8.2 Wind

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8.2 Wind Pages 191-197

Goal 1 Learn wind erosion terms

Goal 1: Be familiar with wind erosion terms ,[object Object],[object Object]

Goal 1: Be familiar with wind erosion terms ,[object Object],[object Object]

Goal 1: Be familiar with wind erosion terms ,[object Object]

Goal 2 Identify 3 conditions that contribute to wind erosion

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Goal 3 Recognize types of dunes; areas where they form and their migration direction

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Tendances

003 008-ocean motions

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Scientists found a system of ridges or mountains in the seafloor similar to those found in the continents.These are called mid-ocean ridges. One of these is the famous Mid-Atlantic Ridge, an undersea mountain chain in the Atlantic Ocean. It has a gigantic cleft about 32-48 km long and 1.6 km deep. The ridge is offset by fracture zones or rift valleys. In the early 1960’s, scientist Harry Hess, together with Robert Dietz, suggested an explanation to the continental drift. This is the Seafloor Spreading Theory.In the early 1960’s, scientist Harry Hess, together with Robert Dietz, suggested an explanation to the continental drift. This is the Seafloor Spreading Theory. This material flows sideways carrying the seafloor away from the ridge, and creates a crack in the crust. The magma flows out of the crack, cools down and becomes the new seafloor. Overtime, the new oceanic crust pushed the old oceanic crust far from the ridge. The process of seafloor spreading allowed the creation of new bodies of water. For example, the Red Sea was created as the African plate and the Arabian plate moved away from each other. Seafloor spreading is also pulling the continents of Australia, South America, and Antarctica away from each other in the East Pacific Rise. The East Pacific Rise is one of the most active sites of seafloor spreading, with more than 14 centimeters every year. Findings that support Seafloor Spreading Theory: 1. Rocks are younger at the mid-ocean ridge. 2. Rocks far from the mid-ocean ridge are older. 3. Sediments are thinner at the ridge. 4. Rocks at the ocean floor are younger than those at the continents.

The seafloor spreading

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Introduction marine geology

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The reason for the occurrence of such a huge mass of water on the globe, is still a myth and reality. The reason goes back to the Origin of Earth itself. The exact mode of origin is not precisely known. Scientists assume, both Primary and secondary sources would have given rise to all both air and water on the earth. Two possible sources as internal source (or) external source have been proposed so far. Some of them are attributed towards the theories of origin of the earth.

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Mainguet M. & Dumay F., 2011. Fighting wind erosion. one aspect of the combat against desertification. Les dossiers thématiques du CSFD. N°3. May 2011. CSFD/Agropolis International, Montpellier, France. 44 pp. - Wind erosion—alone or combined with other physical or socioeconomic causes—is a mechanism that may induce desertification, i.e. severe or irreversible degradation of water and soil resources. Now that this phenomenon is better understood, the model of the 1970s based on three distinct stages (causes, mechanisms, consequences) has been discarded, in view of the many feedbacks and insidious links generated by wind erosion. Timely detection of wind erosion onset thresholds with remote sensing tools (satellite images and aerial photographs), and spatial delimitation and positioning of the phenomena observed are essential to be able to efficiently combat the damaging effects of wind erosion. No field operations can be effective without prior knowledge of wind erosion mechanisms at the land-atmosphere interface.

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Wind has the ability to shape the surface of the Earth. Wind is one of the greatest agents of land erosion and transportation. The action of wind is very significant in arid and semi-arid regions. Due to profound wetness, wind cannot act in humid regions. Wind is capable of eroding, transporting and depositing the surface materials, in drylands. The landforms created by wind action are called as Aeolian landforms. The word “Aeolian” is derived from the Greek word “Aeolus”, meaning, the god of the winds.

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8.2 Wind

1. 8.2 Wind Pages 191-197

2. Goal 1 Learn wind erosion terms

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10. Goal 2 Identify 3 conditions that contribute to wind erosion

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14. Goal 3 Recognize types of dunes; areas where they form and their migration direction

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