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Saskatchewan Glacier, Jasper National
Park
The
Saskatchewan Glacier is part of the Columbia Icefields.
It is located
117Km
south of the
Jasper
Town site, approximately
100K
north of Lake Louise. This hike has
a low elevation
gain of under
250Meters,
but the access in and out is
approximately
15Km
return.
Allow 5-6 hours for a round trip. The
Saskatchewan Glacier trailhead is
unmarked and not an official trail.
Don't attempt to access the route
from the west parking area near the
centre of big bend, it turns into a
long miserable bushwhack. The trailhead is located next to an old
abandoned concrete bridge, just as you enter
big bend on the Jasper Park
highway. Big bend is the large
highway loop
on the Jasper Park Highway before you ascend the
south side of the Columbia
Icefields. The gravel entrance to the old
bridge
is slowly eroding away and may be
gone in a few years. Park at the
old concrete bridge, then cross the
bridge
and take the trail
on your right which leads back west
along the
North Saskatchewan River and
the highway. Follow
this until you reach the trees then
look for an old gravel road heading
to your left. This old road was
built in the 1930's by the
U.S. Army's 87th
Mountain Division. The
Army
Division set up a camp
on the Saskatchewan Glacier to test
winter equipment. There are still
old parts of vehicles
scattered here and there. Logs that
were used
for this camp can still be found
high up on the glacier. Follow the old
road up through what used to be
the terminal
moraine of the Saskatchewan Glacier.
Keep in mind that this is the only
practical route in and out of
the entire valley so beware of
bears.
Grizzly Bears
crossing over the Columbia Icefields
may pass through from
Parker Ridge,
Wilcox Pass
and Castleguard Meadows. We ran into
a
Grizzly
crossing the ground moraine in the spring
of 2010. Once you hike up and over
the old moraine you'll arrive at the start of the valley.
You'll see an old log food stash
that was built by the
Alpine Club of
Canada in the 1950's. There are two
routes from here. The first and
safest day hike route follows the existing
old road straight ahead on the south Side of the
North Saskatchewan River.
This first route is absolutely
beautiful but you cannot get as
close to the Saskatchewan Glacier
due to an impassable
lateral
moraine. The second more dangerous
route is mainly used by climbers.
You'll have to cross a very
nasty looking canyon that is bridged
by a pile of old logs. The
North Saskatchewan River
disappears down this canyon and
reappears back at big bend on the
Jasper Park Highway.
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Follow a worn trail towards a bunch of rotting logs that form a
precarious bridge across the river canyon. Don't confuse
the initial log jam as the bridge.
The natural log bridge is a few meters
further down from the log jamb. Be very
careful here, if you fall into the
canyon it
is certain death. Over the years
this natural bridge, has gone from
one very large single log, to several smaller logs. It changes
from year to year due to erosion and
spring run offs. Climbers and
cavers are the ones that usually
rebuild it or add more logs to it each
year. Do not cross this log bridge unless you have
the proper mountaineering gear and you're absolutely
sure it is safe. Once again if
you breakthrough or fall off you
will most
likely never be found. If you have
any doubts take the first safer trail on
the south side of the
North Saskatchewan River. As you hike towards the toe
of the Saskatchewan Glacier the
scenery is absolutely beautiful.
Cliffs on the south side of the
valley rise
600M straight up.
Parkers and Hilda Ridge can be seen
on the north side. Views of the
hanging glaciers on the south
east faces of Mount Andromeda and
Mount Athabasca are outstanding. Further on you will
start to see the workings and
geology of the glacier.
Eskers,
drumlins,
lateral
moraines,
medial moraine,
ground
moraines,
erratics,
glacial polish,
striation on
rocks,
glacial
deposits,
rock flour,
till plains,
kettle lake,
Paternoster
lakes,
braided river,
katabatic winds
are all here.
See this
interesting survey from 1952
and compare the glacier photos to
these in 2010. Geoheads will love it here,
unusual and eye catching rocks
are everywhere.
