The soaring spire of Mount Thielsen is the highest of several eroded volcanic remnants which mark the central part
of the Cascade Range in Oregon. A few hundred-thousand years ago, Thielsen was a broad shield volcano much like
its western neighbor across Diamond Lake, Mount Bailey. Several stages of heavy glaciation have stripped away the
outer cone, leaving behind only the hard remnants of solidified magma which mark the inner conduits, with broad
talus slopes occupying the gaps between the ridges. The summit spire itself requires one pitch of roped class-5
climbing and is unskiable under any conditions. Thielsen also hosts Oregon's most southerly glacier, the tiny
Lathrop Glacier, which is located in a small cirque at 8000 ft (2400 m) beneath the craggy cliffs of the north
face. However, the steep talus slopes (especially the Southwest Face) provide excellent ski terrain when
snow-covered in winter and spring, although they do not retain snow long into summer. Access is simple from the
Mount Thielsen trailhead near the resort area at Diamond Lake.
Route |
Ratings |
Starting Elevation |
Elevation Gain |
Roundtrip Distance |
Notes |
Quality |
Effort |
Ascent |
Descent |
Ski Mountaineering Routes:
NOTE: All ratings are for ski routes only up to the base of the summit pinnacle. |
Southwest Bowl (to summit climbing route) |
|
6.0 |
|
|
5300 ft (1600 m) |
3700 ft (1100 m) |
10 miles (16 km) |
The standard (and safest) climbing route to the summit of Thielsen follows
the Mount Thielsen Trail to its junction with the PCT near tree line and then heads up the
open, steepening slopes of the southwest bowl to the base of the summit pinnacle. The bowl
provides a variety of skiable lines, in early season starting from just below the summit
pinnacle on slopes approaching 40 degrees. Several of the lines pass through couloirs
between spectacular lava pinnacles which mark the upper portions of the bowl. The bowl
typically remains skiable into late spring, but the uppermost portions lose their
snowcover earliest due to the combined effects of wind and sun. An alternate slope
accessible from the same approach is the northwest bowl, which is skiable from a saddle
near 8500 ft just north of the summit, and due to its NW aspect may sometimes have better
snow conditions.
(See my ski trip report from June 1999.)
|
Northwest Bowl (from Thielsen Trailhead) |
|
5.5 |
|
|
3200 ft (1000 m) |
10 miles (16 km) |
North Bowl / Lathrop Glacier (from Howlock Trailhead) |
|
6.0 |
|
|
5300 ft (1600 m) |
2900 ft (900 m) |
13 miles (21 km) |
Howlock Mountain is a subsidiary peak which lies about 3 miles north of Mount Thielsen
along Sawtooth Ridge. This route initially follows the Howlock Trail, but then turns
southeast up the Thielsen Creek drainage to reach the meadows at Thielsen Camp on the PCT,
beneath the imposing (in fact slightly overhanging) North Face of the summit pinnacle. A
variety of slopes are skiable, including the Lathrop Glacier which reaches 8200 ft in a
cirque below the North Face, although the upper portions may have severe rockfall hazard.
|
|
Upcoming additions: |
Topographic map showing ski routes. |
|
Mount Thielsen from the SW along Highway 230 in June
(photo by Amar Andalkar) <click to enlarge>
|
Useful Web Links:
List of Guidebooks: (detailed references on the
bibliography page)
List of Maps:
Map Series |
Scale |
Topo? |
Map Names |
Year |
Notes |
USGS 7.5-minute |
1:24,000 |
Yes, 40 ft |
Mount Thielsen Diamond Lake |
1985 1985 |
First map covers everything needed, except trailheads are just off the edge |
US Forest Service |
1:126,720 |
No |
Umpqua National Forest |
1995 |
More current road and trail info than USGS maps |
More photos, routes, links, references, etc. coming soon...
Please contact me with any suggestions, additions, or corrections.
|