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What is a blowout?
barchanoid dunes
had their source as glacial sediments
is steeper than the windward side
by saltation as part of the bed load
a shallow depression caused by deflation
D
in the same direction as the wind blows
longitudinal dunes
The thick loess deposits in South Dakota, Nebraska and Iowa
barchanoid dunes
had their source as glacial sediments
is steeper than the windward side
by saltation as part of the bed load
a shallow depression caused by deflation
D
in the same direction as the wind blows
longitudinal dunes
When wind creates a sand dune, the sheltered side of the dune
barchanoid dunes
had their source as glacial sediments
is steeper than the windward side
by saltation as part of the bed load
a shallow depression caused by deflation
D
in the same direction as the wind blows
longitudinal dunes
Sand dunes that form scalloped rows of sand at right angles to the wind are called
barchanoid dunes
had their source as glacial sediments
is steeper than the windward side
by saltation as part of the bed load
a shallow depression caused by deflation
D
in the same direction as the wind blows
longitudinal dunes
How does wind transport sand grains
barchanoid dunes
had their source as glacial sediments
is steeper than the windward side
by saltation as part of the bed load
a shallow depression caused by deflation
D
in the same direction as the wind blows
longitudinal dunes
Long sand ridges that are oriented more of less parallel to the prevailing wind are called
barchanoid dunes
had their source as glacial sediments
is steeper than the windward side
by saltation as part of the bed load
a shallow depression caused by deflation
D
in the same direction as the wind blows
longitudinal dunes
Over time, sand dunes tend to migrate
barchanoid dunes
had their source as glacial sediments
is steeper than the windward side
by saltation as part of the bed load
a shallow depression caused by deflation
D
in the same direction as the wind blows
longitudinal dunes
(in your book p 206 figure 22) Which diagram illustrated lingitudinal lines?
barchanoid dunes
had their source as glacial sediments
is steeper than the windward side
by saltation as part of the bed load
a shallow depression caused by deflation
D
in the same direction as the wind blows
longitudinal dunes
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