During the Pleistocene (~1.8 million years BP - 10,000 years BP) the Oregon Cascades may have been covered by glaciers creating a small ice cap (Porter et al., 1983). Scott (1977) inferred maximum glacial extents at Mount Jefferson to have occurred ~20 - 25,000 years ago, which is comparable to those found on Mt. Rainier, Washington. Licciardi et al. (2004) identified two glacial advances in the Wallowas, one at approximately 21,000 years ago and the other at 17,000 years ago. When compared with other glacial maximums from the western United States, the Wallowas illustrate the influence of the Laurentide Ice Sheet on the regional climate. Holocene (~10,000 years ago to the present) glacial fluctuations are better understood in Oregon.
Lillquist (1989) identified "Little Ice Age" (a global cool period from about 700 years ago to 150 years ago) moraines on Mount Hood and possibly moraines dating to approximately 4,500 - 5,000 years ago. "Little Ice Age" moraines have also been identified on Mount Jefferson (Scott, 1977), the Three Sisters (Marcott, 2005), and Broken Top (Dethier, 1980; Marcott, 2005). Other moraine sets downslope from the "Little Ice Age" moraines on the Three Sisters and Broken Top place glacial advances/stands at about 2,000 - 3,000 and 4,500 - 6,500 years ago. Another moraine set downslope of these pre-dates 7,700 years ago(Marcott, 2005). Kiver (1974) identified "Little Ice Age" moraines in the Wallowas as well as a morainal advance/stand at approximately 2,000 years ago (Prospect Lake). The moraines from the "Little Ice Age" and earlier dates indicate larger glaciers than presently exist.

Coleman (1877) credits the "discovery" of glaciers in Oregon to Lieutenant-Colonel Gordon Granger, who visited the glaciers of Mount Hood in 1840. However, Arnold Hague's descriptions of Mount Hood's glaciers were the first to be published (King, 1871). In 1867, the U.S. Congress passed legislation funding the War Department to survey all lands east of California along the 40th parallel and named Clarence King the geologist in charge. King sent Hague north from San Francisco in August, 1870. Hague examined the glaciers on the south side of the mountain while climbing to the summit in early September. King (1871) is credited with the first "discovery" of glaciers in the American West, during his climb of Shastina (a parasitic volcanic cone on the western flank of Mount Shasta) on September 11, 1870. However, Hague "discovered" the glaciers of Mount Hood at some point between September 4, 1870 and September 18, 1870 (Babson, 1997), and may deserve credit for "discovering" glaciers in the western United States before King. After this expedition, King became the first director of the United States Geological Survey.

Arnold Hague
(Iddings, 1919)

Clarence D. King, 1879
(USGS photo archives)

About 148 snow and ice bodies are found on Mt. Hood with a minimum elevation of 1295 m and maximum elevation of 3420 m with a mean of 2304 m and an area of 22.7 km². Of these perennial snow and ice features, 12 are named glaciers (all are labeled on the map on the right except Coalman Glacier, located in the crater at the summit) (USGS 1:24,000 scale topographic map, current edition 1996, created from 1956 aerial photographs).

Mount Hood is a stratovolcano comprised of mostly andesitic rock. The glaciers of the northern side are mantled with rock debris on their terminus's as a result of frequent rock avalanches from Hood's geothermally altered north face. The glaciers of the southern side are mostly "clean," that is, with little or no rock debris on the ice.

Shaded relief map of Mount Hood. Click on the map above for the full size version.

Map of Hood created by W.A. Langille, circa 1900. (Reid, 1905)

White River Glacier, 1901 (H.F. Reid)

