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- Zone of ablation is the area of a glacier where there is a net loss of ice due to melting, sublimation, and calving, while the zone of accumulation is the area where snowfall exceeds melting and forms new ice.
- In the zone of ablation, the glacier's terminus retreats, while in the zone of accumulation, the glacier advances.
- The zone of ablation typically occurs at lower elevations and is characterized by a negative mass balance, whereas the zone of accumulation is found at higher elevations with a positive mass balance.
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What factor accounts for most of the differences between three common types of soil pedalfer pedocal and laterite?
The main factor accounting for the differences between pedalfer, pedocal, and laterite soils is the varying climate conditions where they form. Pedalfers develop in humid regions with abundant rainfall and are rich in aluminum and iron oxides. Pedocals form in drier regions with more evaporation, leading to the accumulation of calcium carbonate. Laterite soils develop in hot and wet tropical climates with intense weathering, resulting in the leaching of nutrients and the formation of iron and aluminum compounds.
What are the 3 differences between cumulus and stratus clouds?
The three main differences between cumulus and stratus clouds are their appearance, altitude in the sky, and the type of weather they are associated with. Cumulus clouds are fluffy and puffy with distinct edges, found at lower altitudes, and often indicate fair weather. Stratus clouds are flat and layered, found at higher altitudes, and are associated with overcast or rainy conditions.
What are 3 things that affect surface ocean currents?
Wind, deflection from land, temperature differences between layers of cold and warm water.
What factor accounts for most of the differences between three common types of soil pedalfer pedoc and laterite?
The main factor that accounts for the differences between pedalfer, pedoc, and laterite soils is their composition and formation processes. Pedalfers are rich in iron and aluminum, forming in humid, temperate regions with well-drained soil. Pedocs are characterized by their calcareous content and form in semi-arid to arid regions. Laterite soils are highly weathered and rich in iron and aluminum oxides, forming in tropical regions with high rainfall and intense weathering.
What factor accounts for most of the differences between three common types of soil pedal fer pedocaland laterite?
Climate is the factor that accounts for most of the differences between pedocal, pedalfer, and laterite soils. Pedocal soils are found in arid or semi-arid climates, pedalfer soils are typical in humid climates with high rainfall, and laterite soils develop in humid tropical climates with intense weathering. These climate conditions influence the processes of soil formation and the dominant minerals present in each soil type.
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the all smell of poo
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differences between equator and prime meridian
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challa ki labda phire
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give three similarities and three difference between hire purchases and deferred payment
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give three differences between dew and rain
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I cannot answer this question.
What is the differences between the republic of Kenya the republic of South Africa and the republic of Sudan?
They are three different countries, so there would be massive differences between them, far too many to list.
Differences between BS 1387 and BS 4127?
three thousand two hundred sixty
Describe the three differences between com 1 port rs-232 and usb?
Monkey Butt
