Reedy Glacier

The Reedy Glacier (-85.5°N, -134°W) is a major glacier in Antarctica, over 100 nmi long and 6 to 12 nmi wide, descending from the polar plateau to the Ross Ice Shelf between the Michigan Plateau and Wisconsin Range in the Transantarctic Mountains. It marks the limits of the Queen Maud Mountains on the west and the Horlick Mountains on the east.

Naming
The Reedy Glacier was mapped by United States Geological Survey (USGS) from surveys and United States Navy (USN) air photos, 1960–64. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for Rear Admiral James R. Reedy, USN, Commander, U.S. Naval Support Force, Antarctica, from November 1962 until April 1965.

Topography and ice flow
The Reedy Glacier is the most southern large glacier that drains ice through the Transantarctic mountains from the Antarctic Plateau. It drains about 25000 km2 of the polar plateau, with its catchment extending from 200 km south of the South Pole. It flows 140 km from the edge of the polar plateau at -86.5°N, -140°W to become the Mercer Ice Stream at -85°N, -140°W in the southeast corner of the Ross Sea embayment. It is the only large glacier that flows from the Transantarctic mountains into grounded ice in the Ross Sea, although during the Last Glacial Maximum other glaciers also flowed into grounded ice.

The Reedy Glacier is almost 20 km wide at its head and its mouth. It narrows to 9 km in the central section, where for 15 km it flows past cliffs that rise 200 to 600 m above the glacier surface. The Wisconsin Range to the east and the Queen Maud Mountains to the west holds peaks that rise over 2000 m above sea level. At the head of the glacier the ice surface is almost 2000 m above sea level, while at its mouth it is 600 m above sea level. Ice thickness is up to 2000 m.

At the Quartz Hills the center-line velocity is 170 m per year. Elsewhere center-line velocities range from 100 to 200 m per year. Kansas Glacier is the largest tributary, joining the Reedy Glacier 100 km from its head. Other tributaries contribute little to the volume of ice flow. After entering the Ross Ice Shelf the Reedy Glacier becomes the Mercer Ice Stream. In the past it has been at least 250 m thicker than at present.

During the last 290 Ma the glacier has expanded at least six times, each time less than before, with the last expansion during the Last Glacial Maximum, when the ice sheet was up to 500 m thicker than today. The glacier flows into the ice sheet about 100 km behind the Ross Sea grounding line, so the flow and thickness of the glacier are, at least in part, controlled by the damming effest of the West Antarctic Ice Sheet. Reedy Glacier was considerably thicker than it is today at several times in the mid to late Cenozoic. For at least five million years the changes of thickness correlate with changes in thickness of the West Antarctic Ice Sheet.

Course
From the polar plateau the Reedy Glacier flows north past the Spear Nunatak, Strickland Nunatak and Savage Nunatak. It passes the Metavolcanic Mountain to the east and the Watson Escarpment to the west. Past the Gratton Nunatak it is joined from the east by the McCarthy Glacier and the Olentangy Glacier. It is joined from the west by the Wotkyns Glacier and the Gardiner Glacier flowing from the Watson Escarpment. It flows northwest past the Wisconsin Range to the east, from which it receives the Norfolk Glacier and the Hueneme Glacier. Past the Quartz Hills to the west it receives the Colorado Glacier.

Below Blubaugh Nunatak the Reedy Glacier is joined from the west by the large Kansas Glacier. The Kansas Glacier originates on the Stanford Plateau and is fed by the Johns Glacier from the south and Alaska Canyon from the north. The Reedy Glacier continues north past the Ford Nunataks to the east and Abbey Nunatak and Penrod Nunatak to the west. Near its termination it is joined from the east by the Horlick Ice Stream just after that has joined the Davisville Glacier, which has been joined by the Quonset Glacier from the east further upstream. The Reedy Glacier glacier flows northwest past Racine Nunatak and Cohen Nunatak to the west before entering the Ross Ice Shelf.

Except where otherwise stated, the features of the Reedy Glacier glacier region, described below, were mapped by the United States Geological Survey (USGS) from surveys and United States Navy air photos, 1960–64.

