PSU Inventory Reveals Shrinking, Vanishing Glaciers

Portland State University

The Western United States is losing its glaciers.

A new inventory from Portland State University researchers show that some glaciers have disappeared entirely, some no longer show movement, some are too small to meet the 0.01 square kilometer minimum and some are actually rock glaciers — rocky debris with ice in the pore spaces.

Andrew Fountain, a geology professor emeritus at PSU, and research assistant Bryce Glenn, inventoried glaciers and perennial snowfields in the western continental U.S. using aerial and satellite imagery between 2013 and 2020. The inventory, published in the journal Earth System Science Data, identified 1,331 glaciers and 1,176 perennial snowfields.

It updates a mid-20th century inventory, derived from U.S. Geological Survey topographic maps made over a 40-year span, and provides a baseline for estimating future changes amid a warming climate.

"Glaciers are disappearing and this is a quantification of how many around us have disappeared and will probably continue to disappear," Fountain said.

The new inventory excludes 52 of the 612 officially named glaciers because they are no longer glaciers. The official names are those listed in the federal Geographic Names Information System — the nation's repository for the names and locations of landscape features. Milk Lake Glacier in Washington's Mt. Baker-Snoqualmie National Forest and Wyoming's Hooker Glacier have disappeared altogether; 25 were instead classified as perennial snowfields, which unlike glaciers don't move; 18 had areas smaller than the commonly used threshold of 0.01 square kilometers or roughly the size of two football fields side-by-side; and seven were considered rock glaciers.

The loss of glaciers impacts more than aesthetics. Glaciers act as a natural regulator of streamflow, Fountain said. They melt a lot during hot dry periods and don't melt much during cool rainy periods. As glaciers shrink, they have less ability to buffer seasonal runoff variations and watersheds become more susceptible to drought. Retreating glaciers also leave behind sharp, steep embankments on either side, which can collapse and result in catastrophic debris flows. Globally, the loss of glaciers is also a major contributor to sea level rise.

Fountain's co-authors are Bryce Glenn, a PSU alum and research analyst, and Christiopher McNeil, a geophysicist with the USGS' Alaska Science Center. Looking ahead, the group is studying the volume change of the glaciers to see how much ice they've lost since the USGS mapping.

Missing Glaciers: List of officially named glaciers not classified as glaciers and excluded from the final inventory

StateRegionGlacier NameReason
CaliforniaSierra NevadaMatthes Glaciersrock glacier
CaliforniaSierra NevadaMount Warlow Glacierrock glacier
CaliforniaSierra NevadaPowell Glacierrock glacier
ColoradoFront RangeIsabelle Glacierperennial snowfield
ColoradoFront RangeMills Glacierperennial snowfield
ColoradoFront RangeMoomaw Glacierperennial snowfield
ColoradoFront RangePeck Glacierperennial snowfield
ColoradoFront RangeRowe Glacier2
ColoradoFront RangeSaint Marys Glacier2
ColoradoFront RangeTaylor Glacierrock glacier
ColoradoFront RangeThe Dove2
IdahoLost River RangeBorah Glacierrock glacier
MontanaBeartooth Mountains–Absaroka RangeGrasshopper Glacierrock glacier
MontanaCabinet MountainsBlackwell Glacierperennial snowfield
MontanaCrazy MountainsGrasshopper Glacierrock glacier
MontanaLewis RangeBoulder Glacierperennial snowfield
MontanaMission–Swan–Flathead rangesFissure Glacier2
MontanaMission–Swan–Flathead rangesGray Wolf Glacierperennial snowfield
OregonCascade RangeCarver Glacierperennial snowfield
OregonCascade RangeClark Glacierperennial snowfield
OregonCascade RangeIrving Glacierperennial snowfield
OregonCascade RangeLathrop Glacier2
OregonCascade RangePalmer Glacierperennial snowfield
OregonCascade RangeSkinner Glacierperennial snowfield
OregonCascade RangeThayer Glacier2
OregonWallowa MountainsBenson Glacierperennial snowfield
WashingtonCascade Range–NorthernLyall Glacierperennial snowfield
WashingtonCascade Range–NorthernMilk Lake Glacierdisappeared
WashingtonCascade Range–NorthernSnow Creek Glacierperennial snowfield
WashingtonCascade Range–NorthernSpider Glacierperennial snowfield
WashingtonCascade Range–NorthernTable Mountain Glacier2
WashingtonCascade Range–SouthernApe Glacier2
WashingtonCascade Range–SouthernDryer Glacierperennial snowfield
WashingtonCascade Range–SouthernForsyth Glacier2
WashingtonCascade Range–SouthernMeade Glacierperennial snowfield
WashingtonCascade Range–SouthernNelson Glacier2
WashingtonCascade Range–SouthernPackwood Glacierperennial snowfield
WashingtonCascade Range–SouthernPinnacle Glacier2
WashingtonCascade Range–SouthernPyramid Glaciers2
WashingtonCascade Range–SouthernShoestring Glacier2
WashingtonCascade Range–SouthernStevens Glacierperennial snowfield
WashingtonCascade Range–SouthernTalus Glacierperennial snowfield
WashingtonCascade Range–SouthernUnicorn Glacier2
WashingtonCascade Range–SouthernWilliwakas Glacierperennial snowfield
WashingtonOlympic MountainsAnderson Glacierperennial snowfield
WashingtonOlympic MountainsLillian Glacier2
WyomingAbsaroka RangeDuNoir Glacier2
WyomingTeton RangePetersen Glacier2
WyomingTeton RangeTeepe Glacierperennial snowfield
WyomingWind River RangeHooker Glacierdisappeared
WyomingWind River RangeHarrower Glacierperennial snowfield
WyomingWind River RangeTiny Glacier2
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