Erosional features in areas with valley glaciers include U-shaped valleys, cirques (bowl-shaped hollows at the head of glaciers), arêtes (sharp ridge between cirques), and hanging valleys (smaller valleys that join a main glacier valley). Glacial striations (scratches on bedrock caused by moving glacier ice) and moraines (piles of debris deposited by glaciers) are also common erosional features.
A canyon is a landform that is created by erosional forces. Erosion, caused by wind or water, gradually wears away the Earth's surface, carving out deep valleys and creating steep cliffs. Canyons are often found in areas with flowing water, such as rivers or streams.
A landform not common in karst topography is typically a flat plain or plateau. Karst topography is known for its distinctive features such as sinkholes, caves, and disappearing streams, which are caused by the dissolution of soluble rocks like limestone. Flat plains or plateaus are less likely to form in karst areas due to the erosional processes that create the unique karst features.
There are three types of uplift: tectonic uplift caused by movement of tectonic plates, isostatic uplift due to changes in the earth's crustal thickness and density, and erosional uplift caused by erosion stripping away material and uplifting the remaining land.
Plate tectonics
Erosional plains are developments on the Earth's surface caused by natural weathering of glacier activity, wind movement or water (sea, river & stream) torrent and are subdivided on the basis of the type of erosional agent.
Erosional features in areas with valley glaciers include U-shaped valleys, cirques (bowl-shaped hollows at the head of glaciers), arêtes (sharp ridge between cirques), and hanging valleys (smaller valleys that join a main glacier valley). Glacial striations (scratches on bedrock caused by moving glacier ice) and moraines (piles of debris deposited by glaciers) are also common erosional features.
Striation is typically erosional. Striations are long, narrow lines or grooves on a rock surface caused by the movement of a glacier, which acts as a powerful scouring tool that can scrape and polish the bedrock beneath it as it flows.
Desalination plants are not a major source of groundwater pollution. Groundwater pollution is typically caused by activities such as industrial discharges, agriculture runoff, and leaks from underground storage tanks.
Valleys on the surface of a planet or moon suggest the presence of erosional processes, possibly caused by the flow of water, glaciers, or wind. These landforms can provide clues about the planet's geological history and past environmental conditions.
sinking and compaction of the land
ecology
The cone of depression near the well is likely caused by pumping water out of the well faster than the groundwater can naturally replenish itself. This leads to a decrease in water levels around the well, creating a cone-shaped depression.
A canyon is a landform that is created by erosional forces. Erosion, caused by wind or water, gradually wears away the Earth's surface, carving out deep valleys and creating steep cliffs. Canyons are often found in areas with flowing water, such as rivers or streams.
Groundwater contamination is a significant issue, often caused by industrial activities, agriculture, and improper waste disposal. Over-pumping of groundwater can lead to land subsidence and saltwater intrusion in coastal areas. Contaminated groundwater can also pose health risks to humans and ecosystems.
A landform not common in karst topography is typically a flat plain or plateau. Karst topography is known for its distinctive features such as sinkholes, caves, and disappearing streams, which are caused by the dissolution of soluble rocks like limestone. Flat plains or plateaus are less likely to form in karst areas due to the erosional processes that create the unique karst features.
Cholera & Typhoid fever would be two of the more common, but there are many more