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WIND. Chapter 6 Test 3 material End. EOLIAN. EQUALS WIND EROSION + WIND TRANSPORT + WIND DEPOSITION. EROSIONAL CAPACITY OF WIND. ABILITY FOR WIND TO MOVE MATERIALS IS SMALL COMPARED TO ICE (GLACIERS) & WATER (RIVERS). DEFLATION. THE REMOVAL AND LIFTING OF INDIVIDUAL LOOSE PARTICLES

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WIND

Chapter 6

Test 3 material

End


Eolian
EOLIAN

  • EQUALS WIND EROSION + WIND TRANSPORT + WIND DEPOSITION


Erosional capacity of wind
EROSIONAL CAPACITY OF WIND

  • ABILITY FOR WIND TO MOVE MATERIALS IS SMALL COMPARED TO ICE (GLACIERS) & WATER (RIVERS)


Deflation
DEFLATION

  • THE REMOVAL AND LIFTING OF INDIVIDUAL LOOSE PARTICLES

  • DESERT PAVEMENT


Blowout depressions
BLOWOUT DEPRESSIONS

  • RANGE IN SIZE FROM A FEW FEET DEEP AND A FEW FEET ACROSS TO 150 FEET DEEP AND SEVERAL MILES ACROSS


Abrasion
ABRASION

  • PARTICLES PICKED UP BY WIND CAN RUB ACROSS SOLID ROCK THEREBY FILING IT AWAY SIMILAR TO SANDPAPER


Wind transportation
WIND TRANSPORTATION

  • SALTATION - SKIPPING AND BOUNCING

  • SURFACE CREEP


ERG

  • SAND SEA THAT MOVES AS A UNIT


Sand dune movement
SAND DUNE MOVEMENT

  • STOSS - WIND

  • LEE - WHERE SLIP FACE OCCURS


Dune forms
DUNE FORMS

  • BARCHAN

  • TRANSVERSE

  • PARABOLIC

  • LONGITUDINAL

  • STAR


Loess
LOESS

  • DEPOSITS OF WIND BLOWN SOIL

  • MAY COME FROM DESERT REGIONS SUCH AS THE GOBI DESERT IN CHINA WHERE DEPOSITS OF 100-400 FEET OCCUR. YELLOW RIVER

  • GLACIAL /PERIGLACIAL REGIONS ALONG ILLINOIS & MISSISSIPPI RIVERS WITH 300 INCHES DEEP


Why is there a desert here
WHY IS THERE A DESERT HERE?

  • EASTERN FLANK OF THE SUBTROPICAL HIGHS


Arid landforms
ARID LANDFORMS

  • PLAYA IS SALT CRUSTS LEFT BY RUNOFF WATERS THAT EVAPORATE

  • ALLUVIAL FAN - MOUTH OF CANYON WHERE WATER EXITS INTO A VALLEY

  • BAJADA - INDIVIDUAL ALLUVIAL FANS COALESCE INTO ONE SLOPING SURFACE





Frost wedging is an example of
FROST WEDGING IS AN EXAMPLE OF

  • MECHANICAL WEATHERING

  • CHEMICAL WEATHERING

  • MECHANICAL EROSION

  • CHEMICAL EROSION

    CORRECT RESPONSE IS MECHANICAL WEATHERING


Illustrates differential weathering erosion
ILLUSTRATES DIFFERENTIAL WEATHERING & EROSION

  • SANDSTONE

  • SHALE

  • LIMESTONE

  • CONGLOMERATE

  • CORRECT RESPONSE IS LIMESTONE


True of impermeable rock
TRUE OF IMPERMEABLE ROCK

  • WATER FLOWS THROUGH IT

  • IT CONDUCTS GROUNDWATER IN USABLE AMOUNTS

  • AQUIFERS ARE MADE UP OF IT

  • ALL ARE TRUE

  • NONE ARE TRUE

  • CORRECT RESPONSE IS NONE ARE TRUE


Hydraulic action in a stream is due to
HYDRAULIC ACTION IN A STREAM IS DUE TO:

  • TURBULENCE IN WATER

  • STREAM LOAD

  • STREAM PROFILE

  • STREAM LENGTH

  • CORRECT RESPONSE IS TURBULENCE IN WATER


The phreatic zone is
THE PHREATIC ZONE IS

  • ABOVE THE WATER TABLE

  • AT THE WATER TABLE

  • BELOW THE WATER TABLE

  • ABOVE THE SOIL-ROOT ZONE

  • CORRECT RESPONSE IS BELOW THE WATER TABLE


High mountain stair step lakes in glacial area
HIGH MOUNTAIN STAIR-STEP LAKES IN GLACIAL AREA

  • PATERNOSTER

  • ARETE

  • NUNATAK

  • FIORD

  • CORRECT RESPONSE IS PATERNOSTER


Eolian refers to
EOLIAN REFERS TO

  • WIND EROSION

  • WIND TRANSPORT

  • WIND DEPOSITION

  • ALL OF THESE

  • NONE OF THESE

  • CORRECT IS ALL OF THESE


A playa is
A PLAYA IS

  • INDIVIDUAL ALLUVIAL FANS COALESCING TOGETHER

  • SALT CRUSTS LEFT BY RUNOFF WATER THAT EVAPORATED

  • TYPE OF SAND DUNE

  • SAND SEA MOVING AS A UNIT

  • CORRECT RESPONSE IS SALT CRUSTS


Which do find in an old age stream
WHICH DO FIND IN AN OLD-AGE STREAM?

  • DEEP V-SHAPED VALLEYS

  • STRAIGHT STREAM

  • STEEP GRADIENT

  • MANY OXBOW LAKES

  • CORRECT RESPONSE IS MANY OXBOW LAKES


Who wrote your textbook
WHO WROTE YOUR TEXTBOOK?

  • STEVE BLACKMAN

  • BOB DENNISON

  • FRODO BAGGINS

  • ED TARBUCK

  • FRED LUTHMANN

  • ANSWER: ED TARBUCK


Link to reviewsheet
LINK TO REVIEWSHEET

  • http://www.hcc.cc.il.us/staff/bobd/easc121tr3.html


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