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Rocks are usually smooth and perhaps pitted (with holes) on the windward side. The leeward side of tall rock structures such as mountains are also warmer and drier due to precipitation on the windward side, so an abundance of streams may indicate the windward side of a mountain and a lack of streams may indicate the leeward side, forming deserts. "Mushroom rocks" show that the wind is dry and contains sediments which wears away the lower parts of large rocks.

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Q: What can rock structures tell you about wind?
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What is a wind eroded rock called?

Wind eroded rocks are found mostly in arid regions, i.e. Desert Topography. Rocks eroded by wind are of different types and structures and are called different names depending on its form and agent of formation. The names given to some wind eroded rocks are; 1. Inselberg. 2. Rock Pedestals. 3. Zeugen.


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Most rocks are not uniform throughout. On a scale usually best measured in millimeters or centimeters, they are composed of individual mineral grains that vary in size, shape and composition. The geometric characteristics of and relationships between these small-scale rock features constitute rock texture. Rock commonly also vary on larger scales, best measured in centimeters to meters to kilometers. The individual, contrasted, larger-scale features of rocks are called 'structures'. Our task will be to see if there are rock structures that can provide clues to a rock's formational environment: whether it's igneous, sedimentary or metamorphic.There are hundreds of distinct rock structures. Geologists find it convenient to divide them into 'primary' and 'secondary' structures.Primary Structures: structures formed before or at the same as material is in the process of becoming rock. For example, formed as magma crystallizes or as sediment accumulates.Secondary Structures: structures imposed on rock after it has already formed. For example, formed as a result of compression of existing rock.


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an isobar can tell you the wind mileage and the strength of the wind


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