DESERTS AND WIND ACTION - PowerPoint PPT Presentation

About This Presentation
Title:

DESERTS AND WIND ACTION

Description:

DESERTS AND WIND ACTION DESERTS AND WIND ACTION Desert regions and wind erosion Desert and adjacent region desert region which has an arid climate steppe region ... – PowerPoint PPT presentation

Number of Views:384
Avg rating:3.0/5.0
Slides: 26
Provided by: erw93
Category:
Tags: action | and | deserts | wind | action

less

Transcript and Presenter's Notes

Title: DESERTS AND WIND ACTION


1
DESERTS AND WIND ACTION
2
DESERTS AND WIND ACTION
  • Desert regions and wind erosion
  • Desert and adjacent region
  • desert
  • region which has an arid climate
  • steppe
  • region adjacent to a desert with semiarid climate

3
DESERTS AND WIND ACTION
Desert (arid climate) and steppe
(semiarid climate) areas on Earth
4
DESERTS AND WIND ACTION
  • Wind erosion processes
  • deflation is the removal of rock waste from the
    land by the wind
  • blowout or deflation hollow is a depression
    excavated by the wind in materials as sand and
    silt deposits easily eroded because of a lack of
    the presence of adequate vegetation which impedes
    deflation

5
DESERTS AND WIND ACTION
Blowout or deflation hollow
6
DESERTS AND WIND ACTION
Deflation Hollow---Blowout
7
DESERTS AND WIND ACTION
abrasion is the sandblastingeffect on materials
caused by the impact with particles carried by
the windfrosted windows in houses and ventifacts
form
8
DESERTS AND WIND ACTION
  • Wind erosion loads
  • suspended load
  • suspended wind blown particles
  • consists primarily of silt or clay size particles
    and if highly concentrated can result in dust
    storms
  • deposition of the suspended load can result in
    large deposits of loess lacking layering or
    stratification

9
DESERTS AND WIND ACTION
Dust Storms
10
DESERTS AND WIND ACTION
Loess Deposits
11
DESERTS AND WIND ACTION
  • bed load
  • particles bounced along the ground
  • usually consists of sand size particles
  • accumulation of the bed load forms desert sand
    dunes which can migrate easily(active dunes)
  • Active sand dunes
  • Nature of active (unstable) dunes
  • dune profile
  • consists of a more gentle windward slope and
    steeper leeward slope or slipface

12
DESERTS AND WIND ACTION
Dune profile
13
DESERTS AND WIND ACTION
  • shifting dunes
  • shift downwind and can bury roads, airport
    runways, homes, etc.
  • Categories of active dunes
  • based on shape of dune in plan view
  • barchan
  • crescent shaped with convex portion facing the
    wind direction
  • formed with a constant wind direction and limited
    sand supply

14
DESERTS AND WIND ACTION
Barchan dunes
15
DESERTS AND WIND ACTION
  • transverse
  • elongated perpendicular to direction of wind
  • formed with a constant direction of wind and
    large supply of sand

16
DESERTS AND WIND ACTION
  • longitudinal or seif
  • elongated in general direction of wind
  • formed with slightly different wind directions
    and limited sand supply

17
DESERTS AND WIND ACTION
  • star or complex
  • formed with variable wind direction

18
DESERTS AND WIND ACTION
  • Desert landscape and evolution
  • Alluvial fan
  • fan shaped deposit formed at the foot of
    mountains in the desert valley or basin

19
DESERTS AND WIND ACTION
a bajada is an apron of sediment resulting from a
coalescence of alluvial fans
20
DESERTS AND WIND ACTION
Playa lake and playa a temporary shallow lake
formed in the central basin of a desert during a
rare abundant rainfall--a playa is the dry flat
lake bed that remains
21
DESERTS AND WIND ACTION
  • Inselberg
  • an isolated erosional remnant present after long
    term erosion of mountain areas which are reduced
    to these bedrock knobs elevated above the
    surrounding sediment filled basin

22
DESERTS AND WIND ACTION
  • Pediment
  • a carved gently sloping erosional surface on the
    bedrock in a desert mountainous area

23
DESERTS AND WIND ACTION
Stages of landscape in mountainous desert
regions
24
DESERTS AND WIND ACTION
  • Inactive or stable dune---mostly non-desert
  • Parabolic dune(foredune)
  • formed along coastlines of oceans or large lakes
  • winds cause blowouts in sand resulting in a
    crescent shape with the concave side facing the
    prevailing wind direction

25
THATS ALL THE CYBER GEOLOGY COURSE
FOLKS
Write a Comment
User Comments (0)
About PowerShow.com