Geological Field Guide to the Hawaiian Islands: Hilo to by David A. Clague, Richard W. Hazlett

By David A. Clague, Richard W. Hazlett

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Published by way of the yank Geophysical Union as a part of the Field journey Guidebooks Series.

The Hawaiian Islands shape the youngest a part of a series of volcanoes that stretches approximately 6000 km around the north Pacific Ocean (Fig. 1). This targeted geological function contains at the least 107 person volcanoes having a mixed quantity more than 1 million km3 (Bargar and Jackson, 1974). The chain is age innovative with still-active volcanoes on the southeast finish while these on the northwest finish have a while of approximately 75-80 Ma. The volcanoes of the chain have been erupted onto the seafloor with no regard for the age or constitution of the underlying ocean crust. The Hawaiian volcanic ridge is surrounded by way of a symmetrical melancholy, the Hawaiian Deep, up to 0.7 km deeper than the adjoining seafloor. The Hawaiian Deep is in flip surrounded by means of the vast Hawaiian Arch. Clague and Dalrymple (1987) evaluate the environment and age family of the volcanoes that include the chain.

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Additional info for Geological Field Guide to the Hawaiian Islands: Hilo to Honolulu, Hawaii, July 1-7, 1989, July 21-27, 1989

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1983, Origin of Hawaiian EPILOGUE tholeiites and alkalic basalt: Nature, v. 302, p. 785789. This ends the fieldtrip through the Hawaiian Islands. , 1985, Trace element and with submarine preshield to shield stage eruptions isotope geochemistry of lavas from Haleakala occurring frequently at Loihi Seamount, shield stage Volcano, East Maui: Implications for the origin of eruptions occurring frequently on Mauna Loa and Hawaiian basalts: Journal of Geophysical Research, Kilauea, postshield stage eruptions likely within the next v.

This flow is overlain by dune bedded Journal ofResearch, v. 2, p. 545-550. , 1976, Petrology, mineralogy and surges; most are separated by thin airfalilayers. S. Geological Survey Professional Paper surge deposits. Walker (1987b) has described this and 961,53 p. other locations in the Salt Lake Crater cluster. , 1970, Origin of and enter Salt Lake crater on Salt Lake Boulevard. garnet pyroxenite xenoliths at Salt Lake Crater, Oahu: Stop 2s. Turn right on Ala Napunani. 5 Mineralogical Society ofAmerica Special Paper 3, p.

Hawaiian Planetology Conference: NASA Special Publication TMX62632, p. 233-238. , 1982, Focal Hawaii: Memoir Geological Society of America, v. Mechanisms and locations of earthquakes in the 44, p. 219-230. , 1987, Geological Field Guide, Kilauea zone 1970-1979: Implications for tectonics of the Volcano: Hawaii Natural History Association, 117 p. , and Wright, Tectonics, v. 1, p. 495-542. , 1986, Volcano monitoring at the U. S. , 1843, History of the Sandwich Islands: Geological Survey's Hawaiian Volcano Observatory: Lahainaluna, Hawaii, 65 p.

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