Left tributaries
Left (west) tributaries are, from south to north:

Wotkyns Glacier
-86.06667°N, -131.41667°W, A glacier flowing north from Michigan Plateau along the west side of Caloplaca Hills to enter the Reedy Glacier. Named by US-ACAN for Grosenvar S. Wotkyns, hospital corpsman at Byrd Station in 1962.

Gardiner Glacier
-86.01667°N, -131.8°W. A glacier at the south side of Quartz Hills, flowing east from Watson Escarpment into Reedy Glacier. Named by US-ACAN for Richard D. Gardiner, construction electrician at Byrd Station in 1962.

Colorado Glacier
-85.88333°N, -133.08333°W. A tributary glacier, 10 nmi long, draining northeast from Michigan Plateau to enter Reedy Glacier between the Quartz Hills and Eblen Hills. Named by US-ACAN for the University of Colorado, Boulder, CO, which has sent a number of research personnel to Antarctica.

Kansas Glacier
-85.7°N, -134.5°W. A steep glacier, 25 nmi long, draining northeast from Stanford Plateau to enter Reedy Glacier just north of Blubaugh Nunatak. Named by US-ACAN for the University of Kansas, Lawrence, KS, which has sent a number of research personnel to Antarctica.

Johns Glacier
-85.8°N, -136.5°W. An arc-shaped glacier 8 nmi long in the northern part of Watson Escarpment. It drains eastward around the northern side of Mount Doumani to join the Kansas Glacier. Named by US-ACAN for Lt. Ernest H. Johns, USN, a participant in several deployments of Operation Deep Freeze, 1955-68.

Right tributaries
Right (east) tributaries are, from south to north:

McCarthy Glacier
-86.06667°N, -127.4°W. A broad glacier at the south side of Wisconsin Plateau, flowing west to merge with the lower part of Olentangy Glacier before entering Reedy Glacier just southwest of Mount McNaughton. Named by US-ACAN for Lt. Robert J. McCarthy, USN, pilot on flights to the general area during Operation Highjump, 1946-47.

Olentangy Glacier
-86°N, -127.33333°W. A glacier draining that portion of the Wisconsin Plateau of the Horlick Mountains that stands east-north-east of Sisco Mesa, flowing south to merge into McCarthy Glacier and the larger Reedy Glacier to the southwest of Mount McNaughton. The name was proposed by the Ohio State University geological party to the Horlick Mountains, 1964-65. The Olentangy River flows through the University campus.

Norfolk Glacier
-85.88333°N, -130.3°W. A glacier, 12 nmi long, draining westward from Wisconsin Range to enter Reedy Glacier between Mount Soyat and Mount Bolton. Named by US-ACAN after Norfolk, VA, location of Detachment Three, the Meteorological Support Unit of the U.S. Naval Support Force, Antarctica.

Hueneme Glacier
-85.81667°N, -131.25°W. A glacier, 8 nmi long, draining westward from Wisconsin Range to enter Reedy Glacier between Griffith Peak and Mickler Spur. Named by US-ACAN for Port Hueneme, CA, location of the Construction Battalion Center which handles west coast cargo for USN Deep Freeze Operations.

Horlick Ice Stream
-85.28333°N, -132°W. A large ice stream on the featureless ice surface to the north of the main mass of the Horlick Mountains, draining west-southwestward, paralleling these mountains, to enter the lower portion of the Reedy Glacier. Named by US-ACAN in association with Horlick Mountains.

Davisville Glacier
-85.28333°N, -128.5°W. A glacier about 30 nmi long which drains the north slopes of the Wisconsin Range, between Lentz Buttress and Moran Buttress, and trends northwestward to merge with the lower portion of the Horlick Ice Stream. Named by US-ACAN for Davisville, Rhode Island, location of the Construction Battalion Center responsible for cargo matters for USN Operation Deep Freeze on the east coast.

Quonset Glacier
-85.31667°N, -127.08333°W. A glacier about 20 nmi long which drains the north slopes of Wisconsin Range between Mount LeSchack and Ruseski Buttress and trends west-northwest to enter the north side of Davisville Glacier. Named by US-ACAN after the Naval Air Station, Quonset Point, Rhode Island, home base of Antarctic Development Squadron Six (VXE-6).

