Crary Mountains

Crary Mountains (Template:Coord) are a group of ice-covered volcanoes in Marie Byrd Land, Antarctica. They consist of two or three shield volcanoes, named Mount Rees, Mount Steere and Mount Frakes, which developed during the course of the Miocene and Pliocene and last erupted about 30,000-40,000 years ago. The first two volcanoes are both heavily incised by cirques, while Mount Frakes is better preserved and has a Template:Convert wide caldera at its summit. Boyd Ridge is another part of the mountain range and lies southeast of Mount Frakes; it might be the emergent part of a platform that underlies the mountain range.

The volcanoes consist mainly of basalt, trachyte and phonolite in the form of lava flows, scoria and hydrovolcanic formations. Volcanic activity here is linked to the West Antarctic Rift system, which is responsible for the formation of a number of volcanoes in the region. During their existence, the range was affected by glaciation and glacial-volcanic interactions. Template:TOC limit

Geography and geomorphology

The mountain range lies in eastern Marie Byrd Land, Antarctica,Template:Sfn about Template:ConvertTemplate:Sfn from the Bakutis Coast.Template:Sfn It was first visited in 1959–1960, and several accessible outcrops were sampled. The name refers to Albert P. Crary, who was then Deputy Chief Scientist for the US-IGY Antarctic Program.Template:Sfn

The Crary Mountains are a chain of threeTemplate:Sfn shield volcanoesTemplate:Sfn Template:Convert longTemplate:Sfn which extends in northwest–southeast direction.Template:Sfn The volume of the volcanoes exceeds Template:Convert and the edifices consist of lavas, hydrovolcanic deposits such as hyaloclastite, fragments of pillow lavas and tuffs, and scoria.Template:Sfn Unlike many other mountains in Marie Byrd Land, which owing to a lack of erosion display only their highest and youngest parts, in the Crary Mountains the internal structure of the volcanoes are well exposedTemplate:Sfn due to glacial erosion.Template:Sfn The Crary Mountains form a drainage divide for the West Antarctic Ice Sheet;Template:Sfn they dam it, which is thus higher on the southwestern side of the range.Template:Sfn Debris stripes have been observed on the ice near the foot of the mountains.Template:Sfn

The northeasternmost volcano is Mount Rees, which reaches a summit height of Template:Convert at Tasch Peak. Volcanic rocks crop out at Trabucco Cliff on its northeastern flank.Template:Sfn There is no caldera.Template:Sfn Glacial erosion has cut deep cirques into the eastern flank of Mount Rees, and volcanic outcrops indicate that volcanic rocks alternate between subglacial formations and subaerial formations. Outcrops consist of breccia and lavas, which in one case are intruded by a dike.Template:Sfn

File:MountFrakesSteere.jpg

Mount Frakes and Mount Steere

In the middle of the chain lies Mount Steere with a summit elevation of Template:Convert and a rectangular summit caldera. Lie Cliff is a volcanic outcrop on the northeastern flank.Template:Sfn Mount Steere is heavily dissected,Template:Sfn bears evidence of former glaciation in the form of morainesTemplate:Sfn and cirques have been eroded into its northern and northeastern flanks. As with Mount Rees, volcanic rocks alternate between these that formed subglacially and these formed subaerially. Outcrops feature breccias and lava with numerous intruded dikes.Template:Sfn

South of Mount Steere is Mount Frakes, with Template:Convert it is the highest peak in the rangeTemplate:Sfn and the least eroded of the Crary Mountains.Template:Sfn It has a Template:Convert wide circular summit caldera and unlike Mount Rees and Mount Steere it bears no evidence of subglacial eruptions, probably due to lack of erosion that could have exposed them.Template:Sfn Volcanic rocks crop out both on the southern and western flank, at Morrison Rocks and English Rock respectively.Template:Sfn These outcrops are cinder cones that formed on the slopes of Mount Frakes.Template:Sfn Volcanic and nonvolcanic boulders on the slopes of Mount Frakes may either be xenoliths or glacial erratics.Template:Sfn

Boyd Ridge is smaller than the other three volcanoesTemplate:Sfn and located southeast of Mount Frakes and reaches an elevation of Template:Convert.Template:Sfn Runyon Rock crops out to its eastTemplate:Sfn and is the only area of Boyd Ridge not covered by ice. Cinders and a cliff of hyaloclastite are found there.Template:Sfn

