Document ID: chunk:federal_register_of_legislation:F2016C01080:clause:1_4
Version: federal_register_of_legislation:F2016C01080
Segment Type: clause
Provision Reference: sch 1 cl 4
Character Range: 74360–76019

4                                                         62°57′51″S  60°44′10″W

Site F—Telefon Bay
The site incorporates several features created during the 1967 eruption in Telefon Bay, i.e. Pisagua Hill on the southern side of the site, the small shallow Ajmonecat Lake on the ash plain north of Stancomb Cove and the low flat ash plain extending from the shoreline of Telefon Bay to the steep slopes and lava outcrops approximately 0.5 km inland. Pisagua Hill was created as a new island in 1967, but is, as of 2014, joined to the main island by the aforementioned ash plain. At the northern end of the plain is Extremadura Cove, which was a lake until the narrow isthmus (approximately 2 m wide and 50 m long) separating it from Port Foster was breached in approximately 2006. Extremadura Cove is excluded from the site.
The northern shoreline of the lagoon (Stancomb Cove) at the southwest of Telefon Bay marks the southern boundary of the site, and the south‑western shore of the Extremadura Cove to the north of Telefon Bay marks the north‑eastern boundary of the site. The south‑eastern boundary extends along the shore south of Pisagua Hill, north to the shoreline of the Extremadura Cove at the northern end of Telefon Bay. The north‑western boundary is roughly delineated by the 10 m contour of Telefon Ridge that links Stancomb Cove to Extremadura Cove. Ajmonecat Lake (62°55′23″S, 60°40′45″W), including its shoreline, is included in the site. The shoreline of Telefon Bay is excluded from the site to allow access past the site.

Boundary coordinates for Site F—Telefon Bay
Item                                         Latitude    Longitude