mid-ocean ridges where the moho and the lithosphere / asthenosphere boundary are at the same depth.
subbduction zones
A relationship that has "depth"?
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The relationship between water depth and pressure is linear. As water depth increases, the pressure exerted by the water also increases. This relationship is described by the hydrostatic pressure formula, which states that pressure is directly proportional to the depth of the fluid and the density of the fluid.
The relationship between underground temperature and depth is that the temperature increases as you go deeper underground. This is because the Earth's core is hot, and heat is transferred from the core to the surface.
The relationship between depth and sunlight is that sunlight penetration decreases as depth increases in water. This is due to the absorption and scattering of light by water molecules and particles. Consequently, less sunlight reaches deeper parts of the water column, affecting the availability of light for photosynthesis and primary production.
pressure of liquid on bottom=density*gravitational force*depth :)
As the depth increases, the density increases also.
the deeper you go, generally the colder it gets
Please see attached links.
No, the relationship between temperature and depth is primarily influenced by factors such as geothermal heat flux and thermal conductivity of the material, while pressure at depth is mainly dependent on the weight of overlying material. Temperature generally increases with depth due to geothermal heating, while pressure increases with depth due to the weight of the material above.
The pressure exerted by a fluid increases with depth due to the weight of the fluid above pushing down. This relationship is described by the hydrostatic pressure formula, which states that pressure is directly proportional to the depth of the fluid and the density of the fluid.