Cirrocumulus Clouds
Geology

Cirrocumulus Clouds

Cirrocumulus Clouds: Patchy white high altitude cloud composed of ice crystals. Found in an altitude range from 5.000 – 18.000 m. This happens because of…
Batholith
Geology

Batholith

Batholith: A large mass of subsurface intrusive igneous rock that has its origins from mantle magma. It is a very large igneous intrusion extending to…
Asthenosphere
Geology

Asthenosphere

Asthenosphere Zone in the Earth’s mantle that exhibits plastic properties. It is the upper layer of the earth’s mantle, below the lithosphere, in which there…
Caldera Volcano
Geology

Caldera Volcano

Caldera Volcano: A caldera is a volcanic feature formed by the collapse of a volcano into itself, making it a large, special form of volcanic…
Calcification
Geology

Calcification

Calcification: A dry environment soil-forming procedure that results in the accumulation of calcium carbonate in surface soil layers. It is a soil process in which…
Biome
Geology

Biome

The biome is a Largest recognizable assemblage of animals and plants on the Earth. The distribution of the biomes is controlled mainly by climate. A biome…
Bajada
Geology

Bajada

Bajada: Consecutive series of alluvial fans forming along the edge of a linear mountain range. The surface of this feature undulates in a rolling fashion…
Aurora
Geology

Aurora

Aurora: Multicolored lights that appear in the upper atmosphere (ionosphere) over the Polar Regions and visible from locations in the middle and high latitudes. It…
Atmospheric Pressure in Geography
Geology

Atmospheric Pressure in Geography

Atmospheric Pressure: Weight of the atmosphere on a surface. At sea-level, the average atmospheric pressure is 1013.25 mb. Pressure is measured by a device called…
Adiabatic Lapse Rate
Geology

Adiabatic Lapse Rate

Adiabatic Lapse Rate: It is the rate of change of temperature of an air parcel as it moves upwards through the atmosphere rapidly. The rate…
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