sand dunes
sand dunes
Large underground lava deposits are called magma chambers. These chambers are reservoirs of molten rock beneath the Earth's surface that can feed volcanic eruptions when the magma rises to the surface through volcanic vents.
Deposits of very large boulders at random are called "erratics." These erratic boulders are typically transported by glacial movement and deposited in locations where they differ from the surrounding geology. They serve as indicators of past glacial activity and help geologists understand the history of glacial movements.
A landform created when a river reaches a large body of water and deposits sediments is called a delta. Deltas are typically triangular or fan-shaped and form where the river's velocity decreases, causing it to deposit the sediments it has been carrying.
Shield volcanoes are the type of volcano that forms large deposits of basalt often in smooth ropey formations called pahoehoe. Shield volcanoes have low viscosity magma that allows for the lava to flow more easily and create these distinct formations.
sand dunes
they are called layers
Ore
it has large deposits of it
Erratic blocks or "erratics" for short.
The types of wind deposits include dunes, loess deposits, and sand sheets. Dunes are mounds of sand shaped by wind, while loess deposits consist of fine-grained sediment deposited by wind. Sand sheets are large areas covered with wind-blown sand.
where are large deposits of salt found in rajasthan
Large underground lava deposits are called magma chambers. These chambers are reservoirs of molten rock beneath the Earth's surface that can feed volcanic eruptions when the magma rises to the surface through volcanic vents.
The thick wind-blown soil formed from the pulverization of rocks by glaciers is called "loess." This sediment consists of fine particles that are easily transported by wind and can accumulate in large deposits, often creating fertile agricultural land. Loess is typically rich in nutrients and has good drainage properties, making it valuable for farming.
Fine-grained wind-blown sediments, also known as loess, are deposits of silt-sized particles that have been transported and deposited by the wind. These sediments are typically unconsolidated and can form extensive and thick layers covering large areas. Loess deposits are common in arid and semi-arid regions and play a significant role in shaping landscapes and soil fertility.
large seeded grasses
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