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National Geologic Map Database
Geologic Unit: Kailua
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Map showing publication footprint
  • Usage in publication:
    • Kailua volcanic series*
  • Modifications:
    • Named
  • Dominant lithology:
    • Basalt
  • 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 village of Kailua [Mokapu 7.5' quad] Island of Oahu. Forms low hills surrounding Kailua between Kaneohe and Waimanalo. Composed of amygdaloidal basalt and its feeding dike complex which is best exposed on Mokulua Islands off Lanikai. Flows of pahoehoe and aa are as much as 60 ft thick. In general flows have total thickness of 600 ft and are slightly folded near Lanikai. Underlies Koolau volcanic series. Is deeply weathered and except along coast is almost completely covered with Lantana and soil, both of which make its relation to Koolau series obscure.

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


Map showing publication footprint
  • Usage in publication:
    • Kailua volcanic series*
  • Modifications:
    • Mapped
  • AAPG geologic province:
    • Oahu
Publication:

Stearns, H.T., 1939, Geologic map and guide of the Island of Oahu, Hawaii: Hawaii Division of Hydrography Bulletin, no. 2, 75 p., (incl. geologic map, scale 1:62,500)


Summary:

Map shows Tertiary and early Pleistocene(?) age. "It is believed that the Kailua volcanic series was formed in and under the caldera of the Koolau Volcano."

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


Map showing publication footprint
  • Usage in publication:
    • Kailua volcanic series*
  • Modifications:
    • Not used
  • AAPG geologic province:
    • Oahu
Publication:

Stearns, H.T., 1940, Supplement to the geology and ground-water resources of the Island of Oahu, Hawaii: Hawaii Division of Hydrography Bulletin, no. 5, 164 p.


Summary:

Unit referred to as "Kailua amygdaloidal basalt" or "Kailua lava". Kailua dike complex may have been laid down within Koolau caldera. "It is now proposed to group these rocks with the Koolau throat breccia and call them all a caldera complex."

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


Map showing publication footprint
  • Usage in publication:
    • Kailua volcanic series*
  • Modifications:
    • Age modified
  • AAPG geologic province:
    • Oahu
Publication:

Stearns, H.T., 1946, Geology of the Hawaiian Islands: Hawaii Division of Hydrography Bulletin, no. 8, 106 p.


Summary:

These lavas and their feeding dikes are exposed only near Kailua where the beds are 600 ft thick. Stratigraphic chart (p.27) shows Pliocene age, but correlation chart (p.23) shows Pliocene and older age.

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


Map showing publication footprint
  • Usage in publication:
    • Kailua volcanic series*
  • Modifications:
    • Age modified
  • AAPG geologic province:
    • Oahu
Publication:

Macdonald, G.A., 1949, Hawaiian petrographic province: Geological Society of America Bulletin, v. 60, no. 10, p. 1541-1596.


Summary:

Geologic figure map indicates Pliocene(?) age. [no basis given]

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


Map showing publication footprint
  • Usage in publication:
    • Kailua volcanic series*
  • Modifications:
    • Revised
  • 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:

Total exposed thickness is about 1600 ft but rocks extend below sea level. Included in Koolau volcanic series. Probably separated from adjacent extra-caldera Koolau lavas by faults and buried fault scarps. Formerly regarded as older than Koolau lavas, now believed to be contemporaneous with or even younger than Koolau volcanic series in crest region of Koolau Range. Assigned Pliocene(?) age.

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


Map showing publication footprint
  • Usage in publication:
    • Kailua Volcanic Series*
  • Modifications:
    • Not used
  • AAPG geologic province:
    • Oahu
Publication:

Doell, R.R., and Dalrymple, G.B., 1973, Potassium-argon ages and paleomagnetism of the Waianae and Koolau volcanic series, Oahu, Hawaii: Geological Society of America Bulletin, v. 84, no. 4, p. 1217-1242.


Summary:

[Kailua Volcanic Series not mentioned in text but map shows Koolau Volcanic Series where Kailua Volcanic Series should be.]

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


Map showing publication footprint
  • Usage in publication:
    • Kailua Member*
  • Modifications:
    • Revised
  • 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:

Stearns (1940) recognized that Kailua was part of Koolau Volcano. Kailua Volcanic Series (Stearns, IN Stearns and Vaksvik, 1935) reduced in rank and renamed Kailua Member of Koolau Basalt. No type locality specified. Principal reference locality: Kaiwa Ridge [21 deg 23'08"N, 157 deg 43'22"W] [Kaiwa Ridge not on topo quad but on map in Stearns (1939)] Reference locality: east side of Puu Papaa. Is probably Pleistocene(?) age.

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


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