Sunday, February 5, 2023
Home NEW Flow Patterns – Dendritic, Radial, Rectangular and Trellis

Flow Patterns – Dendritic, Radial, Rectangular and Trellis

River Flow Pattern – We need to know that there are kinds and forms of river flow patterns, where later it will be seen how the river flows or where the river water flows which in the end will all end up in the sea.

There are several types of river flow patterns, among them Dendritic, Radial, Rectanguler, Trellis, Parallel, Annular, multi-basinal or Sink Hole, Contorted and other sub-flow patterns which we will discuss below.

Understanding River Flow Patterns

River Flow Pattern

The water in its motion will always erode earthresulting in the formation of basins where water is taken up by small or large channels, usually referred to as flow channels or bodies (Sandy, 1985).

These waterways (small and large) meet and form specific flow patterns that are influenced by factors rock and morphologically (Barstra, 1982, Thornbury, 1954).

River flow pattern is a group of rivers with the same shape that can describe the state of the profile and genetics of the river (Sandy, 1985 and Katili, 1950; Lobeck, 1939).

From this definition it can be seen that flow patterns are influenced by, among others, morphology, rock constituents, erosion and geological structures.

Types of Flow Patterns

Types of Flow Patterns
Flow Pattern Type

The difference in flow patterns from one area to another is largely determined by differences in the trend, topography, structure, and lithology of the bedrock. In general, the known streaming patterns are as follows:

Dendritic Stream

Dendritic
Dendritic

The first flow flow pattern is the flow flow pattern dendritic. If we look at the cross section of a leaf with its veins, we will see this flow pattern. Yes, this dendritic flow pattern is similar to the cross section of a leaf.

So we will see that this main river has branches flowing in all directions. In general, the flow pattern of such a flow is controlled by the different lithology homogeneous. This flow pattern has a flow structure that is controlled by rock type.

Dendritic flow pattern is a flow pattern with flow branches that resemble lines in the cross section of the leaf. In general, this flow pattern is controlled by a homogeneous lithology. This flow pattern has a flow structure (flux density) which is controlled by rock type. The flow texture is defined as the flow length per unit area.

For example, a stream flowing over erosion-resistant rock forms a dense flow structure. Resistant rock (such as granite) forms a smooth texture. Rock resistance to erosion has a major impact on the formation of river basins. Unstable rock can easily erode and form flow channels.

This flow texture is defined as the flow length per unit area. For example, flow that propagates in rock that is less resistant to erosion forms a dense flow structure, while rock that is erosion resistant forms a smooth flow structure.

The resistance of rocks to erosion significantly affects the process of forming river basins, that is, non-resistant rocks tend to be eroded more easily and form flow channels.

Radial River Flow

Radial
Radial

The next type of flow flow pattern is the radial flow flow pattern. As the name suggests, a radial flow pattern is a flow pattern that propagates in all directions.

So that the river that has a river pattern has a center that spreads the river in all directions. An example is the eye air mountains that spread water in all directions.

A radial flow pattern is a flow flow pattern in which the flow direction is distributed radially from a certain elevation point, e.g. B. the peak of the volcano or the peak of the theft of magma.

This pattern is formed after the formation of the convex surface of the earth, which is the origin of the resulting flow. This radial flow pattern is also found in domes and laccoliths. In this type of landscape, the flow flow pattern may be a combination of radial and annular patterns.

Another example that follows a radial flow pattern is a crater/magma on top of a mountain. This magma pattern appears after the formation of the convex surface of the earth, which is the origin of the resulting flow. Radial flow patterns can also be found in the shape of a dome.

Centripetal Radial Flow

Centripetal
Centripetal

The next flow pattern is the centripetal radial flow pattern. This flow pattern is called radial, except that it is also centripetral. Despite the same name, this flow pattern is the opposite of the radial flow pattern.

In radial flow flow, when the spring is completely convex flowing in all directions, the spring actually goes in one direction in this centripetal radial direction.

The centripetal radial pattern is the opposite pattern to the radial pattern. In this pattern, the river usually flows into a large (lower) basin. This flow pattern is mainly found in the western and northwestern United States.

Therefore it can be said that the flow pattern in this redial flows to a certain point, for example to a large basin or well. Areas commonly found in such rivers are typically located in the western and northwestern United States.

This flow pattern can develop into an annular pattern. The annular shaped pattern itself is a pattern that is initially a radial stripetal flow, but then a sub-sequence river, an obse- quent river, which is parallel as well as a successive river. and subsequent flows.

Rectangular River Flow

Rectanguler
Rectanguler

In general, flow with a rectangular flow pattern is controlled by geological structures such as fault and fault structures. Rivers with rectangular flow patterns usually appear in magmatic rock structures.