Features
Nunataks and other isolated features along the course of the glacier were mapped by USGS from surveys and United States Navy air photos, 1960–64. They include, from south to north:

Spear Nunatak
-86.53333°N, -124.1°W. A nunatak lying 3 nmi south of Strickland Nunatak; apparently being the farthest south outcrop along the east side of the head of Reedy Glacier. Named by US-ACAN for Milton B. Spear, construction electrician, a member of the wintering party at Byrd Station in 1962.

Strickland Nunatak
-86.48333°N, -124.2°W. A large nunatak between Savage Nunatak and Spear Nunatak at the head of Reedy Glacier. Named by US-ACAN for Ernest E. Strickland, utilitiesman at Byrd Station in 1962.

Savage Nunatak
-86.45°N, -124.96667°W. A nunatak located 7 nmi southeast of Hatcher Bluffs, along the east margin of upper Reedy Glacier. Named by US-ACAN for Henry C. Savage, builder at Byrd Station in 1962.

Hatcher Bluffs
-86.33333°N, -125.6°W. A line of bluffs facing northwest, located 5 nmi south of Metavolcanic Mountain, at the east side of Reedy Glacier. Named by US-ACAN for Julius O. Hatcher, construction mechanic at Byrd Station in 1962.

Morales Peak
-86.25°N, -126.36667°W. A peak which rises from the south part of Metavolcanic Mountain, just east of Reedy Glacier. Named by US-ACAN for Tommy S. Morales, radioman at Byrd Station in 1962.

Metavolcanic Mountain
-86.21667°N, -126.25°W A large flat-topped mountain, 2,480 m high located 5 nmi north of Hatcher Bluffs on the east side of Reedy Glacier. Composed of dark metavolcanic rock, this mountain contrasts with lighter-colored granites elsewhere along the glacier. The name was suggested by geologist J.H. Mercer, Institute of Polar Studies, Ohio State University, following field work in the vicinity.

Mount Pool
-86.21667°N, -127°W. A peak, 2,090 m high, standing at the northwest side of Metavolcanic Mountain, at the east flank of Reedy Glacier. Named by US-ACAN for Douglas A. Pool, construction electrician at Byrd Station in 1962.

Gratton Nunatak
-86.1°N, -127.76667°W. A bare, linear nunatak lying at the south side of the mouth of McCarthy Glacier, where the latter enters Reedy Glacier. Named by US-ACAN for John W. Gratton, construction mechanic at Byrd Station in 1962.

Blubaugh Nunatak
-85.75°N, -134.1°W. A ridge-like nunatak located just south of the mouth of Kansas Glacier where it enters Reedy Glacier. Named by US-ACAN for Donald D. Blubaugh, construction mechanic, Byrd Station winter party, 1957.

Abbey Nunatak
-85.61667°N, -134.71667°W. A nunatak 2 nmi southeast of Penrod Nunatak, lying at the west side of Reedy Glacier just north of the mouth of Kansas Glacier. Mapped by USGS from surveys and USN air photos, 1960-64. Named by US-ACAN for Gordon Abbey, radioman with the Byrd Station winter party, 1957.

Penrod Nunatak
-85.58333°N, -134.88333°W. A nunatak 2 nmi northwest of Abbey Nunatak, lying at the west side of Reedy Glacier just north of the mouth of Kansas Glacier. Named by US-ACAN for Jack R. Penrod, builder with the Byrd Station winter party, 1957.

Langford Peak
-85.55°N, -135.38333°W. An isolated peak 2 nmi west of the lower part of Reedy Glacier and 5 nmi northwest of Abbey Nunatak. Named by US-ACAN for Lawrence G. Langford, Jr., a builder with the Byrd Station winter party, 1958.

Racine Nunatak
-85.46667°N, -136.3°W. Nunatak, 960 m, located 3 nmi west of the lower part of Reedy Glacier and 7 nmi ESE of Berry Peaks. Named by US-ACAN for Edward J. Racine, a member of the crew of the icebreaker Eastwind in Operation Deep Freeze 1967.

Cohen Nunatak
-85.4°N, -136.2°W. A nunatak lying 1 nmi west of the lower part of Reedy Glacier and 7 nmi east of Berry Peaks. Named by US-ACAN for Lt. (jg) Harvey A. Cohen, USNR, public affairs officer on the staff of the Commander, U.S. Naval Support Force, Antarctica, in Operation Deep Freeze 1966 and 1967.