Document ID: chunk:federal_register_of_legislation:F2016C01080:clause:1_2:p1
Version: federal_register_of_legislation:F2016C01080
Segment Type: clause
Provision Reference: sch 1 cl 2 (pt 1/3)
Character Range: 147557–150683

2  Description
  The Area comprises 3 high altitude geothermal sites, Tramway Ridge on the summit of Mount Erebus (7731′S, 16706′E), 3 locations of geothermal activity on the summit of Mount Melbourne (7421′S, 16442′E), and the summit of Mount Rittmann (7328′S, 16537′E).

Tramway Ridge, Mount Erebus
Tramway Ridge is a ridge that rises to approximately 3 450 m above sea level on the north‑western slope of the main crater of Mount Erebus. The site is located along this ridge approximately 1.5 km from the main crater.
The boundary of the site comprises a rectangle of 200 m by 200.8 m which encompasses most of the geothermally heated ground of lower Tramway Ridge. The boundary is as follows:
 (a) starting at the north‑western boundary corner at 7731′01.853″S, 16706′21.251″E (Point A), it extends south to the south‑western boundary corner at 7731′08.327″S, 16706′20.686″E (Point E);
 (b) then east to the south‑eastern boundary corner at 7731′08.448″S, 16706′50.521″E (Point D);
 (c) then north to the north‑eastern boundary corner at 7731′01.976″S, 16706′51.074″E (Point B);
 (d) then back to Point A.

Mount Melbourne
Mount Melbourne is a stratovolcano located in northern Victoria Land, between Wood Bay and Terra Nova Bay, on the western side of the Ross Sea, and approximately 10 km east of Campbell Glacier.
The site consists of 3 separate locations, 2 on the main summit crater and a third on the north‑western slope of the mountain. On the south‑eastern rim of the main summit crater of Mount Melbourne, there are 2 adjacent designated locations.
The first location (Cryptogam Ridge) is a distinct crescent shaped ridge and consists of areas of snow‑covered unheated ground, snow‑free geothermally‑heated ground and ice‑hummocks covering steam emissions that extends approximately 40 m in all directions from the ridge line.
The boundary (see Map A2) is as follows:
 (a) starting at the north‑western boundary corner at 74°21′20.389″S, 16441′31.652″E (Point 1A), it extends south approximately 50 m to the south‑western boundary corner at 7421′22.096″S, 16441′32.551″E (Point 1N);
 (b) then east following the crescent shape of Cryptogam Ridge to the following unmarked points:
 (i) 7421′21.383″S, 16441′38.254″E (Point 1M);
 (ii) 7421′20.840″S, 16441′45.230″E (Point 1L);
 (iii) 7421′21.220″S, 16441′49.934″E (Point 1K);
 (iv) 7421′21.815″S, 16441′54.574″E (Point 1J);
 (v) 7421′22.588″S, 16441′58.044″E (Point 1I);
 (c) then to the south‑eastern boundary corner at 7421′24.103″S, 16442′00.579″E (Point 1H);
 (d) then north to the north‑eastern boundary corner at 7421′23.355″S, 16442′07.010″E (Point 1G);
 (e) then west following the crescent shape of Cryptogam Ridge to the following unmarked points:
 (i) 7421′21.523″S, 16442′03.989″E (Point 1F);
 (ii) 7421′20.117″S, 16441′57.869″E (Point 1E);
 (iii) 7421′19.307″S, 16441′51.137″E (Point 1D);
 (iv) 7421′19.153″S, 16441′45.329″E (Point 1C);
 (v) 7421′19.650″S, 16441′37.695″E (Point 1B);
 (f) then back to Point 1A.
Both the northern and southern boundaries are located below the ice‑free ridge.
The second location