The rectangular flow pattern is usually formed in the direction of the fault. The characteristics of rivers with this flow pattern are the vertical shape of the river and a collection of waterways that follow the pattern of geological structures.

This rectangular flow pattern is generally formed in erosion-resistant rocks whose species are almost uniform, but are controlled by two directions that are interrupted at normal angles. Flow branches that have this flow generally form an obtuse angle with the main stream or main stream.

This pattern generally occurs in igneous rocks, usually in a straight line following a fault structure and characterized by river shapes that are perpendicular to each other. The rectangular pattern generally occurs in erosion-resistant rocks, with a nearly uniform type of erosion, but controlled by bilateral bending at right angles to each other.

Stumps are generally less resistant to erosion, so it is very possible for water to flow and develop through the fracture which eventually forms a drainage pattern that follows the muscles. Rectangular flow patterns can be found in the most elevated areas.

Rivers that form follow paths that are less resilient and are concentrated in places where the rock banks are soft. The river arm forms an obtuse angle with the main river.

Trellis River Flow

Trellis
Trellis

Grid usually we know about the fence. It is true, as the name suggests, that the flow pattern of the Trellis River is a river whose river resembles a fence controlled by geological structures in the form of synclines and anticline folds.

A river with a lattice flow pattern is characterized by a group of water channels that form a parallel pattern that flows towards the slope and perpendicular to the main channel. The main channel in this river usually runs towards the fold axis.

Trellis Flow Pattern is a flow pattern shaped like a fence (trellis) controlled by geological structures in the form of synclines and anticlines. The Trellis River is characterized by a collection of waterways that form a parallel pattern and flow along the slopes and perpendicular to the main channel. Usually, the direction of the main channel is in the direction of the folding axis.

In this pattern, there is a combination of successive and connected rivers. This pattern can also form along parallel valleys in folded mountain belts. In this area, the river flows through the valley and opens into the main channel.

This lattice flow pattern contains a combination of sequential and contiguous flows. This lattice flow pattern can also form along parallel valleys in folded mountain belts. In this region, many rivers flow through valleys and open into main channels, which eventually lead to river mouths.

Annular River Flow

Annular
Annular

A drainage pattern in which a river or its tributaries are distributed in a circle. It is generally found in the dome area with adult status. This pattern is an extension of the radiation pattern. This distribution pattern follows gaya stone coating.

Multibasal Stream or Sink Hole

Annular
Multibasinal atau Sink Hole

Imperfect flow patterns, sometimes visible on the earth’s surface, sometimes not visible, are referred to as underground rivers. This drainage pattern develops in karst or limestone areas.

Contorted . River Stream

Annular
Contorted

A flow pattern in which the direction of flow is reversed. A control structure operating in the form of an irregular crease pattern that allows the formation of bends or bends in sediment layer available.

This is the presentation of the River Flow above, hopefully useful

What is meant by river flow pattern?

River flow pattern is a group of rivers with the same shape that can describe the state of the profile and genetics of the river (Sandy, 1985 and Katili, 1950; Lobeck, 1939).

How many types of river flow patterns are there?

There are several types of river flow patterns, among them Dendritic, Radial, Rectanguler, Trellis, Parallel, Annular, multi-basinal or Sink Hole, Contorted and other sub-flow patterns.

Mention other sub-patterns of river flow?

Namely Pinnate, Sub-dendritic, Sub-parallel and Deranged

Also Read Other Articles:

RELATED ARTICLES

Moment Davido Collected A Drink From Chioma At Israel DMW’s Wedding Got People Talking

<!-- Moment Davido Collected A Drink From Chioma At Israel DMW’s Wedding Got People Talking...

Russian security forces thwarted a terrorist attack in the Stavropol Territory

Russia’s Federal Security Service (FSB, for its Russian acronym) reported today that it had thwarted a terrorist attack in Russia’s Stavropol Territory prepared by...

Kingdom Wars Mod Apk v2.0.2 Unlimited Gold Diamond Terbaru

Afmar.Co.Id – Hello, What’s up bro and mbak bro. Yesterday I reviewed how “Omega Legends“. This time I will review an article about “Kingdom...

LEAVE A REPLY

Please enter your comment!
Please enter your name here

Most Popular

Advantages of business trip massage

xn--hz2b17kttdbub47a07t.com is practice of massage therapy is an alternative therapy that is quickly gaining popularity. In recent years, the...

Best Sports Toto

Totowiki is formed by a fixed refund rate method and a fixed dividend rate method. The method of fixed refund rate is called 'Toto',...

Uses of Digital Pressure Regulator

In a short time, these regulators have become very popular. They provide flexibility, robustness and have the capability to handle high pressure electronically. Before...

part-time job night part-time job

Chipmakers are beginning to target job cuts and other adjustments, including reducing factory hours to cope with the economic downturn, chief executive...

Recent Comments