External geological agents

 The EXTERNAL GEOLOGICAL AGENTS are natural systems that carry out different geological processes. They modify, alter or transform the surface of the planet and produce characteristic landforms (they carry out the process of modelling the land relief).

They are dynamic agents because they have the ability to move, and they act thanks to the solar energy of the sun (the energy of the sun makes air masses move and this causes the water cycle with  precipitation).

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There are SIX MAJOR GEOLOGICAL AGENTS which are:

1.- WIND: It´s air moving on the Earth surface. It acts mainly in areas with no vegetation like the deserts and beaches.

Also, the wind is capable of eroding, transport and sediment. Wind can transport materials and vegetation anywhere on the planet.

On the one hand, the wind's ability to erode is due to the sand that it transports, which, when colliding with the rocks, wears them down. On the other hand, the sand carried by the wind is depositedin certain areas, forming dune fields. Dunes are large accumulations of sand that move and move slowly in the direction of the wind. 

The main landforms produce by the wind are: pedestal rocks, regs and barchans.

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2.- GLACIERS: is a slowly moving mass or river of ice. It has a tremendous capacity for erosion and transport of materials. It is formed by the accumulation and compaction of snow in the mountains or near the poles.

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3.- RIVERS: they are natural streams of water that transport and erode materials. Rivers flow toward a sea, ocean, lake or another river. There capacity of erosive and transporting capacity depends on the speed of flow of water, the climate and location (high mountain or valley). The erosion and the amount of material transported is condicionated by the flow and the gradient.

In the upper course of the river, the slope is greater and erosion and transport processes dominate. In the middle course the slope decreases. Although the river retains a certain capacity to erode and transport materials, begins to sediment eroded material upstream. In the lower course the slope is very gentle, the river practically loses its ability to erode and only deposits sediments.

The main landforms produce by rivers are: meanders, V-shaped valleys and deltas.

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4.- OCEANS: they cause coastal erosion along the shore line removing materials from the coastline and sometimes forming cliffs where we can see the great capacity of erosion of the water. They also carry rivers sediments.

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The waves erode the rocks in the area littoral, transport the produced sediment and deposit it later. This causes different effects of erosion and sedimentation.

Currents and tides also produce processes of erosion, transport and sedimentation due to fluctuations in sea level.

The main landforms produce by marine sedimentation are: sand bars, sand spits, salt marshes, coastal lagoon, beaches and tombolo. 

5.- GROUNDWATER: In the water cycle, a part of which precipitates over the continents infiltrates into the subsoil, through permeable rocks, until finding a layer of rock waterproof that retains it. Groundwater is  water that flows downward influenced by gravity and it  can dissolve (due to the acidity) soluble underground rocks and it can form, galleries, chambers, limestone pavement, caves, stalatites, dolines, potholes, etc.

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6.- SURFACE RUN OFF: excess of water (rain, melted snow or other waterflows over the land surface) that flows over that land. It has a bigger capacity of erosion in areas in which doesn’t usually rain and torrential rains. It can create: ravines, gorges, rills, gullies…

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INTRODUCTION

  INTRODUCTION: DEFINITION: A  GLACIER  is a slowly moving mass or river of ice. It has a tremendous capacity for erosion and transport of m...