Coe Glacier, 1901.(H.F. Reid)
Photo courtesty of Mazamas

Newton Clark Glacier, 1901 (H.F. Reid)
Photo courtesty of Mazamas

About 35 perennial snow and ice features are found on Mt. Jefferson with a minimum elevation of 1877 m and a maximum elevation of 2496 m with a mean of 2496 m and an area of 5.5 km². Of these snow and ice bodies, four are named glaciers (all are labeled on the map on the right) (USGS 1:24,000 scale topographic map, current edition 1997, created from 1949 aerial photographs). The glaciers of Mt. Jefferson are mostly confined to the north, east, and southeast slopes of the mountain. However, in the early twentieth century a glacier was described occupying the western flank of the mountain and was named "Milk Creek Glacier" (Milk Creek is the area under the "Mt. Jefferson" label on the map on the right). However, as Hatch (1917) stated, it was merely a glacial remnant of "stagnant ice" partially covered in debris. The current glacier coverages delineated on USGS 1:24,000 scale quadrangle maps (see figure at right) do not label this feature. As early as 1917, Hatch (1917) noted that Russel and Jefferson Park glaciers (along with the rest of the mountain) had undergone a recent retreat leaving behind well-defined lateral moraines. Hatch (1917) described Whitewater Glacier as approximately five miles wide and one to two miles long splitting into five lobes. Currently, however, Whitewater Glacier is only about three kilometers (1.9 miles) wide and just over one kilometer long.

Shaded relief map of Mount Jefferson. Click on map for a full sized version.

Aerial image of Mount Jefferson, 1979. (USGS)

August, 1917 map of Mount Jefferson created by R.J. Davidson (Hatch, 1917)

1937 oblique aerial photograph of Whitewater Glacier (center) and Waldo Glacier (far left), looking west, courtesy of Mazamas (A.J. Gilardi)

Whitewater Glacier. August 2007. (John Scurlock)

North/Middle Sisters

Shaded relief map of the North/Middle Sisters. Click on the map above for the full size version.

Middle and North Sisters, 2004 (S. Marcott)

South Sister

Shaded relief map of the South Sister. Click on the map above for the full size version.

Lewis Glacier and moraine-dammed lake, 2004 (M. Weaver)

South Sister and Green Lake, 2004 (S. Marcott)

South Sister (right) and Broken Top (left) from Middle Sister, 2005 (M.Weaver)

Unnamed perennial ice feature in the summit crater of South Sister, 2004 (M.Weaver)

Broken Top

About 33 perennial snow and ice features are found on Broken Top with a minimum elevation of 2152 m and a maximum elevation of 2736 m with a mean of 2382 m and an area of 3.3 km². Of these snow and ice bodies, two are named glaciers (both are labeled on the map on the right) (USGS 1:24,000 scale topographic map, current edition 1997, created from 1957 aerial photographs).

Many of the snow and ice bodies on Broken Top exist as a result of topographic shading as these bodies exist at a lower elevation than do those on the nearby Three Sisters.

Shaded relief map of Broken Top. Click on the map above for the full size version.

Broken Top and Bend Glacier, 2005 (M. Weaver)

Glacier and moraine-dammed lake to the east of Broken Top summit,1938 (K.N. Phillips, 1938)

One ice body (two lobes that are grouped as one glacier--Lathrop) is found on Mt. Thielsen and ranges in elevation from 2498 m to 2601 m with a mean of 2565 m and an area of 0.003 km² (USGS 1:24,000 scale topographic map, current edition 1998, created from 1994 aerial photographs).

Shaded relief map of Mount Thielsen. Click on the map above for the full size version.  

Lathrop Glacier, 1998 (R. Nafziger) Note how the glacier is shaded, helping to preserve the ice

Mount Thielsen essentially is a geomorphic feature called a horn. This is a glacially-modified peak, the most famous of which is the Matterhorn. Four cirques surround the mountain almost perfectly leaving four aretes and a horn, a classic example of glacial erosion. Lathrop Glacier was "discovered" in 1966 when Dr. Theodore Lathrop peered from the summit down the north face of Mt. Thielsen and thought the two small snow and ice bodies he saw might be an active glacier. Starting in 1968, Dr. Lathrop's nephew, Ralph Nafziger and others began monitoring Lathrop Glacier's east and west lobes with photographs after repeated attempts at placing stakes in the glacier surface failed.Lathrop Glacier lies in a shady northeastern slot and is the last remaining glacier on Thielsen and the southernmost glacier in Oregon.

Click HERE for a photographic record of Lathrop Glacier, donated by Ralph Nafziger of Albany, Oregon.

Dr. Theodore Lathrop on Lathrop
Glacier, 1968.(J.Torrance)

About 131 perennial snow and ice features are found in the Wallowa Mountains with a minimum elevation of 2297 m and a maximum elevation of 2898 m with a mean of 2688 m and an area of 1.5 km². Of these snow and ice bodies, only one is a named glacier (USGS 1:24,000 scale topographic maps, current edition 1990, created from 1981 aerial photographs).

