Lava Channels on Tristan da Cunha
- 1 August 1963
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 100 (4) , 345-351
- https://doi.org/10.1017/s0016756800056089
Abstract
Lava channels flanked by lava levees are described from Tristan da Cunha. These have been formed by the building up of the levees by overflow and solidification of fluid lava from the channels. A distinction is made between the terms “lava levee” and “lava moraine”.Keywords
This publication has 6 references indexed in Scilit:
- Royal Society Expedition to Tristan Da Cunha: Preliminary ReportNature, 1962
- Structures and forms of basaltic rocks in HawaiiPublished by US Geological Survey ,1953
- Grooved LavaThe Journal of Geology, 1938
- The Keaiwa or 1823 Lava Flow from Kilauea Volcano, HawaiiThe Journal of Geology, 1926
- The Geology of Ascension IslandProceedings of the American Academy of Arts and Sciences, 1925
- Preliminary report on the geology and water resources of central OregonPublished by US Geological Survey ,1905