The volcanoes rise from a platform formed by lava flows and pyroclastic rocks.Template:Sfn This platform lies at about Template:Convert elevation and the Boyd Ridge may be a southeastward extension thereof. It appears that the platform — which crops out only on the eastern side of the Crary Mountains — was tilted westward by faulting.Template:Sfn Echo and magnetic sounding have imaged the root of the Crary Mountains in the West Antarctic Ice Sheet, finding that the underlying terrain is steep and flanked by narrow troughs.Template:Sfn The mountains are associated with a strong magnetic anomaly that may reflect subglacial rocks containing magnetite.Template:Sfn

Geology

Cenozoic volcanism in Marie Byrd Land is related to the West Antarctic Rift and has been explained by the activity of a mantle plume. This plume either underlies Marie Byrd Land and its volcanoes, or it rose to the surface before Antarctica separated from New Zealand during the middle Cretaceous and induced volcanism across the continental borderlands of the Southwest Pacific. In the latter theory, the Marie Byrd Land volcanism is caused by a remnant plume head underneath the continent.Template:Sfn The basement crops out along the coast and consists of granitoids and metamorphic sediments left by a Devonian-Cretaceous volcanic arc.Template:Sfn

This volcanism manifests itself with 18 large and numerous smaller volcanoes, which occur in groups, rows or as solitary systems in Marie Byrd Land. The larger centres have produced phonolite, rhyolite, trachyte and rocks with intermediate compositions, and reach heights of over Template:Convert above sea level.Template:Sfn The smaller centres are found at the foot of the larger centres, as parasitic vents on their slopes or along the coast. These vents have produced alkali basalt, basanite and hawaiite.Template:Sfn

Composition

Basalt occurs at all four volcanoes. Phonolite and trachyte are found at Mount Rees and Mount Steere, the former also at Mount Frakes; Mount Rees also features rhyolite. Phenocrysts include clinopyroxene, magnetite, olivine and plagioclase.Template:Sfn The magma erupted in the Crary Mountains originated in the mantle and underwent fractional crystallization after formation.Template:Sfn

Geologic history

The Crary Mountains were active between 9.3 and 0.04 million years agoTemplate:Sfn during the Miocene and Pliocene.Template:Sfn The youngest dates have been obtained by argon-argon dating on Mount Frakes, and imply an eruption 35,000±10,000–32,000±10,000 years ago.Template:Sfn These ages were obtained on English Rock, which has also yielded ages of 826,000±79,000–851,000±36,000Template:Sfn and 1.62±0.02 million years ago.Template:Sfn Tephra deposits in ice cores recovered at Byrd Station may have originated at Marie Byrd Land volcanoes such as these of the Crary Mountains.Template:Sfn

The maximum age of each volcano decreases in southeastward direction, from 9.34±0.24 million years old Mount Rees to 2.67±0.39 million years old Boyd Ridge. The pattern of volcanism migrating along the chain has been observed at other mountain ranges such as the Executive Committee Range, where it takes place at a pace of Template:Convert like at the Crary Mountains. It is directed away from the centre of the Marie Byrd Land volcanic province and may reflect the propagation of a fracture in the crust.Template:Sfn

West Antarctica has been subject to glaciation since the Oligocene, where a perhaps local ice cap or snow deposit existed at Mount Petras. Volcanoes erupting through ice leave specific geologic structures which can be used to reconstruct the timing and extent of past glaciations.Template:Sfn Geologic evidence at the Crary Mountains implies that a substantial West Antarctic Ice Sheet existed during the Miocene, and that fluctuations in its size may have stressed the crust and modulated the activity of volcanoes in its area.Template:Sfn Before its formation the Crary Mountains might have been islands.Template:Sfn In the Crary Mountains, ice occurred either in the form of slope ice when the mountains were eruptingTemplate:Sfn or as a thick continental ice sheet.Template:Sfn The glaciers were cold-based and thus did not produce tillites or glacial surfaces,Template:Sfn and were probably thin.Template:Sfn Glacial erosion took place mainly between 8.55 and 4.17 million years ago; it formed the cirques in Mount Rees and Mount SteereTemplate:Sfn and transported glacial erratics on the mountains.Template:Sfn

