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Geologic Unit: Koko
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Map showing publication footprint
  • Usage in publication:
    • Koko volcanics*
  • Modifications:
    • Named
  • Dominant lithology:
    • Volcanics
  • AAPG geologic province:
    • Oahu
Publication:

Stearns, H.T., 1935, Geography and geology, [Island of Oahu, Hawaii], Part 1, IN Stearns, H.T., and Vaksvik, K.N., Geology and ground-water resources of the Island of Oahu, Hawaii: Hawaii Division of Hydrography Bulletin, no. 1, p. 3-198.


Summary:

Named for occurrence at Koko Head and Koko Crater cones and associated lava flows [Koko Head 7.5' quad] Island of Oahu. Lava flows include those of Hanauma Bay and Kahauloa Craters. Included as unit in upper part of Honolulu volcanic series. Composed of well-bedded gray to brown tuff, partly palagonitized forming a row of cones and firefountain spatter and lava flows. Overlies soil-covered emerged reef of Waimanalo stand of sea; also overlies with erosional unconformity Koolau volcanic series. Assigned latest Pleistocene or Recent age based on stratigraphic relations.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Koko volcanics*
  • Modifications:
    • Overview
  • AAPG geologic province:
    • Oahu
Publication:

Macdonald, G.A., and Davis, D.A., 1956, Zone des Hawaii, Chapter 2, IN Avias, Jacques, and others, Oceanie proprement dite; Fasc. 2 of V. 6, Oceanie: Lexique Stratigraphique International, p. 70-143(?)., Prepared by the Centre National de la Recherche Scientifique (Paris), International Geological Congress, Commission on Stratigraphy


Summary:

Includes Koko Crater tuff, Koko Head tuff, Hanauma Bay tuff and Kaohikaipu lava [from Koko rift], none of which are regarded as formal names (Winchell, 1947 p.16,21). Covers area of about 3 sq mi extending NE from Koko Head 2 to 5 mi SW of Makapuu Head. No fossils. Age assignment of latest Pleistocene or Recent based on relationship to reef of Waimanalo stand of sea.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Koko volcanics*
  • Modifications:
    • Age modified
  • AAPG geologic province:
    • Oahu
Publication:

Hay, R.L., and Iljima, A., 1968, Nature and origin of palagonite tuffs of the Honolulu Group on Oahu, Hawaii, IN Coats, R.R., Hay, R.L., and Anderson, C.A., eds., Studies in volcanology; a memoir in honor of Howel Williams: Geological Society of America Memoir, 116, p. 331-376.


Summary:

Tuffs of Koko Crater are subdivided into stratigraphic units: upper unit, as much as 75 ft thick, consisting of well-stratified, medium-to-coarse-grained tuffs containing accretionary lapilli (ash pisoliths) from 1 to 5 cm in diam., and lower unit of underlying beds forming bulk of cone consisting of crudely bedded to massive lapilli tuffs and coarse tuffs with scattered bombs and blocks. Authors believe "Koko Group" erupted previous to Waimanalo stand of sea based on prominent bench from 5 to 12 ft above sea level cut into tuffs on seaward side of Koko Group and well-developed 4-ft clayey soil locally present on surface of Koko volcanic rocks.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Koko Volcanics*
  • Modifications:
    • Geochronologic dating
  • AAPG geologic province:
    • Oahu
Publication:

Gramlich, J.W., Lewis, V.A., and Naughton, J.J., 1971, Potassium-argon dating of Holocene basalts of the Honolulu volcanic series, IN Note and Discussion: Geological Society of America Bulletin, v. 82, no. 5, p. 1399-1404.


Summary:

K-Ar ages on alkali olivine basalt from Koko lava of Honolulu Volcanic Series range from 43.4 +/-1.0 ka to 35.5 +/-2.2 ka.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Koko Volcanics*
  • Modifications:
    • Age modified
  • AAPG geologic province:
    • Oahu
Publication:

Stearns, H.T., 1974, Submerged shorelines and shelves in the Hawaiian Islands and a revision of some of the eustatic emerged shorelines: Geological Society of America Bulletin, v. 85, no. 5, p. 795-804.


Summary:

Koko Volcanics erupted during low stand of sea during either Kawela low or Mamala low of Wisconsinan, not during earlier low [referred to Hay and Iljima, 1968]

Source: GNU records (USGS DDS-6; Menlo GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Koko Volcanics†
  • Modifications:
    • Abandoned
  • AAPG geologic province:
    • Oahu
Publication:

Langenheim, V.A.M., and Clague, D.A., 1987, Stratigraphic framework of volcanic rocks of the Hawaiian Islands, Part II, IN The Hawaiian-Emperor volcanic chain, Chapter 1, OF Decker, R.W., Wright, T.L., and Stauffer, P.H., eds., Volcanism in Hawaii: U.S. Geological Survey Professional Paper, v. 1, 1350, p. 55-84. [http://ngmdb.usgs.gov/Prodesc/proddesc_42485.htm]


Summary:

Koko Volcanics (Stearns, IN Stearns and Vaksvik, 1935) abandoned as formally named unit. Rocks reallocated to Koko Crater tuff cone, Hanauma tuff cone, and Koko Head flow (and associated cone), informal units of Honolulu Volcanics.

Source: GNU records (USGS DDS-6; Menlo GNULEX).


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Asterisk (*) indicates published by U.S. Geological Survey authors.

"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).

Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).