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Kohala Volcano

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Journal Article
Published: 23 May 2018
Environmental & Engineering Geoscience (2018) 24 (2): 187–205.
...Kim M. Bishop Abstract The Hawaiian Island volcanic edifices have shed at least 15 giant submarine landslides, each classified as either a slump or debris avalanche. Controversy exists regarding the number, size, and type of landslides on the northeast flank of Kohala Volcano. This study provides...
FIGURES | View All (16)
Journal Article
Journal: Geology
Published: 01 July 2011
Geology (2011) 39 (7): 659–662.
... rift zone of Mauna Kea, but the new ages validate proposals that it is the distal east rift zone of Kohala, the oldest subaerial volcano on the island. These ages constrain the inception of tholeiitic volcanism at Kohala, provide the first measured duration of tholeiitic shield building (≥870 k.y...
FIGURES | View All (4)
Journal Article
Journal: Geology
Published: 01 September 2004
Geology (2004) 32 (9): 741–744.
... Lanai: Kohala has been subsiding for at least 470 k.y. ( Ludwig et al., 1991 ). On the northwest flank of Kohala, Stearns and Macdonald (1946) found marine fossiliferous conglomerates that they attributed to an ancient highstand. Highstand deposits are incompatible with a sinking volcano, so in May...
FIGURES
Journal Article
Journal: Geology
Published: 01 November 1981
Geology (1981) 9 (11): 531–533.
...Mark D. Feigenson; Frank J. Spera Abstract At Kohala volcano, Hawaii, the amount of source partial melting decreases rapidly toward the end of magmatic activity. The decreasing amounts of partial fusion lead to progressively higher concentrations of incompatible trace elements in lavas erupted...
Journal Article
Journal: GSA Bulletin
Published: 01 October 1973
GSA Bulletin (1973) 84 (10): 3483–3484.
Journal Article
Journal: GSA Bulletin
Published: 01 October 1973
GSA Bulletin (1973) 84 (10): 3485–3487.
Journal Article
Journal: GSA Bulletin
Published: 01 December 1972
GSA Bulletin (1972) 83 (12): 3731–3738.
...IAN McDOUGALL; D. A SWANSON Abstract Kohala is regarded as the oldest major shield volcano on the island of Hawaii. Potassium-argon ages of nine lava flows from the predominantly tholeiitic Pololu Volcanic Series of Kohala Volcano range from about 0.33 m.y. o t about 0.45 m.y. These results suggest...
Journal Article
Journal: GSA Bulletin
Published: 01 July 1971
GSA Bulletin (1971) 82 (7): 1997–2000.
...G. BRENT DALRYMPLE Abstract Potassium-argon ages on five lava flows from the Pololu Volcanic Series, thought to be among the oldest rocks exposed on the island of Hawaii, indicate that the main subaerial shield-building phase of Kohala Volcano occurred about 0.7 ± 0.15 m.y. ago and that most...
Journal Article
Journal: GSA Bulletin
Published: 01 December 1969
GSA Bulletin (1969) 80 (12): 2597–2600.
...IAN McDOUGALL Abstract Kohala Mountain is regarded as the oldest volcano on the island of Hawaii. Potassium-argon ages on three lavas of the Hawi Volcanic Series, the youngest sequence of lavas on Kohala, range from 0.14 to 0.20m.y. and indicate that volcanism ceased in the very late Pleistocene...
Image
Image of <span class="search-highlight">Kohala</span> <span class="search-highlight">Volcano</span> with view toward the southwest (from Google Earth, ...
Published: 23 May 2018
Figure 2. Image of Kohala Volcano with view toward the southwest (from Google Earth, 2017).
Image
Geologic map of <span class="search-highlight">Kohala</span> <span class="search-highlight">volcano</span> re-drawn from  Sherrod et al. (2007)  and  W...
