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A resurgent stream is formed when an underground river is forced to reappear when it reaches a layer of impermeable bedrock. For a river to become an underground river in the first place it must flow over an area of limestone rock. The mildly acidified river water (it is acidified by dissolved carbon dioxide which is present in rainwater) reacts with the limestone (which is 80% calcium carbonate) and dissolves it. This forms a swallow hole into which the river flows. The river then continues to chemically weather the limestone underground thus forming an underground river. The river is forced to reappear (in the form of a resurgent stream) on the surface when there is a change of rock type from permeable limestone to impermeable bedrock. Hence resurgent streams are typically only found in limestone areas.

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Is there a layer of limestone at the bottom of a Kettle?

Kettles are glacial landforms that form when a block of ice is left behind by a retreating glacier and then melts. The presence of limestone at the bottom of a kettle would depend on the local geology of the area where the kettle formed. If the area has limestone deposits, it is possible for a kettle to have a layer of limestone at its bottom.


What do limestone deposits tell about there environment they were formed in?

Limestone deposits suggest that they were formed in a marine environment, typically in shallow, warm, and calm waters where the accumulation of calcium carbonate skeletons and shells of marine organisms was prevalent. The presence of fossils within limestone can indicate the past biodiversity and environmental conditions of the area where the deposits formed. Additionally, the purity and composition of the limestone can provide clues about the depositional processes and the source of the materials.


What type of bedrock most likely exists in an area that has numerous sinkholes?

Limestone bedrock is most likely to exist in an area with numerous sinkholes. Sinkholes are formed when acidic groundwater dissolves the limestone bedrock, creating underground cavities that can cause the land surface to collapse.


Where is an alluvial fan formed on dry land?

An alluvial fan is typically formed at the base of a mountain or hilly area where a river or stream exits a narrow canyon or valley, and the water carrying sediments spreads out onto a flatter, open area. The fan shape is created as the water slows down and deposits the sediment it was carrying.


What is The land form often formed at the mouth of a heavily silted stream called?

The land form often formed at the mouth of a heavily silted stream is called a delta. This triangular-shaped area is created as the sediment carried by the stream is deposited when the water flow slows down upon entering a larger body of water, such as an ocean or a lake. Deltas are often fertile areas due to the rich soil deposited by the stream.

Related Questions

Is there a layer of limestone at the bottom of a Kettle?

Kettles are glacial landforms that form when a block of ice is left behind by a retreating glacier and then melts. The presence of limestone at the bottom of a kettle would depend on the local geology of the area where the kettle formed. If the area has limestone deposits, it is possible for a kettle to have a layer of limestone at its bottom.


What type of rock is castleton built on?

Castleton is built on limestone, which is a sedimentary rock formed from the remains of marine organisms. Limestone is known for its durability and ease of shaping, making it a popular choice for construction in the area.


What do limestone deposits tell about there environment they were formed in?

Limestone deposits suggest that they were formed in a marine environment, typically in shallow, warm, and calm waters where the accumulation of calcium carbonate skeletons and shells of marine organisms was prevalent. The presence of fossils within limestone can indicate the past biodiversity and environmental conditions of the area where the deposits formed. Additionally, the purity and composition of the limestone can provide clues about the depositional processes and the source of the materials.


What is the area where a freshwater river or stream enters the ocean?

The area where a freshwater river or stream enters the ocean is called an estuary. It is a coastal area of brackish water formed when freshwater enters the ocean.


What is an area of exposed limestone known as?

Limestone soil is the soil created by the gradual breakdown of rocky limestone banks and outcroppings into a highly alkaline soil. Most plants typically do not grow well in limestone soil, but there are a few which do well.


What type of bedrock most likely exists in an area that has numerous sinkholes?

Limestone bedrock is most likely to exist in an area with numerous sinkholes. Sinkholes are formed when acidic groundwater dissolves the limestone bedrock, creating underground cavities that can cause the land surface to collapse.


Where is an alluvial fan formed on dry land?

An alluvial fan is typically formed at the base of a mountain or hilly area where a river or stream exits a narrow canyon or valley, and the water carrying sediments spreads out onto a flatter, open area. The fan shape is created as the water slows down and deposits the sediment it was carrying.


What is responsible for rock formation?

Gypsum is formed underwater, usually between layers of shale and limestone. When the water evaporates and the area dries, the gypsum becomes solid "rock" gypsum.


What is the name of the area from which limestone is extracted?

quarry


What is The land form often formed at the mouth of a heavily silted stream called?

The land form often formed at the mouth of a heavily silted stream is called a delta. This triangular-shaped area is created as the sediment carried by the stream is deposited when the water flow slows down upon entering a larger body of water, such as an ocean or a lake. Deltas are often fertile areas due to the rich soil deposited by the stream.


Which of these landforms is characteristic of an area with karst topography?

Sinkholes are characteristic of an area with karst topography. Karst topography is formed by the dissolution of soluble rocks like limestone, creating unique landforms such as sinkholes, caves, and disappearing streams.


What formation is responsible for rock gypsum?

Gypsum is formed underwater, usually between layers of shale and limestone. When the water evaporates and the area dries, the gypsum becomes solid "rock" gypsum.