The size of the region is about 375 km east-west and 200 km north-south, with an estimated area of 57 000 km². It is only a bit more than 700 km south of the North Pole. The area is mountainous, with elevations to 1 950 m in the heavily glaciated Roosevelt Range and to comparable heights in the little-explored H.H. Benedict Range. It is free of Greenland's inland ice cap. Being mostly north of the 82°N parallel, it contains the most northerly ice-free region of the world, mostly in Southern Peary Land (such as Melville Land just north of the Independence Fjord. Precipitation levels are so low (only about 25 to 200 mm per year, all as snow) that it is called a polar desert. It was not covered by glaciers during the most recent ice age. However, in its western part, there is a local icecap, Hans Tausen Icecap, with ice at least 344 m thick.
Caribou and musk oxen are supported by the sparse vegetation, which covers only about 5% of the surface, and which includes 33 species of flowering plants. Other fauna includes arctic fox, polar wolf, polar bear, and arctic hare.
The area is named after Robert E. Peary, who first explored it during his expedition of 1891 to 1892.
There are two Arctic research stations on Jørgen Brønlund Fjord, Brønlundhus (erected in 1948) and Kap Harald Moltke (erected in 1972). Both stations were built on initiative of Eigil Knuth, and have been the basis for many scientific expeditions. Kap Harald Moltke station was built later in connection with use of the natural runway east of Jørgen Brønlund Fjord mouth. . The stations located 10 km from each other on either side of the fjord, with Brønlundhus on the western side, and communication between them in summer is by boat, depending on ice conditions. Since the death of Eigil Knuth, the stations are administered by Peary Land Foundation. Today, Brønlundhus can be characterised as a museum, with a collection of artefacts from polar explorations.
Late Cretaceous-Palaeocene Continental Rifting in the High Arctic: U-Pb Geochronology of the Kap Washington Group Volcanic Sequence, North Greenland
Sep 01, 2011; Abstract: The Kap Washington Group volcanic sequence is exposed on the north coast of Greenland. The sequence was erupted in a...
New fossil worms from the Lower Cambrian of the Kinzers Formation, Pennsylvania, with some comments on Burgess shale-type preservation
May 01, 1999; ABSTRACT-Two new fossil worms are described from the Lower Cambrian Kinzers Formation of southeast Pennsylvania. Both are unique...