The Wallowas were once heavily glaciated, as displayed by large U-shaped glacial valleys as well as cirques (a bowl-shaped depression resulting from glacial erosion). Wallowa Lake is a moraine-dammed lake, the moraines were formed during the last ice age. However, it is highly unlikely that any of the blue areas identified on this map are more than perennial snowpacks. Benson Glacier (below), named for Frank W. Benson, an early governor of Oregon, is located on Eagle Cap (see figure at right), and may still be an active glacier.

Shaded relief map of the Wallowas. Click on the map above for the full size version.

Repeat photograph of Benson Glacier (Skovlin et al., 2001)

Benson Glacier. September 2007. John Scurlock

Sholes Glacier:

Located on Mount McLoughlin, about 85 km south of Mount Thielsen, was "discovered" in 1896, but by 1939 it had vanished (Phillips, 1939).

Sholes Glacier: left image from 1896 (B.W. Evermann), right image from 1939 (K.N. Phillips)

Timberline Glacier:

Located on Mount Jefferson, Timberline Glacier was photographed (right) and described by Phillips (1938) but no longer is shown or labeled on maps.

Timberline Glacier, 1937 (A.J. Gilardi)

Milk Creek Glacier:

Located on Mount Jefferson, Milk Creek Glacier occupied the western slope of the mountain (two adjacent lobes) when first explored by Williams in 1916 (Hatch, 1917), but by 1938 (below) was merely a glacial remnant and currently is not labeled on United States Geological Survey 1:24,000 scale topographic maps.

Milk Creek Canyons, 1937 (A.J. Gilardi)

Glacial remnant of Milk Creek Glacier, 1938 (K.N.Phillips)

Jack Glacier:

Located on Three Fingered Jack and described by Phillips (1938), Jack Glacier is no longer labeled on United States Geological Survey maps and may no longer exist. However, this aerial photograph from September 14, 1990 (below) displays remaining patches of ice, and its extremely well-protected location limits solar radiation and may be the ideal location for a glacier to still remain.

Jack Glacier, 1937 (A.J. Gilardi)

Jack Glacier, 1990 (USFS)

Crater Glacier:

Located on Broken Top, Crater Glacier is actually mistakenly labeled as Crook Glacier on the 1:24,000 scale United States Geological Survey topographic quadrangle maps. Phillips (1938) identified Crater Glacier as well as nearby Crook Glacier (several hundred meters to the east) but when the topographic maps were created in 1957 Crater Glacier was labeled Crook Glacier and Crook Glacier received no name. Crater Glacier was smaller and less protected from solar radiation and has possibly disappeared since the 1966 oblique aerial photograph below.

Broken Top, looking northwest, 1956 (H. Ackroyd)

September 22, 1966 (A. Post)

Dutchman Glacier:

Located on Bachelor Butte, in the early 1920's Dutchman Glacier extended down to a moraine-dammed lake, but by 1938 had retreated to what most likely was a stagnant body of ice with no crevasses (Phillips, 1938). Current United States Geological Survey topographic quadrangle maps do not show any remaining perennial snow or ice on Bachelor Butte. However, in 1967, an ice body still remained (below) and may still persist.

Dutchman Glacier, 1938 (K.N. Phillips)

September 19, 1967 (A. Post)

Diamond Glacier:

Located on Diamond Peak, Diamond Glacier was "discovered" in 1938 by Harry L. Clark and Kenneth N. Phillips (Phillips, 1938). This was the southernmost glacier in Oregon, but currently is most likely no longer present. Current United States Geological topographic quadrangle maps do not show the glacier.

Diamond Glacier, 1938 (K.N. Phillips)

• Mt. Hood was first climbed on July 11, 1857 by Henry Lewis Pittock (employee for the Weekly Oregonian newspaper), W. Lyman Chittenden, Wilbur Cornell, and the Rev. T.A. Wood (McNeil, 1937).
• The Three Sisters were named Faith, Hope, and Charity by early settlers ( Cascades Volcano Observatory website ¹).
• A section of land three miles southwest of South Sister is bulging at a rate of 3.6 cm a^-1 ( Cascades Volcano Observatory website ²).
• The Historic Cloud Cap Inn was constructed on Mount Hood's northeast side on a volcanic satellite cone at 1825 m elevation in 1889 and is currently in use by the Crag Rats search and rescue organization ( website )
• The Palmer Glacier (originally named the "Salmon River Glacier") was not discovered until the very warm summer of 1924 exposed crevasses on what was previously assumed to only be perennial snow (Nelson, 1924). In fact, George Calverley dropped a horse into a crevasse the following summer (Grauer, 1975). Since then, however, these crevasses have never been exposed nor caused any problems.
• The Oregon state flower is the oregon grape (Mahonia aquifolium). The state beverage of Oregon is milk (Dairycus milkium)
• Membership in the Mazamas, a Portland-based outdoor club,  requires that applicants have climbed a mountain with a glacier.

