Exploration and naming
Benson Glacier was mapped in 1957 by the New Zealand Northern Survey Party of the Commonwealth Trans-Antarctic Expedition (1956–1958), and indicated as a somewhat longer glacier including the presentLocation
Midship Glacier divide features
Features of the terrain around the contact between Midship Glacier, Benson Glacier andJetsam Moraine
. A thin, sinuous medial moraine that arcs smoothly for from a point near Mount Razorback to beyond the far (northeast) side of Black Pudding Peak. Its curved trajectory marks the contact between Benson Glacier ice and that of Midship Glacier. So named by a 1989–1990 NZARP field party from association with Flotsam Moraines and because all supraglacial moraines are "floating" on the glacier ice, and drift similar to flotsam and jetsam.Mount Morrison
. A mountain, high, standing between Midship Glacier and the head of Cleveland Glacier. Discovered by the British National Antarctic Expedition (BrNAE) (1901–1904) and named after J. D. Morrison of the ''Morning'', a relief ship to the expedition.Flotsam Moraines
. The moraines trailing northeastward from Mount Morrison, trapped in the ice eddies between Midship Glacier and ice from local mountainside glaciers. So named by a 1989-90 NZARP field party from association with Jetsam Moraine and because all supraglacial moraines are "floating" on the glacier ice, and drift in a manner similar to marine flotsam and jetsam.Dogwatch Saddle
. A snow saddle between Mount Brøgger and Mount Morrison, separating the glacial catchments of the Benson Glacier and Cleveland Glacier. A NZARP field party made a late-night temporary camp on the saddle in January 1990. The name commemorates the midnight hours kept at this location.Mount Brøgger
. A mountain, high, which forms part of the north wall of Cleveland Glacier about north of Referring Peak. Charted by the British Antarctic Expedition (1910–1913) which named it for Professor Waldemar C. Brøgger, Norwegian geologist and mineralogist.Shipwreck Moraine
. An extensive moraine in a valley beside the Benson Glacier, between Black Pudding Peak and Mount Brøgger. Named by a 1989–1990 NZARP field party (Trevor Chinn) to commemorate an incident at the site. On a descent to the moraine, the motor toboggan and a sledge ran onto blue ice thinly disguised by snow and careened out of control down the slope, tossing gear and personnel overboard as the sledge overturned.Black Pudding Peak
. An isolated black mountain located northwest of Mount Brøgger. Named for its squat black appearance by the 1957 New Zealand Northern Survey Party of the CTAE, 1956–1958.Névé features
Feature of the Flight Deck Névé, the main source to Benson Glacier, include:Flight Deck Névé
. An elevated and unusually flat glacier névé, about by , between Flagship Mountain and Mount Razorback. The feature is the primary source of ice to the east-flowing Benson Glacier at Scuppers Icefalls. One of a group of nautical names in Convoy Range applied by NZGB in 1994.Holystone Slope
. A glacial slope distributary from Flight Deck Névé, wide, that descends northwest over subdued steps between Dotson Ridge and Dory Nunatak. Named by New Zealand Geographic Board (NZGB) (1993) in association with other nautical theme place names in the Convoy Range.Dory Nunatak
. An isolated sandstone nunatak, long, rising above the southwest part of Flight Deck Névé, southwest of Dotson Ridge. One of a group of nautical names in Convoy Range. So named by a 1989–1990 NZARP party because the feature appears to be sailing in the midst of the glacier névé like a small boat.Dotson Ridge
. A ridgelike nunatak, long, rising to high in the northwest part of Flight Deck Névé. Mapped by the United States Geological Survey (USGS) from ground surveys and Navy air photos. Named by the United StatesMount Davidson
. A mountain, high, standing at the head ofMount Nespelen
. A massive mountain, the highest in the coastal ranges between theScuppers Icefalls
. A prominent line of icefalls, long and nearly high high, between Mount Razorback and Mount Nespelen. The icefalls are the main outflow draining from Flight Deck Névé into Benson Glacier. One of a group of nautical names in Convoy Range, this descriptive name is derived from the drainage of the feature, suggestive of stormwater on a ship's deck draining through scuppers along the rail. Named by a NZARP field party, 1989–1990.Lower features
Features of the terrain near the coast include:Mount Whitcombe
. A large mountain, high, standing just north of Mount Perseverance and west of Mount Arrowsmith at the west side of Evans Piedmont Glacier. Mapped in 1957 by the New Zealand Northern Survey Party of the CTAE, 1956–1958. Named by them for its similarity to the Canterbury, New Zealand, mountain of the same name, and in association with Mount Arrowsmith.Mount Perseverance
. The high peak near the south end of the ridge from Mount Whitcombe, overlooking the lower Benson Glacier in Victoria Land. So named because it was the final station occupied by the New Zealand Northern Survey Party of the CTAE (1956-58) during a particularly long day's field work on October 22, 1957.Mount Arrowsmith
. A jagged rock peak near Mount Perseverance, along a ridge running northeast from that mountain, and a like distance east of Mount Whitcombe in Victoria Land. Mapped in 1957 by the New Zealand Northern Survey Party of the CTAE (1956–1958). Named by them for its similarity to the Canterbury, New Zealand, mountain of that name, and in association with Mount Whitcombe.Mount Forde
. A mountain over high, standing at the head ofReferences
Sources
* * * * {{Include-USGov , agency=United States Geological Survey Glaciers of Victoria Land Scott Coast