Here is a list of subtopics without any description for Radial Drainage Pattern:
- Radial drainage pattern
- Drainage pattern
- Drainage basin
- Stream
- River
- Tributary
- Meander
- Delta
- Alluvial fan
- Ephemeral stream
- Permanent stream
- Headwater stream
- Trunk stream
- Distributary
- Confluence
- Mouth
- Watershed
- Catchment area
- Drainage divide
- Water table
- Aquifer
- Groundwater
- Spring
- Geyser
- Karst topography
- DolineDoline
- Sinkhole
- Uvala
- Polje
- Cave
- Fluvial landform
- Alluvial landform
- Glacial landform
- Aeolian landform
- Karst landform
- Coastal landform
- Volcanic landform
- Tectonic landform
A radial drainage pattern is a type of drainage pattern in which streams radiate outward from a central point, such as a mountain peak or volcano. This type of drainage pattern is common in areas with hilly or mountainous terrain.
The radial drainage pattern is formed when PrecipitationPrecipitation falls on the slopes of a mountain and then flows downhill in all directions. The streams that form in this way eventually converge at the base of the mountain, where they may join a larger river or flow into a lake.
The radial drainage pattern is a common type of drainage pattern in many parts of the world, including the Rocky Mountains, the Andes Mountains, and the Alps. It is also found in some volcanic areas, such as Hawaii and Iceland.
The radial drainage pattern has a number of distinctive features. One of the most obvious features is that the streams radiate outward from a central point. This is in contrast to other types of drainage patterns, such as the Dendritic Drainage Pattern, in which the streams branch off from each other in a more complex way.
Another distinctive feature of the radial drainage pattern is that the streams are often short and steep. This is because the streams have to flow downhill over a short distance in order to reach the base of the mountain.
The radial drainage pattern also has a number of implications for the landscape. One of the most important implications is that the streams can cause erosion. The streams are often very powerful, and they can carry away large amounts of SoilSoil and rock. This can lead to the formation of gullies and other features on the landscape.
The radial drainage pattern can also affect the climate of an area. The streams can help to regulate the temperature of the air, and they can also provide a source of water for plants and animals.
Overall, the radial drainage pattern is a common and important type of drainage pattern. It is found in many parts of the world, and it has a number of distinctive features. The radial drainage pattern can also have a number of implications for the landscape and the climate.
Here are some additional details about the subtopics listed above:
- Drainage pattern: A drainage pattern is the way in which streams and rivers flow over the land. There are many different types of drainage patterns, including radial, dendritic, parallel, and trellis.
- Drainage basin: A drainage basin is an area of land that is drained by a single stream or river. The boundaries of a drainage basin are defined by the watershed, which is the line that separates two drainage basins.
- Stream: A stream is a body of water that flows over the land. Streams are usually smaller than rivers, and they often have a more winding course.
- River: A river is a large body of water that flows over the land. Rivers are usually longer than streams, and they often have a more direct course.
- Tributary: A tributary is a stream that flows into a larger stream or river. Tributaries are often named after the larger stream or river that they flow into.
- Meander: A meander is a curve in a stream or river. Meanders are often caused by the erosion of the streambed by the flowing water.
- Delta: A delta is a fan-shaped deposit of sediment that forms at the mouth of a river. Deltas are formed when the river slows down as it reaches the ocean, and the sediment that it carries is deposited.
- Alluvial fan: An alluvial fan is a fan-shaped deposit of sediment that forms when a stream flows out of a narrow canyon onto a plain. Alluvial fans are often found in arid and semi-arid regions.
- Ephemeral stream: An ephemeral stream is a stream that flows only during periods of heavy rainfall. Ephemeral streams are common in arid and semi-arid regions.
- Permanent stream: A permanent stream is a stream that flows year-round. Permanent streams are common in humid regions.
- Headwater stream: A headwater stream is a small stream that flows from a spring or a melting glacier. Headwater streams are often the source of larger streams and rivers.
- Trunk stream: A trunk stream is a large stream that is formed by the confluence of two or more headwater streams. Trunk streams are often the main channel of a river.
- Distributary: A distributary is a stream that flows away from the main channel of a river. Distributaries are often formed when a river divides into two or more channels.
- Confluence: A confluence is the point where two or more streams meet. Confluences are often important landmarks, as they can be used to navigate rivers.
- Mouth: The mouth of a river is the point where it flows into another body of water, such as an ocean, lake, or another river. The mouth of a river is often an important location for shipping and commerce.
- Watershed:
Radial drainage pattern
A radial drainage pattern is a type of drainage pattern in which streams radiate outward from a central point, such as a mountain peak. This type of drainage pattern is common in areas with hilly or mountainous terrain.
Drainage pattern
A drainage pattern is the way in which streams and rivers flow over the land. The shape of a drainage pattern is determined by the underlying geology, topography, and climate.
Drainage basin
A drainage basin is an area of land that is drained by a single stream or river. The boundary of a drainage basin is called the drainage divide.
Stream
A stream is a body of water that flows in a channel on the surface of the Earth. Streams are usually smaller than rivers, but they can be larger in some cases.
River
A river is a large natural stream of water flowing in a channel to the sea, a lake, or another river. Rivers are usually larger than streams, but they can be smaller in some cases.
Tributary
A tributary is a stream or river that flows into a larger stream or river. Tributaries are usually smaller than the stream or river they flow into, but they can be larger in some cases.
Meander
A meander is a bend in a river. Meanders are caused by the erosion of the riverbank on the outside of the bend and the deposition of sediment on the inside of the bend.
