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Lava trees and tree moulds as indicators of lava flow direction

Published online by Cambridge University Press:  01 May 2009

J. P. Lockwood  and
I. S. Williams
J. P. Lockwood
Affiliation:
U.S. Geological Survey, Hawaiian Volcano Observatory, Hawaii 96718
I. S. Williams
Affiliation:
Research School of Earth Sciences, Australian National University, Canberra, A. C. T.
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Summary

Lava trees and tree moulds are common in many areas where fluid basaltic lava has moved rapidly over forested terrain. Lava trees are formed only by thin flows, but tree moulds are preserved in both thin and thick flows. Both structures may indicate the direction of flow of the lava in which they are preserved. The usefulness of lava trees in this regard is limited to recent flows; tree moulds, however, have been described in rocks as old as middle Tertiary. Features commonly well preserved on the inner walls of moulds indicate the local flow direction. When found in sufficient number, tree moulds provide information on the palaeoslope and vent location.

Type
Articles
Information
Geological Magazine , Volume 115 , Issue 1 , January 1978 , pp. 69 - 74
Copyright
Copyright © Cambridge University Press 1978

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References

Bailey, E. B. & Anderson, E. M. 1925. The geology of Staffa, Iona, and western Mull (a description of Sheet 43 of the geologic map). Mem. Scotland geol. Survey.Google Scholar
Bartrum, J. A. 1925. An interesting lava-mold of a carbonized tree-trunk from Hokianga, North Auckland, New Zealand. Bull. U.S. geol. Surv. Hawaiian Volcano Observatory 8, no. 7, 55–6.Google Scholar
Brigham, W. T. 1868. Notes on the volcanic phenomena of the Hawaiian Islands, with a description of modern eruptions. Mem. Boston Soc. Nat. Hist. 1, pt. 3, 341–472.Google Scholar
Bullard, F. M. 1971. Volcanic history of the Great Rift, Craters of the Moon National Monument, south-central Idaho. Geol. Soc. America Abs. with Prog., South Central Sec., Lubbock, Tex., 3, no. 3, 234.Google Scholar
Finch, R. H. 1931. Lava tree casts and tree molds. The Volcano Letter (Hawaiian Volcano Observatory), no. 316.Google Scholar
Fiske, R. S. & Koyanagi, R. Y. 1968. The December 1964 eruption of Kilauea Volcano, Hawaii. Prof. Pap. U.S. geol. Surv. 607.Google Scholar
Fryxell, Roald. 1963. Notes on the occurrence of silicified wood from the Ginko flow of the Yakima Basalt Formation, Washington. Sigma Xi Trans. 1 32–6.Google Scholar
Greeley, R. & Hyde, J.H. 1972. Lava tubes of the Cave basalt, Mount Saint Helens, Washington. Bull.geol. Soc. Am. 83, no. 8, 2397–418.CrossRefGoogle Scholar
Jackson, D. B., Swanson, D. A., Koyanagi, R. Y. & Wright, T. L. 1975. The August and October 1968 east rift eruptions of Kilauea Volcano, Hawaii. Prof. Pap. U.S. geol. Surv. 890.Google Scholar
Jaggar, T. A. 1930. The island volcano Niuafoou. The Volcano Letter (Hawaiian Volcano Observatory no. 312).Google Scholar
Jaggar, T. A. 1945. Volcanoes Declare War. Honolulu; Paradise of the Pacific, Ltd.Google Scholar
Kanehira, Keiichiro, & Shimazaki, Yoshihiko., 1971. Native iron in basalt surrounding tree-molds at Mt Fuji, Japan. Neues Jb. Miner. Monatsh. 3, 124–30.Google Scholar
Lyman, C. S. 1849. Observations on the ‘Old Crater’ adjoining Kilauea (Hawaii), on the east. Am. J. Sci. ser. 2, 7, no. 20, p. 287 (from a letter dated 30 Jan. 1848).Google Scholar
Macdonald, G. A. & Abbott, A. T. 1970. Volcanoes in the Sea– The Geology of Hawaii. Honolulu: Univ. of Hawaii Press..CrossRefGoogle Scholar
Moore, J. G. & Richter, D. H. 1962. Lava tree molds of the September, 1961 eruption, Kilauea Volcano, Hawaii. Bull. geol. Soc. Am. 73, 1153–8.CrossRefGoogle Scholar
Nicols, R. L. 1940. Velocity of basaltic flows indicated by lava-trees. Trans. Am. Geophys. Union 21, 357.Google Scholar
Perret, F. A. 1913. Some Kilauean formations. Am. J. Sci., 4th ser., 36, no. 212, 151–9.CrossRefGoogle Scholar
Reclus, E. 1872. The Earth (trans. Woodword, R. B.). New York: Harper.Google Scholar
Searle, E. J. 1958. A note on the formation of native iron and other effects associated with contact of basalt and carbonized wood at Auckland, New Zealand. New Zealand J. Geol. Geophys. 1, no. 3, 451–8.CrossRefGoogle Scholar
Shrock, R. R. 1948. Sequence in Layered Rocks, 1st ed. New York: McGraw-Hill.Google Scholar
Stearns, H. T. 1928. Craters of the Moon National Monument, Idaho. Bull. Idaho Bur. Mines Geol.. 13, 120–6.Google Scholar
Swanson, D. A.. & Wright, T. L. 1976. Guide to field trip between Pasco and Pullman, Washington, emphasizing stratigraphy, vent areas, and intra-canyon flows of Yakima Basalt. Geol. Soc. America Cordilleran Sec. Mtg., Pullman, April 1976, Guidebook, no. 1, 33pp.Google Scholar
Tilling, R. I., Koyanagi, R. Y., Lipman, P. W., Lockwood, J. P., Moore, J. G. & Swanson, D. A.. 1976. Earthquake and related catastrophic events, Island of Hawaii, November 29, 1975 – A preliminary report. U.S. geol. Surv. Circular no. 740.Google Scholar
Tsuya, Hiromichi. 1971. Fuji-san – Results of Cooperative Scientific Survey of Mt Fuji– Topography and Geology of Volcano Mt Fuji. Tokyo: Fuji Kyuko Co.Google Scholar
Waters, A. C. 1960. Determining direction of flow in basalts. Am. J. Sci. 258-A, 350–66.Google Scholar
Yagi, T. 1933. Tree-like mould of lava at the northern foot of Mt Asama.J. Geogr. (Tokyo) 45, no. 536, 478–83. (In Japanese.)Google Scholar