This information has been developed from one or more of these publications:
|
Location: | Rhyll - 575465. 1 km east of Long Point. | Elizabeth Island is surrounded by low bluffs and shore platforms |
Access: | By boat only. Recommended access is at high tide onto the rocky beach at the southern end of the Island. | |
Ownership: | Private land and Crown land. | |
Geology/Geomorphology: | Elizabeth Island is geologically continuous with the main island as it is composed of Tertiary Older Volcanics with a small outcrop of Lower Cretaceous sediments at its northern tip. The island is separated from the main island by inter-tidal mudflats and a tidal channel. The shoreline of the island is a narrow, rock-strewn low tide shore platform cut in basalts and Mesozoic sediments, in front of a low vegetated bluff. A small pocket of mangroves and salt marsh occurs in a sheltered site on the eastern coast of the island. | |
Significance: | Regional. The volcanics of Elizabeth Island may represent a later stage of the Tertiary volcanic sequence as the petrology of the basalt appears different from that found on French Island. Preservation of the restricted outcrops of this possibly later volcanic suite is recommended for future research investigations. | |
Management: | Class 2. To preserve the extent of outcrop on the island it is recommended that no quarrying of basalt be permitted. |
Elizabeth Island. Low vegetated bluff with salt marsh terrace overlying a former shore platform. Mangroves occupy the seaward edge, Site 215. |