- the bed of a river.
Bedforms are
often preserved in the rock
record as a
result of
being present in a
depositional setting.
Bedforms are
often characteristic...
- of
bedforms such as
ripples or
dunes in a
flowing fluid. The
fluid flow
causes sand
grains to
saltate up the
stoss (upstream) side of the
bedform and...
- In geology,
ripple marks are
sedimentary structures (i.e.,
bedforms of the
lower flow regime) and
indicate agitation by
water (current or waves) or directly...
-
varying speeds and
velocities produce different structures, are
called bedforms. In the
lower flow regime, the
natural progression is from a flat bed,...
-
regime bedforms. As a result,
antidunes migrate in an
upstream direction,
counter to the
current flow.
Antidunes are
called in-phase
bedforms, meaning...
- such as ripples, dunes, or
antidunes on the
river or
stream bed.
These bedforms are
often preserved in
sedimentary rocks and can be used to
estimate the...
- next
blows in the
dominant direction.
Draas are very large-scale dune
bedforms; they may be tens or a few
hundreds of
metres in height,
kilometres wide...
-
current ripples spread out and
merge on the
basin floor.
These sedimentary bedforms are best seen in
aerial images and at low sun angles.
These giant current...
- Hall, Minard; Ramón, Patricio; Dingwell,
Donald B. (2013-10-13). "Dune
bedforms produced by
dilute pyroclastic density currents from the
August 2006 eruption...
-
characteristic of
turbidity currents. The
surface of a
particular bed,
called the
bedform, can also be
indicative of a
particular sedimentary environment. Examples...
