Located at 148°15' West and 15°50' South, in the northwesternmost part of the Tuamotu archipelago (Central Pacific), Makatea island is isolated from its nearest
neighbouring atolls, Rangiroa and Tikehau by about 80 km, and it is 245 km from its closest volcanic neighbour, Tahiti. This island rises at least 3,500 m above the sea floor.
Like all Tuamotu islands, Makatea consists of biogenic deposits. But unlike the other islands which rise no more than a few metres above sea level and surround lagoons, Makatea reaches more than 100 m in elevation. Based on foraminiferal assemblages, age determination clearly indicated that the island frame was built up during Early Miocene (Montaggioni et al. 1985 a; Montaggioni, 1985).
Available online
Call Number: [EL]
Physical Description: 38 p.
Field | Value |
---|---|
Publisher | The Smithsonian Institution |
Modified | 15 February 2022 |
Release Date | 19 August 2021 |
Source URL | https://library.sprep.org/content/seward-margin-makatea-uplifted-carbonate-isla… |
Identifier | VL-34678 |
Spatial / Geographical Coverage Location | SPREP LIBRARY |
Relevant Countries | Pacific Region |
License |
Public
|
Author | Montaggioni, L.F. |
Contact Name | SPREP Records and Archives Officer |
Contact Email | [email protected] |