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valpartijen

Valpartijen, plural of valpartij, is a Dutch term used primarily in geology and winter sports to describe avalanches—the rapid downslope flow of snow. They occur when the snowpack becomes unstable due to factors such as heavy snowfall, warming, rain-on-snow events, or wind loading that creates slabs. Avalanches can be slab avalanches, in which a cohesive block of snow releases and slides as a unit, or loose-snow avalanches, which start at a point and fan out as they descend.

The risk depends on snow depth, the presence of weak layers within the snowpack, slope angle (most

Valpartijen have a long history in mountainous regions, shaping safety practices, rescue services, and backcountry etiquette.

likely
between
about
30
and
45
degrees),
terrain
features,
and
exposure
to
wind.
In
practice,
avalanche
danger
is
assessed
by
forecast
centers
that
issue
daily
bulletins
with
danger
ratings
and
travel
advisories.
To
reduce
risk,
professionals
and
trained
recreational
users
employ
planning
methods,
check
forecasts,
and
carry
rescue
gear
such
as
an
avalanche
transceiver,
probe,
and
shovel.
Optional
safety
measures
include
airbag
backpacks
and
companions
trained
in
avalanche
rescue.
In
Dutch
usage,
valpartij
is
principally
a
technical
term
found
in
safety,
meteorology,
and
sports
contexts;
the
more
general
everyday
term
for
the
phenomenon
is
lawine.