SCAR Gazetteer Information: Each place can have one or more entries in the SCAR Composite Gazetteer, dependant on its origin. By viewing an individual entry, you may see multiple references to the same place. SCAR uses a more general feature type coding, so each place will, in general, have multiple feature types.

Showing all 3 place names.

Name Latitude Longitude Feature Type
Haven Mountain (AUS) 80° 01' 59.9" S 155° 10' 00.1" E Mountain
Name ID: 1398 Place ID: 6112

A prominent feature, 2,560 m high, with a level razorback snow ridge at its highest part. The ridge is semi-circular in plan with a sheer, bare rock face about 500 m high on the inside and a steep snow slope on the outer (southern) face of the semi-circle. The area enclosed by the semi-circular ridge consists of rock debris and is largely snow-free. Named by the Darwin Glacier Party of TAE (1956-58) who sheltered there for five days.

Haven Mountain (NZL) 80° 02' 08.4" S 155° 09' 10.6" E Buttress
Name ID: 139377 Place ID: 6112

A prominent feature with a level razorback snow ridge, rising to c.2420m at its highest part where it branches from the southwest of Venta Plateau. The ridge is semi-circular in plan with a sheer, bare rock face about 500m high on the inside and a steep snow slope on the outer (southern) face of the semi-circle. The area enclosed by the semi-circular ridge consists of rock debris and is largely snow-free. Feature depicted on: NZ AntTopo50-MN03

Haven Mountain (USA) 80° 02' 00.0" S 155° 12' 00.0" E Mountain
Name ID: 126296 Place ID: 6112

A prominent mountain, 2,470 m, with a level razor-back snow ridge at its highest (eastern) part, standing 2 mi NE of Three Nunataks in the NW part of Britannia Range. So named by the Darwin Glacier Party of the CTAE (1956-58), who sheltered for five days in the largely snow-free area below the N side of the summit ridge.

Showing all 3 place names.

The SCAR Composite Gazetteer is hosted by the Australian Antarctic Data Centre. The information in the footer below pertains to the AADC web site.