Published: 23 May 2018
Figure 4. Geologic map of Kohala volcano re-drawn from Sherrod et al. (2007) and Wolfe and Morris (1996) .
Image
Figure 3. Shaded relief map of <span class="search-highlight">Kohala</span> <span class="search-highlight">Volcano</span> with volcanic units outlined ...
Published: 01 July 2007
Figure 3. Shaded relief map of Kohala Volcano with volcanic units outlined following Wolfe et al. (1996) . Note that the Pololū volcanic series is not patterned. Coastal profile A–A′ is shown in Figure 4 . Contour map of average annual precipitation (1961–1990) is shown, with a contour interval
Image
Figure 5. Topographic profile from <span class="search-highlight">Kohala</span> <span class="search-highlight">Volcano</span> over the Pololū Slump. P...
Published: 01 July 2007
Figure 5. Topographic profile from Kohala Volcano over the Pololū Slump. Profile location is shown in Figure 2 . All dashed lines are untested interpretations of the topography before and immediately after the Pololū Slump. Note that sea level at the time of the slump was probably ∼1000 m lower
Journal Article
Journal: Geology
Published: 01 June 2000
Geology (2000) 28 (6): 547–550.
... and similar to those of Kohala volcano. This terrace evidently is a product of Kohala instead of Mauna Kea. Almost all of Hilo Ridge below the terrace therefore must predate the principal growth of Mauna Kea, which has superficially isolated the ridge from its Kohala source by overlapping its proximal segment...
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Image
Cross section showing the area of depletion existing at the summit of Kohal...
Published: 23 May 2018
Figure 9. Cross section showing the area of depletion existing at the summit of Kohala Volcano.
Image
A. Photomicrograph of an apatite microphenocryst in a hawaiite from <span class="search-highlight">Kohala</span> ...
Published: 01 December 2000
F ig . 6. A. Photomicrograph of an apatite microphenocryst in a hawaiite from Kohala volcano, Hawai’i. B. Olivine phenocryst in glassy picrite (oceanite) from Kîlauea volcano, Hawai’i. C. Glass inclusion from olivine phenocryst in Figure 6B. Spinel (black) and augite (?) inclusions in the glass.
Journal Article
Published: 01 April 2006
Journal of Micropalaeontology (2006) 25 (1): 55–56.
..., on the flanks of the extinct Kohala volcano ( Fig. 1 ). This unit is found between modern altitudes of c . 1.5–61 m above sea-level. The deposit is sandwiched between a fossil soil below and a modern soil above in Keawe'ula Bay ( Fig. 2 ). Dating of coral fragments from within the deposit indicate an age...
FIGURES | View All (4)
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Bathymetric map showing locations of long submarine rift zones. Historical ...
Published: 01 July 2011
Figure 1. Bathymetric map showing locations of long submarine rift zones. Historical eruptions in red. Dashed line is inferred buried east rift of Kohala. Volcanoes: EM—East Molokai'i; HA—Haleakala; HU—Hualalai; K—Kaho'olawe; KL—Kilauea; KO—Kohala; L—Lanai; LO—Lo'ihi; M—Mahukona; MI—West Maui; MK
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Maps that depict previous landslide proposals for the northeast flank of Ko...
Published: 23 May 2018
Figure 3. Maps that depict previous landslide proposals for the northeast flank of Kohala Volcano. (A) Pololu debris avalanche. ( Moore et al., 1989 ). (B) Pololu slump ( Smith et al., 2002 ) with cross section. (C) Un-named debris avalanche ( Smith et al., 2002 ) with cross section. Dashed line
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Figure 1. 10 m shaded relief and topographic contour map of northeast side ...
Published: 01 July 2007
Figure 1. 10 m shaded relief and topographic contour map of northeast side of Kohala Volcano. Contour interval is 100 m. The 1500 m contour is labeled. Present-day sea level is at 0 m. The four large Kohala amphitheater-headed valleys are named on the figure. Longitudinal profiles for valleys