Sand Dunes Flashcards
Formation: Dunes have a downwards ‘lee’ slope and
An upwards ‘stoss’ slope.
Formation: An obstacle, such as a
Rock, allows transported particles to settle around it. The particles build up to form a dune.
Formation: The wind moves particles up the
Stoss slope by saltation. The particles accumulate on the lee slope.
Formation: As material becomes unstable,
It moves down the lee slope, resulting in dune migration downwind.
Scale: Greater dune height =
Slower movement.
Scale: Taller dune =
Greater volume.
Scale: Ripples - usually measured in
cm to 10’s of cm.
Scale: Ripples - Wind blows on
Sand crest, ripple crests are perpendicular to wind direction.
Scale: Ripples - Wavelength of ripples is
Determined by the average distance sand particles jump during saltation.
Scale: Dunes - Wavelengths measured in
10’s - 100’s metres.
Scale: Dunes - Height measured in
Metres.
Scale: Dunes -
Accumulation of sand, blown into a mound by the wind.
Scale: Draas - Large dunes, measured in
Kilometres.
Scale: Draas - Height measured in
Metres.
Form: Crescentric dunes - (3)
Crescent shaped.
Segment is wider than it is long.
In areas with a single wind direction.