In this website a series of
photo's of ephemeral gullies is shown from South Limbourg, the
Netherlands, an area with an undulating topography and loess soils.
Ephemeral gullies are a form
of soil erosion. The gullies are very much
wider than
deep. They are formed during heavy rainfall, mostly on fallow arable
land. They tend not to go deeper than the
tilled layer. They are removed by normal tillage. Hence, the name
ephemeral gullies (= short lived, temporary, transient, transitory). For a
detailed discussion of ephemeral
gullies and the difference with other forms of soil erosion (rill
erosion, classical gully erosion) see Foster
(1986) Understanding ephemeral gully erosion.
Ephemeral
gully head viewed in a downslope direction.
View upslope of an ephemeral gully.
Uprooting of crop
(sugarbeets) by an ephemeral gully.
Uprooting of crop (sugarbeets)
This and the next eight
pictures are of an
event of 55 mm of rain in 2 hours incl.
30 mm in 30 minutes. The
aerial
photographs
of
the
event
were
taken
by
D. Koeman. The
location is the Ransdalerveld, South Limbourg, The Netherlands. The width of the road
(Vrakelbergerweg) alongside
the gully is appr. 4 m. Notice that a
cropped field was not eroded by the gully, showing that a crop can
protect the soil.
The ephemeral gully follows
the course of a dry valley bottom along de Vrakelbergerweg.
The ephemeral gully has
removed the plough layer of a recently ploughed field.
Very shallow ephemeral gully,
same location as above.
Notice the dark narrow strip
from left to right in the middle of the photo were the farmer has just
begun to plough a field, removing the gully in doing so. The cropped
field in the lower left hand corner was eroded by the gully. This was
not everywhere the case during this event. See the upper part of the
photo and the aerial photo's above and below. The direction of the
tillage furrows was perpendicular to the gully.
The water flow has crossed
two cropped fields without disturbing the crop.
The water flow has crossed a
cropped field without eroding the soil and the crop, showing that a crop can protect
the soil. It is surprising to see that there are hardly any signs of mud deposition in the field.
Same event and general area
as the pictures above. The colluvial fan in the bend of the road is
shown in the next photo.
Ephemeral gully crossing a
corn (maize) field ending in a colluvial fan at a road side (see photo
above).
This slide and the following
slides show ephemeral gullies from another event than the one above
(South Limbourg, The Netherlands). The soil contains rounded gravel
from
the river Meuse (a so called river terrace deposit).
Same site as above.
Same site as above.
Photo showing the
left part of the bare field of the
picture above.
Same field as above.
Same field as above.
Barely discernable incipient
ephemeral gullies coming from above crossing a cropped field
Incipient ephemeral gullies
and flowpaths crossing the ridges between tillage furrows.
Deposit left by an ephemeral
gully.
Deposit left by an ephemeral
gully.
Deposit left by an ephemeral
gully.
Deposit left by an
ephemeral
gully. Mud is removed from the road.
The copyright of the
photographs on this website is owned by F.J.P.M. Kwaad.