Save
...
F2: Sedimentory
Environments
Desert Environment
Save
Share
Learn
Content
Leaderboard
Share
Learn
Created by
Meredith Thomas
Visit profile
Cards (5)
Often found in
continental
interiors. Rainfall is rare but when it does occur is
torrential
and leads to
flash flood
Wadis
Desert stream channels, steed gradients, very high energy so transport coarse grained, energy is lost rapidly
Poorly sorted, angular to rounded
Red colour
Breccia and Conglomerate
Alluvial Fan
Same idea as
rivers
Close To mountains -
breccia
Further away transported length, greater and so grains are smaller
Often
feldspar
and mica from granites in the higher mountains -
Arkose
Desert Sandstone
Very well
sorted
Very well
rounded
High sphere it’s
Entirely
Quartz
Red due to
iron cement
Large scale
cross bedding
Playa Lake
Metal ions from weathered rock in the high ground become more concentrated. eventually precipitated out of solution
Siltstone/mudstone
Evaporties
Salt Psuedomorphs
Dessicration Cracks
ripple Mark