• This is a photograph of Arnold Hague's saddle, which he used on his western expeditions ( United States Geological Survey ):

Babson, S.G. 1997. Letters from Arnold Hague: early Mount Hood explorer, editor. Oregon Historical Quarterly, Summer 1997.

Cascades Volcano Observatory Website - Three Sisters Volcanoes, Oregon.http://vulcan.wr.usgs.gov/Volcanoes/Sisters/description_three_sisters.html Last accessed 01-Dec-2005.

Coleman, E.T. 1877. Mountains and Mountaineering in the Far West. The Alpine Journal, 8:233-242.

Dethier, D.P. 1980. Reconnaissance study of Holocene glacier fluctuations in the Three Sisters area, Oregon. EOS Transactions, American Geophysical Union 61:69.

Iddings, J.P. 1919. Biographical Memoir of Arnold Hague 1840-1917. National Academy of Sciences of the United States of America: Biographical Memoirs. Vol IX.

Grauer, J. F. 1975. Mount Hood: A complete history. Privately printed.

Hatch, L. 1917. The glaciers of Mt. Jefferson. Mazama, 134-139.

Hodge, E.T. 1925. Mount Multnomah, ancient ancestor of the Three Sisters: Univ. Oregon Publication. Vol 3, no. 2. Eugene, Oregon.

Jackson, K., and A.G. Fountain. 2007. Spatial and morphological change on Eliot Glacier, Mount Hood, Oregon, USA. Annals of Glaciology 46: 222-226.

King, C. ,1871. Active Glaciers within the United States. Atlantic Monthly, 27:8 March 371-377.

Kiver, E.P. 1974. Holocene glaciation in the Wallowa Mountains, Oregon. In: Mahaney, W.C. (ed.) Quaternary Environments Proceedings of a Symposium: Geographical Monographs No. 5 , York University, Toronto, Canada.

Licciardi, J.M., Clark, P.U., Brook, E.J., Elmore, D., and Sharma, P. 2004. Variable responses of western U.S. glaciers during the last deglaciation. Geological Society of America , 32:81-84.

Lillquist, K.D. 1989. Holocene Fluctuations of the Coe Glacier, Mt. Hood, Oregon. M.S. Thesis, Portland State University, Portland, Oregon.

Marcott, S. 2005. A tale of Three Sisters: Reconstructing the Holocene glacial history and paleoclimate record at Three Sisters Volcanoes, Oregon, United States. M.S. Thesis, Portland State University, Portland, Oregon.

McNeil, F.H. 1937. Wy'east "The Mountain" . United States: Metropolitan Press.

Nelson, L.A. 1924. A new glacier on Mt. Hood. Mazama, 67-70.

Phillips, K.N. 1938. Our vanishing glaciers. >Mazama, 24-41.

Phillips, K.N. 1939. Farewell to Sholes Glacier. Mazama,37-40.

Porter, S.C., Pierce, K.L., and Hamilton, T.D. 1983. Late Wisconsan mountain glaciation in the Western United States, in Porter, S.C., ed., Late-Quaternary Environments of the United States, Volume 1: Minneapolis, University of Minnesota Press, p. 71-111.

Reid, H.F. 1905. The glaciers of Mt. Hood and Mt. Adams. Mazama, 195-200.

Scott, W.E., 1977. Quaternary Glaciation and Volcanism, Metolius River area, Oregon. Geological Society of America Bulletin, 88:113-124.

Skovlin, J.M., Strickler, G.S., Peterson, J.L., and Sampson, A.W. 2001. Interpreting landscape change in high mountains of northeastern Oregon from long-term repeat photography. United States Department of Agriculture General Technical Report PNW-GTR-505.

Williams, I.A. 1916. Glaciers of the Three Sisters. Mazama, 14-23.