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features that are created when water dissolves surface and subsurface limestone

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Features That Are Created When Water Dissolves Surface And Subsurface Limestone?

Features that are created when water dissolves surface and subsurface limestone, like sinkholes, troughs, caverns, natural bridges, and towers, are collectively called: karst landscapes.

Which feature is created from water dissolving bedrock?

Sinkholes. A sinkhole is a depression or hole formed when the land surface sinks due to underground bedrock dissolution or cave collapse.

What is the progressive development of a meander?

This figure shows the progressive development of a meander in a river system. What feature is created in the fourth panel? Oxbow lake;FEEDBACK: Meanders grow further and further outward until the neck is cut by erosion. At this point, the meander becomes abandoned, leaving behind an oxbow lake.

Which of the following statements about the water table is false group of answer choices?

B. the water table is generally flat is the false statement.. Water table is defined as the level of ground below which the area is saturated with water. Water table is not flat but the shape depends on the topology of surface of ground, weather, geology and use of land.

What is the term for the percentage of empty space in sediment or rock that can store water?

porosity. the percentage of the total volume of a rock or sediment that consists of open spaces. Only $47.88/year. permeability. the ability of a rock or sediment to let fluids pass through its open spaces or pores.

How caves and features such as stalactites stalagmites and sink holes form in limestone regions?

Caves often form in limestone areas when underground water dissolves the rock, forming tunnels passages and even large caverns. … Many interesting limestone features can be found within limestone caves. Some common ones are stalactites, stalagmites and pillars.

Where a stream emerges from the limestone?

Karst springs are locations where groundwater emerges from the limestone and flows across the surface forming a stream or contained pool. The flow of Karst springs is generally dependant on the weather and climate.

What causes meandering?

Meanders are produced when water in the stream channel erodes the sediments of an outer bend of a streambank and deposits this and other sediment on subsequent inner bends downstream. … Eventually, the meander may be cut off from the main channel, forming an oxbow lake.

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Which is the primary cause of meandering as per the latest accepted theory behind meandering?

presence of an excessive bed slope in the river.

What is the term for the land area drained by all of the streams that empty into a tributary?

A watershed, also called a drainage basin or catchment, is an area drained by a river and its tributaries.

Which source of water among the following is not a subsurface source?

The storage reservoir is the source of water that is not a sub-surface.

How does the water table change around a pumping water well how does the water table change around a pumping water well?

Groundwater moves over larger distances, over longer timescales. How does the water table change around a pumping water well? The water table elevation decreases. What is the cone of depression?

What causes water to eject from a geyser?

In geysers the superheated water collects in underground pockets. There a small drop in pressure caused by the release of water at the surface flashes the superheated water into steam, which expands and ejects a column of steam and water into the air.

What affects the permeability of subsurface earth materials?

Permeability is affected mostly by the size and arrangement of the grains in the soil. As rain and runoff enter the soil the water begins to fill the pore spaces in the ground. The water will continue to work its way down until it accumulates above an impermeable layer (bedrock).

What characteristics of limestone make it a good groundwater subsurface aquifer?

The cracks and joints in limestone are generally made as the rock slowly dissolves in slightly acidic water, leaving places for groundwater to flow. Sometimes caverns are formed that hold water and extend for thousands of feet.

What are the two features of a good aquifer?

Aquifers must be both permeable and porous and include such rock types as sandstone, conglomerate, fractured limestone and unconsolidated sand and gravel.

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How do the interesting features like stalactites form?

As the redeposited minerals build up after countless water drops, a stalactite is formed. If the water that drops to the floor of the cave still has some dissolved calcite in it, it can deposit more dissolved calcite there, forming a stalagmite. Speleothems form at varying rates as calcite crystals build up.

What feature is formed when the roof of an underground cave collapses?

Sinkholes occur naturally, especially where there is abundant rainfall, and the rock beneath the surface soil is limestone. For instance, a cenote (pronounced “seh-NOH-tay”) is a type of sinkhole that forms when the roof of an underground cave collapses, exposing the water to the surface.

What type of weathering occurs when stalactites and stalagmites on caves are formed?

Stalactites and stalagmites are formed by chemical weathering. Water dissolves the calcites in the rock of a cave roof and the calcite is deposited as strange and wonderful structures below.

Which of the following features are commonly found in karst landscapes?

karst, terrain usually characterized by barren, rocky ground, caves, sinkholes, underground rivers, and the absence of surface streams and lakes. It results from the excavating effects of underground water on massive soluble limestone.

What reactions that occur with water help create features of karst topography?

Rainwater dissolves the limestone by the following reaction: Calcite + Carbonic acid = Calcium ions dissolved in ground water + Bicarbonate ions dissolved in ground water.

Which of the following features commonly result from the collapse of underground limestone caverns?

Collapse sinkholes develop by the collapse of surface or near-surface material into an underground cavern. As subsidence features, these sinkholes can develop into spectacular structures.

How are the features of a meander formed?

The formation of a meander. As the river erodes laterally, to the right side then the left side, it forms large bends, and then horseshoe-like loops called meanders . … The force of the water erodes and undercuts the river bank on the outside of the bend where water flow has most energy due to decreased friction.

What feature is formed when sediment cuts off the neck of a meander?

oxbow lake, small lake located in an abandoned meander loop of a river channel. It is generally formed as a river cuts through a meander neck to shorten its course, causes the old channel to be rapidly blocked off, and then migrates away from the lake.

Which feature is associated with the meandering of a river?

A meandering stream has a single channel that winds snakelike through its valley, so that the distance ‘as the stream flows’ is greater than ‘as the crow flies. ‘ As water flows around these curves, the outer edge of water is moving faster than the inner.

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Which of the following is a characteristic that applies to a meandering stream?

Which of the following features characterize meandering streams? They have channels that are very curved, commonly forming tight loops.

What is river meandering phenomenon describe on the causes of meandering and factors controlling the meandering process?

Rivers flowing over gently sloping ground begin to curve back and forth across the landscape. These are called meandering rivers. from the outer curve of each meander bend and deposit it on an inner curve further down stream. This causes individual meanders to grow larger and larger over time.

What is the primary cause of meandering?

Main cause is Extra turbulence generated by the excess of river sediment during floods.

What three factors describe the movement of surface water in streams and rivers?

The stream or river’s gradient, flow, and stream load are three factors that describe the movement of surface water.

What are the characteristics of a river basin?

River basins have typical features, these include: Tributaries – smaller rivers flowing into a larger river. A Watershed – an area of highland surrounding the river basin. A confluence – where a river joins another river.

What are the characteristics of watershed?

Characteristics of Watersheds. A watershed is an area of land that forms the drainage system for a stream or river. This area collects surface water from land within specific topographic boundaries (such as hills, valleys, mountains, and other landscape characteristics).

What are the subsurface sources of water?

subsurface, underground water can be made available for use.

In this category the following sources can be listed:
  • Open Wells: …
  • Tube Wells: …
  • Artesian Wells: …
  • Infiltration Gallery: …
  • Infiltration Wells:

What is subsurface water?

Subsurface water – liquid water found below the ground surface, including soil water above the water table and ground water below the water table, but does not include water chemically bound to minerals or organic matter.

Which source of water among the following is a sub surface source?

groundwater, water that occurs below the surface of Earth, where it occupies all or part of the void spaces in soils or geologic strata. It is also called subsurface water to distinguish it from surface water, which is found in large bodies like the oceans or lakes or which flows overland in streams.

Formation of Karst Landscapes

How Groundwater Moves in the Karst Landscape (A Short Animation)

Karst Landscape: The Chemical Weathering of Limestone Features

Limestone Cave Formations

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