Pensacola Mountains

Discovery and naming

The Pensacola Mountains were discovered and photographed on 13 January 1956 in the course of a transcontinental nonstop plane flight by personnel of United States Navy Operation Deep Freeze I from McMurdo Sound to Weddell Sea and return. They were named by the United States Advisory Committee on Antarctic Names (US-ACAN) for the U.S. Naval Air Station, Pensacola, Florida, in commemoration of the historic role of that establishment in training aviators of the United States Navy. The mountains were mapped in detail by United States Geological Survey (USGS) from surveys and United States Navy air photos in 1956–67.

Geology

The Pensacola Mountains were originally continuous with the Ventana Mountains near Bahía Blanca in Argentina, Cape Fold Belt in South Africa, the Ellsworth Mountains (West Antarctica) and the Hunter-Bowen orogeny in eastern Australia.

The Ordovician-Devonian Neptune Group rests unconformably on a Cambrian succession, and is overlain disconformably by the Dover Sandstone of the Beacon Supergroup. Within the Neptune Group is the Brown Ridge Conglomerate, Elliott Sandstone, Elbow Formation, and the Heiser Sandstone.

Western features

The Foundation Ice Stream flows through the western part of the range. File:Pecora Escarpment USGS.jpg|Pecora Escarpment, South tip of Patuxent Range File:Thomas Hills USGS.jpg|Patuxent Range. Rambo Nunataks to north File:C83052s5 Schmidt Hills.jpg|North part of Neptune range

• Pecora Escarpment (), an irregular escarpment, 7 nmi long, standing 35 nmi southwest of Patuxent Range and marking the southernmost exposed rocks of the Pensacola Mountains.
• Patuxent Range (), a major range of the Pensacola Mountains. It comprises the Thomas Hills, Anderson Hills, Mackin Table and various nunataks and ridges bounded by the Foundation Ice Stream, Academy Glacier and the Patuxent Ice Stream.
• Rambo Nunataks (), a loose chain of nunataks which lie northwest of Patuxent Range and extend along the west side of the Foundation Ice Stream for 17 nmi.
• Neptune Range (), a mountain range, 70 nmi long, lying west-southwest of Forrestal Range in the central part of the Pensacola Mountains. The range comprises Washington Escarpment with its associated ridges, valleys and peaks, the Iroquois Plateau, the Schmidt Hills and Williams Hills.

Northern features

The northern part of the range is to the south of the Filchner–Ronne Ice Shelf. File:C82052s5 Ant.Map Cordiner Peaks.jpg|Cordiner Peaks, West part of Dufek Massif File:C82045s1 Ant.Map Davis Valley cropped.jpg|East part of Dufek Massif. North part of Forrestal Range File:Saratoga Table USGS.jpg|South part of Forrestal Range File:C82037s5 Ant.Map Argentina Range.jpg|Argentina Range

• Cordiner Peaks (), a group of peaks extending over an area of 6 nmi standing 8 nmi southwest of Dufek Massif in the northern part of the Pensacola Mountains.
• Dufek Massif (), a rugged, largely snow-covered massif 27 nmi long, standing west of the Forrestal Range in the northern part of the Pensacola Mountains.
• Forrestal Range (), a largely snow-covered mountain range, about 65 nmi long, standing east of Dufek Massif and the Neptune Range in the Pensacola Mountains.
• Argentina Range (), a range of rock peaks and bluffs, 42 nmi long, lying 35 nmi east of the northern part of Forrestal Range in the northeastern portion of the Pensacola Mountains.

References

Sources

• {{citation|url=https://pubs.usgs.gov/fedgov/70039167/report.pdf |accessdate=2023-12-03 |edition=2 |editor-last=Alberts |title=Geographic Names of the Antarctic |editor-first=Fred G.
• {{citation |title=Lower-mid-Palaeozoic sedimentation and tectonic patterns on the palaeo-Pacific margin of Antarctica, in Geological Evolution of Antarctica

References

1. "Pensacola Mountains".