Mount
Castleguard and Castleguard meadows
can be seen to the left half way up
the Saskatchewan Glacier.
Castleguard
Cave,
which is the longest cave in Canada
is located near here. As of 2007
cavers have surveyed
20357M of
passages and its
the fifth deepest at 384m.
Castleguard
Cave ascends gently from its
entrance and terminates beneath the
Columbia
Icefield.
Due to the caves flash flooding the
entrance is barred and locked by the
Parks Department. Parks permission and a
key, is required to enter
Castleguard
Cave. Be very
careful around the lake and the toe
of the Saskatchewan Glacier, there
is deep glacial silt along with hidden ice
under steep rock. Do not climb up
the
glacier unless you have
mountaineering experience and the
proper gear. Trailheads to
Parker Ridge,
Hilda Ridge,
Hilda Glacier,
Nigel Pass,
Wilcox Pass,
Weeping Wall,
Mount
Athabasca north Glacier,
Castleguard
Mountain Alpine Climb
and
Boundary Lake are
also located in this area.
You are in
bear country.
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Saskatchewan Glacier |
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Start at the
unmarked parking area. |
Big Bend on
highway before the Columbia Icefields. |
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Old bridge at
parking area. |
Canyon under
old bridge. |
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Hiking towards the Saskatchewan Glacier
valley along Big Bend |
Canyon under
old bridge. |
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More Alberta
Wildflowers. |
More Alberta
Mushrooms. |
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Trail leading
up into the valley. |
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Trail leading
down into the valley. |
waterfall
near trail leading down into the valley. |
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south east
face of Mount Andromeda |
southeast
Face of Mount Athabasca. |
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Old food
stash built by the Alpine Club of Canada in
the 1950's. |
More Alberta
Interesting Vegetation. |
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Old parts
left by the military from 1930. |
south side of
Parker and Hilda Ridge
near top,
ground moraine
to glacier. |
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More Alberta
Wildflowers. |
More Alberta
Interesting Vegetation. |
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Log jamb at
the start of the Saskatchewan
River gorge. |
Log bridge
over the Saskatchewan River gorge. (Extreme
Caution Here). |
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Saskatchewan
River gorge. |
Saskatchewan
River gorge. |
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south east
face of Mount Andromeda |
Saskatchewan
River braided on the
ground moraine
leading to the glacier. |
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Striation on
rocks. |
More Alberta Rocks. |
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Cliffs and
waterfall on south side of valley. |
Cliffs and
waterfall on south side of valley. |
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Glacial polish
and
striation on
rocks. |
More Alberta Rocks. |
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Trilobites |
Trilobites |
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Trilobites |
Trilobites |
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Trilobites |
Trilobites |
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Rolling hills
of
glacial
deposits. |
Paternoster lake
and stagnant ice covered in rock. This is or
was an outflow. |
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Saskatchewan Glacier
(More Here) |
Saskatchewan Glacier
(More Here) |
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Paternoster lake
and stagnant ice covered in rock. This is or
was an outflow. |
Kettle
lake and tents near
the toe of Saskatchewan Glacier. |
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Tents near
the toe of the Saskatchewan Glacier.
(More Here) |
Tents near
the toe of Saskatchewan Glacier.
(More Here) |
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Paternoster lakes |
Glacial
deposits and
Paternoster lakes |
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Looking
towards Castleguard meadows. Mount
Castleguard on right. |
Medial
Moraine to right of glacier. This was level
with the ice in 1990. |
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(More Here) |
(More Here) |
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Saskatchewan Glacier |
Saskatchewan Glacier |
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(More Here) |
(More Here) |
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Saskatchewan Glacier |
Eskers |
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(More Here) |
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Saskatchewan Glacier south Side of Valley. |
Saskatchewan Glacier north Side of Valley
and
rock flour. |
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Till plains
looking down the valley. |
Till plains
looking down the valley. |
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Till plains
looking towards glacier. |
Till plains
looking down the valley. |
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Till plains
looking towards glacier. |
Till plains
looking towards glacier. |
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Erratics |
Eskers |
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More
Hikes |
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