Delta
A delta is a fan-shaped deposit of sediment that forms at the mouth of a river. Deltas are formed when the river slows down and drops its sediment load.
Alluvial fan
An alluvial fan is a fan-shaped deposit of sediment that forms when a stream or river flows out of a narrow canyon onto a plain. Alluvial fans are formed when the stream or river slows down and drops its sediment load.
Ephemeral stream
An ephemeral stream is a stream that flows only during periods of heavy rainfall. Ephemeral streams are common in arid and semi-arid regions.
Permanent stream
A permanent stream is a stream that flows year-round. Permanent streams are common in humid regions.
Headwater stream
A headwater stream is a small stream that flows from a spring or a mountain. Headwater streams are the source of larger streams and rivers.
Trunk stream
A trunk stream is a large stream that is formed by the confluence of two or more headwater streams. Trunk streams are the main channels of larger rivers.
Distributary
A distributary is a stream that flows away from the main channel of a river. Distributaries are formed when a river splits into two or more channels.
Confluence
A confluence is the point where two or more streams meet to form a larger stream.
Mouth
The mouth of a river is the point where it flows into a lake, the ocean, or another river.
Watershed
A watershed is an area of land that drains into a single stream or river. The boundary of a watershed is called the drainage divide.
Catchment area
A catchment area is the same as a watershed.
Drainage divide
The drainage divide is the boundary between two watersheds. The drainage divide is usually a ridge or mountain range.
Water table
The water table is the upper surface of the groundwater. The water table is usually at the level where the ground is saturated with water.
Aquifer
An aquifer is a layer of rock or sediment that can store groundwater. Aquifers are usually found in porous rock or sediment.
Groundwater
Groundwater is water that is stored in the ground. Groundwater is usually found in aquifers.
Spring
A spring is a place where groundwater flows out of the ground. Springs are usually found where the water table is close to the surface.
Geyser
A geyser is a hot spring that erupts periodically. Geysers are formed when groundwater is heated by magma or hot rocks.
Karst topography
Karst topography is a type of topography that is characterized by SinkholesSinkholes, caves, and underground Drainage Systems. Karst topography is formed when limestone or dolomite rock is dissolved by groundwater.
Doline
A doline is a type of sinkhole that is formed when limestone or dolomite rock is dissolved by groundwater. Dolines are usually small, but they can be large in some cases.
Sinkhole
A sinkhole is a hole in the ground that is formed when limestone or dolomite rock is dissolved by
1. Which of the following is a drainage pattern that forms in a cone-shaped landform with streams radiating from a central point?
(A) Radial drainage pattern
(B) Dendritic drainage pattern
(CC) Trellis Drainage Pattern
(D) Parallel Drainage Pattern
A drainage basin is:
(A) The area of land that drains into a stream or river.
(B) The area of land that is covered by water.
(C) The area of land that is not covered by water.
(D) The area of land that is used for agriculture.A stream is:
(A) A body of water that flows over the surface of the land.
(B) A body of water that flows underground.
(C) A body of water that is frozen.
(D) A body of water that is not moving.A river is:
(A) A large stream.
(B) A small stream.
(C) A stream that flows into a lake.
(D) A stream that flows into the ocean.A tributary is:
(A) A stream that flows into a larger stream.
(B) A stream that flows out of a larger stream.
(C) A stream that flows into a lake.
(D) A stream that flows into the ocean.A meander is:
(A) A curve in a stream.
(B) A straight section of a stream.
(C) A waterfall.
(D) A rapid.A delta is:
(A) A fan-shaped deposit of sediment at the mouth of a river.
(B) A triangular deposit of sediment at the mouth of a river.
(C) A crescent-shaped deposit of sediment at the mouth of a river.
(D) A straight deposit of sediment at the mouth of a river.An alluvial fan is:
(A) A fan-shaped deposit of sediment at the foot of a mountain.
(B) A triangular deposit of sediment at the foot of a mountain.
(C) A crescent-shaped deposit of sediment at the foot of a mountain.
(D) A straight deposit of sediment at the foot of a mountain.An ephemeral stream is:
(A) A stream that flows only during the rainy season.
(B) A stream that flows all year round.
(C) A stream that flows only during the winter.
(D) A stream that flows only during the summer.A permanent stream is:
(A) A stream that flows only during the rainy season.
(B) A stream that flows all year round.
(C) A stream that flows only during the winter.
(D) A stream that flows only during the summer.A headwater stream is:
(A) A stream that is located at the head of a drainage basin.
(B) A stream that is located at the mouth of a drainage basin.
(C) A stream that is located in the middle of a drainage basin.
(D) A stream that is located at the end of a drainage basin.A trunk stream is:
(A) The largest stream in a drainage basin.
(B) The smallest stream in a drainage basin.
(C) The middle-sized stream in a drainage basin.
(D) The stream that flows into the ocean.A distributary is:
(A) A stream that flows out of a lake.
(B) A stream that flows into a lake.
(C) A stream that flows into a river.
(D) A stream that flows out of a river.A confluence is:
(A) The point where two streams meet.
(B) The point where a stream meets the ocean.
(C) The point where a stream meets a lake.
(D) The point where a stream meets a glacier.A mouth is:
(A) The point where a stream meets the ocean.
(B) The point where a stream meets a lake.
(C) The point where a stream meets a glacier.
(D) The point where a stream meets another stream.A watershed is:
(A) The area of land that drains into a stream or river.
(B) The area of land that is covered by water.
(C) The area of land that is not covered by water.
(D) The area of land that is used for agriculture.A catchment area is:
(A) The area of land that