They should bring everything the person asked for and be on time.
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Relation between buoyancy, isostatic equilibrium, and epeirogenic processes</u></h2>
Buoyant force or buoyancy, is the force exerted in an object which is fully or partially occupied in a fluid. Isostatic equilibrium is the gravitational equilibrium between earth's crust and underlying mantle. while epeirogenic process is the depression of land having long wavelengths.
Both epeirogenic process and isostatic equilibrium uses the principle of buoyancy. The crust of the Earth or the lithosphere floats over underlying mantle at an elevation depending upon its density and thickness.
Answer:
geyser
Explanation:
The water feature shown by the image is a geyser.
Geyser are natural feature that ejects a column of hot water, steam or vapor into the atmosphere.
- Geysers are usually formed in areas of active volcanic and tectonic activities.
- When surface water comes in contact with a very hot body in formations, they become pressurized and rises up.
- They then become forcefully ejected through rock cavities and joints.
- This forced ejection leads to a head of water rising above the surrounding area.
Answer:
Porosity
Explanation:
Porosity is defined as the total percentage of pore spaces that are present within a rock. These spaces are found between the rock particles and fractures and are mostly filled with fluid mixture or water. It is the ratio between the total pore space in a rock to the total volume of the rock. It is mainly calculated in terms of percentage.
Porosity is directly affected by sorting. Well-sorted rocks indicate high porosity but poorly-sorted rocks indicate low porosity. Some of the examples of rocks exhibiting high porosity are limestone, shale, and sandstone. Rocks with low porosity include granite and mudstone.
