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20121209 1744UTC 7163kHz JX9JKA
Date : 09/Dec/2012 1744UTC
Freq : 7163kHz LSB
Rig : SDR(PI4THT)
ANT : GP
PC recording
Postage EU = 13 NKR, World = 15 NKR. 1 USD = 5,5 NKR. EUROPE AND REST OF THE WORLD: 3 GREEN STAMPS OR 1 IRC.
No eQSL please. SWL reports are welcome. QSL Direct only.
Svein Rabbevag, Brendlia 12, N-6013 ALESUND, NORWAY
Jan Mayen Island is a volcanic island in the Arctic Ocean and part of the Kingdom of Norway. It is 55 km (34 mi) long (southwest-northeast) and 373 km2 (144 sq mi) in area, partly covered by glaciers (an area of 114.2 km (71.0 mi) around the Beerenberg). It has two parts: larger northeast Nord-Jan and smaller Sør-Jan, linked by anisthmus 2.5 km (1.6 mi) wide. It lies 600 km (370 mi) northeast of Iceland, 500 km (310 mi) east of central Greenlandand 1,000 km (620 mi) west of the North Cape, Norway. The island is mountainous, the highest summit being theBeerenberg volcano in the north. The isthmus is the location of the two largest lakes of the island, Sørlaguna (South Lagoon), and Nordlaguna (North Lagoon). A third lake is called Ullerenglaguna (Ullereng Lagoon). Jan Mayen was formed by the Jan Mayen hotspot.
Geography and geology
Jan Mayen consists of two geographically distinct parts. Nord-Jan has a round shape and is dominated by the 2,277 m (7,470 ft) high Beerenberg volcano with its large ice cap (114.2 km2 or 44 sq mi), which can be divided into twenty individual outlet glaciers. The largest of those is Sørbreen, with an area of 15 km2 (5.8 sq mi) and a length of 8.7 km2(3.36 sq mi). South-Jan is narrow, comparatively flat and unglaciated. Its highest elevation is Rudolftoppen at 769 m (2,523 ft). The station and living quarters are located on South-Jan. The island lies at the northern end of the Jan Mayen Microcontinent. The microcontinent was originally part of the Greenland Plate, but now forms part of theEurasian Plate.
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