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Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead
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Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Dec 22, 2015

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Darrell Rich
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Page 1: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Desert Arch

• Typically formed by wind• Narrow ridges are formed

and the softer substrata is weathered first, forming a bridge/arch overhead

Page 2: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.
Page 3: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Ventifact

• Created by wind erosion

• Wind carries fine particles that work like a sand blaster (i.e. sand, silt, clay, and ice particles)

• The windward face of the rock is flattened and smoothed

• Usually pebble to cobble sized

Page 4: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.
Page 5: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

• A type of ventifact that has three ridges

• Multiple faces have been formed by either a changing prevailing wind or movement of the actual rock being weathered

Dreikanter

Page 6: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.
Page 7: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Desert pavement

• Formed in arid environments when wind carries finer, more lightweight particles such as sand away

• Large particles are left behind and protect from further erosion

Page 8: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.
Page 9: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Loess

• Yellowish, fine grained silt and clay sized particles

• Formed by glaciers

• Carried and deposited by wind

Page 10: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

leeward leewardwindward

Page 11: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Sand Dunes

• Piles of sand

• Deposited by wind

• Leeward side (slipface) has a steeper slope

• Windward side is more gradual

Page 12: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.
Page 13: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Barchan Dune

• Crescent shaped dunes

• Concave side is the leeward side

• Formed from a unidirectional wind

Page 14: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.
Page 15: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Transverse dunes

• A dune that elongates perpendicular to the prevailing wind

• Caused by a combination of wind directions

Page 16: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.
Page 17: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Parabolic dunes

• Crescent shaped dunes

• Concave side is the windward side

• Found in coastal deserts

• Arms of the crescent lag behind because they are held in place by vegetation

Page 18: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.
Page 19: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Ergs

• Huge dune fields

• Notice the source of sand from the photos

Page 20: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.
Page 21: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Ripple marks

• Miniature dunes within a dune (not more than 2 inches tall)

• Formed by wind

• May form from cross winds and appear to be traveling in a different direction than the large dune

Page 22: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.
Page 23: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Deflation

• Low spots carved out by wind erosion

• High elevations are left due to vegetative stabilization

Page 24: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.
Page 25: Desert Arch Typically formed by wind Narrow ridges are formed and the softer substrata is weathered first, forming a bridge/arch overhead.

Pedestal rock

• Base of a rock is weathered and eroded more quickly due to sand blasting

• Sand grains can only be picked up a couple of feet