Named features

File:C76114s1 Ant.Map Crary Mountains.jpg

Crary Mountains in southwest of map

Named features, from northwest to southeast, include Trabucco Cliff, Mount Rees, Tasch Peak, White Valley, Mount Steere, Lie Cliff, Mount Frakes, English Rock, Morrison Rocks, Campbell Valley, Boyd Ridge and Runyon Rock.Template:Sfn The features were all mapped by the United States Geological Survey (USGS) from surveys and United States Navy aerial photography in 1959–66.Template:Sfn

Trabucco Cliff

Template:Coord. A cliff at the tip of the broad spur which forms the northeast extremity of Mount Rees. Named by the United States Advisory Committee on Antarctic Names (US-ACAN) for William J. Trabucco, United States Antarctic Research Program (USARP) ionospheric physicist at McMurdo Station, 1969, and Siple Station, 1973.Template:Sfn

Mount Rees

{{#invoke:Labelled list hatnote|labelledList|Main article|Main articles|Main page|Main pages}} Template:Coord. Mountain located Template:Convert northwest of Mount Steere in the north end of Crary Mountains. Named by US-ACAN for Manfred H. Rees, aurora scientist at Byrd Station, 1965–66 season.Template:Sfn

Tasch Peak

Template:Coord. A rocky peak in the southeast portion of Mount Rees. Named by US-ACAN for Paul Tasch, USARP geologist in the Sentinel Range and Ohio Range, summer 1966–67, and Coalsack Bluff, 1969–70.Template:Sfn

White Valley

Template:Coord. A broad ice-covered valley that indents the northern part of Crary Mountains between Trabucco Cliff and Lie Cliff. Named by US-ACAN for Franklin E. White, USARP ionospheric physicist at Byrd Station in four summer seasons, 1966–71.Template:Sfn

Mount Steere

Template:Coord. Prominent mountain Template:Convert high standing Template:Convert north-northwest of Mount Frakes. Named by US-ACAN for William C. Steere, biologist at McMurdo Station, 1964–65 season.Template:Sfn

Lie Cliff

Template:Coord. A prominent rock cliff at the eastern foot of Mount Steere. Named by US-ACAN for Hans P. Lie, USARP ionospheric physicist at Siple Station in the 1970–71 and 1973-74 summer seasons.Template:Sfn

Mount Frakes

Template:Coord. A prominent mountain Template:Convert high marking the highest elevation in the Crary Mountains. Named by US-AC AN for Lawrence A. Frakes, USARP geologist who worked three summer seasons in the Falkland Islands and Antarctica, 1964-65 through 1967–68.Template:Sfn

English Rock

Template:Coord. A rock outcrop near the foot of the western slope of Mount Frakes. Named by US-ACAN for Claude L. English Jr., United States Navy, helicopter crewman with Squadron VXE-6 during Deep Freeze 1970; he also deployed with the Squadron during Deep Freeze 1961, 1962 and 1965.Template:Sfn

Morrison Rocks

Template:Coord. A group of rocks which outcrop along the southern slope of Mount Frakes. Named by US-ACAN for Paul W. Morrison, United States Navy, hospital corpsman at the South Pole Station in 1974.Template:Sfn

Campbell Valley

Template:Coord. An ice-filled valley, or pass, extending east–west between the main group of peaks of the Crary Mountains and Boyd Ridge. Named by US-ACAN for Wallace H. Campbell, ionospheric physicist at McMurdo Station in the 1964–65 season; Macquarie Island, 1961–62.Template:Sfn

Boyd Ridge

Template:Coord. An ice-covered ridge, Template:Convert long, which extends in an east–west direction and forms the south end of the Crary Mountains. It is separated from the main peaks of the group by Campbell Valley. Named by US-ACAN for John C. Boyd, USARP biologist at McMurdo Station, 1965–66 and 1966–67 seasons.Template:Sfn

Runyon Rock

Template:Coord. A prominent rock along the northern side of Boyd Ridge. Named by US-ACAN for William E. Runyon, United States Navy, construction electrician at the South Pole Station in 1969 and 1974.Template:Sfn

References

Sources

• Template:Citation Template:Include-USGov
• Template:Cite book
• Template:Cite book
• Template:Cite conference
• Template:Citation
• Template:Cite journal
• Template:Cite journal
• Template:Citation
• Template:Cite journal
• Template:Cite journal
• Template:Cite journal
• Template:Cite journal
• Template:Cite journal
• Template:Cite journal
• Template:Cite journal

• Template:Include-USGov

External links

• Template:Gnis