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Page 1: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

GE0-3112GE0-3112 Sedimentary processes and products Sedimentary processes and products

Lecture 7. Aeolian sedimentsLecture 7. Aeolian sediments

Geoff CornerGeoff CornerDepartment of GeologyDepartment of GeologyUniversity of TromsøUniversity of Tromsø20062006

Literature:Literature:- Leeder 1999. Ch. 16 - Leeder 1999. Ch. 16 Aeolian sediments in low-latitude desertsAeolian sediments in low-latitude deserts(See also Ch. 8 & Ch. 13). (See also Ch. 8 & Ch. 13).

Page 2: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

ContentsContents

►7.1 Aeolian environments7.1 Aeolian environments►7.2 Desert types and distribution7.2 Desert types and distribution►7.3 Sediment flow paths7.3 Sediment flow paths►7.4 Dunes and draas7.4 Dunes and draas►7.5 Desert facies and architecture7.5 Desert facies and architecture

Page 3: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Aeolian environmentsAeolian environments

►Types:Types: Deserts and semi-arid regionsDeserts and semi-arid regions Beaches and sabkasBeaches and sabkas Sandy river banksSandy river banks Periglacial regionsPeriglacial regions

►Characteristics:Characteristics: Lack of vegetationLack of vegetation Moderate to strong windsModerate to strong winds Mobile sand and silt sedimentMobile sand and silt sediment

Page 4: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

DefinitionsDefinitions

►Desert: arid zone having a large deficit Desert: arid zone having a large deficit of precipitation (P) in relation to of precipitation (P) in relation to evaotranspiration (ET)evaotranspiration (ET)

►Definitions/subdivision (P/ET ratios):Definitions/subdivision (P/ET ratios): Hyperarid:Hyperarid: <0.03 <0.03 Arid: Arid: 0.03-0.20.03-0.2 Semiarid:Semiarid: 0.2-0.50.2-0.5 Subhumid:Subhumid: 0.5-0.70.5-0.7

Page 5: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

World distribution of deserts (arid, hyperarid) and other dry areas.

Sahara

Arabia

Gobi

KalahariNamib

Patagonia(Argentina))

Atacama (Chile)

South-centralAustralia

SouthwestN. America

Page 6: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Desert types and distributionDesert types and distribution

►Trade wind deserts (subtropical high-Trade wind deserts (subtropical high-pressure)pressure) N. Africa, Arabia, south-central Australia.N. Africa, Arabia, south-central Australia. Atacama, Namib (cool offshore current).Atacama, Namib (cool offshore current).

►Continental desertsContinental deserts Central asia.Central asia.

►Rain shadow/continentalRain shadow/continental western N. America, western N. America,

sub-Andean S. America.sub-Andean S. America.

Page 7: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

► Sub-tropical high pressure cells and trade winds.Sub-tropical high pressure cells and trade winds.

Page 8: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

► Rain shadow effect (lower precipitation E of Rain shadow effect (lower precipitation E of mountains)mountains)

Page 9: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Deserts and aeolian depositsDeserts and aeolian deposits

►Rocky desertsRocky deserts►Sandy desertsSandy deserts►Most deserts contain rock outcrops Most deserts contain rock outcrops

and aeolian, lake or playa, and alluvial and aeolian, lake or playa, and alluvial depositsdeposits

►Loess deposits in and beyond desertsLoess deposits in and beyond deserts

Page 10: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

► Presently active sand dunes.Presently active sand dunes.

► Glacial maximum sand dunes.Glacial maximum sand dunes.

► Loess (mostly glacial maximum).Loess (mostly glacial maximum).

Distribution of Distribution of aeolian depositsaeolian deposits

Page 11: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Sediment transportSediment transport

Sand-flow map for Saharan ergs

►SandSand

Page 12: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Aerosol dust budgets for the Sahara and adjacent Atlantic Oceann.

►DustDust

Page 13: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Page 14: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Dune types and interdune Dune types and interdune terrainterrain

►Bedrock and erosional forms (yardangs)Bedrock and erosional forms (yardangs)►DunesDunes

BarchansBarchans Transverse dunesTransverse dunes Linear dunesLinear dunes Star dunesStar dunes

►Lakes and (saline) playasLakes and (saline) playas►Alluvial fans and stream bedsAlluvial fans and stream beds

Page 15: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Linear and compound dunes

Star dunes

Linear dunes

Interdune and intererg areas

Barchan dunes

Saharan dunes

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Aeolian GEO-3112 2006

Star dunes

Barchan dunes

Page 17: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Linear dunes

Page 18: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Linear and compound dunes

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Aeolian GEO-3112 2006

Star dunes

Namib desert

Transverse dunes?

Page 20: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Uluru (Ayer’s Rock),Central Australia

Page 21: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Controls on sand depositionControls on sand deposition

Page 22: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Facies and architectureFacies and architecture

Facies sequencesat the marginsof an erg.

Page 23: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Aeolian architectureAeolian architecture

Dune Interdune

Page 24: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

► U. Jurassic Entrada U. Jurassic Entrada sandstone, W. USA. sandstone, W. USA.

Page 25: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

► Permian Rotliegendes, Permian Rotliegendes, NW EuropeNW Europe

Page 26: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Active dry phase

Wet phase

Formation of ’supersurface’

Page 27: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Page 28: GE0-3112 Sedimentary processes and products Lecture 7. Aeolian sediments Geoff Corner Department of Geology University of Tromsø 2006 Literature: - Leeder

Aeolian GEO-3112 2006

Further readingFurther reading

►Galloway & Hobday 1996. Ch. 10. Galloway & Hobday 1996. Ch. 10. Eolian systems.Eolian systems.

►Kocurek, in Reading (ed.), 1996. Ch. 5. Kocurek, in Reading (ed.), 1996. Ch. 5. Desert aeolian systems. Desert aeolian systems.