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![Page 1: Available on World Wide W - USGSBase, intended for visual reference only, is fitted to GIS-based coastline by inspection Geology of Ko‘olau Range and many island-wide sedimentary](https://reader035.vdocuments.us/reader035/viewer/2022070723/5f01e21e7e708231d40180b4/html5/thumbnails/1.jpg)
QTkdc
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21˚30′
158˚17′30″
158˚17′30″ 158˚07′30″ 157˚52′30″ 157˚45′ 157˚37′30″21˚45′
21˚37′30″
21˚22′30″
21˚15′
21˚45′
21˚37′30″
21˚30′
21˚22′30″
21˚15′
158˚00′158˚15′
158˚07′30″ 157˚52′30″ 157˚45′ 157˚37′30″158˚00′158˚15′
Geologic linework in Universal Transverse Mercator projection, North American datum 1983, zone 4
Topographic base and bounding latitude-longitude ticks from U.S. Geological Survey, Honolulu County, year of publication unspecified. Universal Transverse Mercator projection, zone 4, International spheroid
Base, intended for visual reference only, is fitted to GIS-based coastline by inspection
Geology of Ko‘olau Range and many island-wide sedimentary units from Stearns (1939). Digital compilation by K.M. Brunt, D.R. Sherrod, and S.E. Watkins. Fitting to modern topographic base by D.R. Sherrod and S.E. Watkins, 2004Volcanic geology in Wai‘anae Range by J.M. Sinton, 1980-2004. Compiled into digital version by D.R. Sherrod, 2004
21˚30′
SCALE 1:100 000
PLANIMETRIC BASE; NO TOPOGRAPHIC DEPICTION
0 4 8 12 KILOMETERS
Geologic Map of the State of Hawai‘i, Sheet 3—Island of O‘ahuBy
David R. Sherrod, John M. Sinton, Sarah E. Watkins, and Kelly M. Brunt2007
MAPLOCATION
PRINCIPAL HAWAIIANISLANDS
U.S. DEPARTMENT OF THE INTERIORU.S. GEOLOGICAL SURVEY
OPEN-FILE REPORT 2007-1089SHEET 3 of 8
Pamphlet accompanies map
Available on World Wide Web at http://pubs.usgs.gov/of/2007/1089/
QTkl
Takl
Tapl
Tapl
QTao
QTkdc
QTkl
QTkl
Qbd
Qdo
Qot
Qov
QolQot
Qf
QTkkl
QTkkdc
QTkbr
Qdy
Qdo
QTkkdc
QTao
Qokt
QoktQokl
Qokl
Qokt
Qokl
QoksQoks
QobrQa
QotQdo
Qotl
QolQTkt
QTktQottQbd
Qf
Qcrs
Qf
Qf
Talev
Tolel
TalelTakl
Qcrs
QTao
TakbrTakl
Takiv
Takmk
Takil
Tapl
Talel
Talec
TalelTapv
Talev
Talel
QTaoQcrs
Qcrs
Qcrs
Qcrs
Qcrs
Qbd
Takbr
Takl
QTao
QTao
TalecTalel
Takil
Takbr
Talv
TallTall
Talev
Talev
Talel
Talel
Qbd
Qot
Qol
QovQf
Qot
Qcrs
QoklQoks
QTkl
Q Tkl
Qotl
Qf
Qcrs
Qoks
Qobr
QaQTao
QTao Qa
Qa
Qa
Qbd
QTkdc
QTkdc
QTkdc
QTkdc
QTkdcQaQbd
Qcrs
Qcrs
Qbd
QdoTakl
Qa
QTao
Tapl
Talev
QTao
QTao
QTkl
QTkl
Tapl
Takl
Qcrs
Takl
Qbd
QcrsTall
Takil
TakbrQa
Qot
QolQovQol
KolekolePass
LualualeiValley
MaunaKūwale
Nu
‘u anu
Pa l i
Takiv
Tall
Qdy
QaQbd
Qcrs
Qol
QTkl QTkt QTkdc QTki QTkkl QTkkdc
Qov Qobr Qot
QotlQokl Qokt Qoks
Talel Talev Talec
Tall Talv
Qa
Qf
Qbd Qdy Qld Qlg Qls Qtc
Qcrs Qcbc
QTao
Qt
Takl Takv TakbrTakmkTakil
Tapl Tapv Tai
Ni‘ihauvolcano
Kaua‘ivolcano
Ko‘olau volcano Wai‘anae volcano
East Moloka‘ivolcano
West Moloka‘ivolcano
NI‘IHAU KAUA‘I O‘AHU MOLOKA‘I
Wai
mea
Can
yon
Bas
alt
Pān
ī‘au
Bas
alt
Ki‘e
k‘ie
Bas
alt
Kōl
oa V
olca
nics
Ko‘
olau
Bas
alt
Wes
t Mol
oka‘
i Vol
cani
cs
Eas
t Mol
oka‘
iVo
lcan
ics
Kal
aupa
paVo
lcan
ics
Wai
‘ana
eVo
lcan
ics
Hon
olul
u Vo
lcan
ics
CORRELATION OF MAP UNITS
SURFICIAL DEPOSITS COMMON TO SEVERAL OF THE ISLANDS
VOLCANIC AND INTRUSIVE ROCKS AND SPARSE INTERBEDDED SEDIMENTARY BEDS
QTkkbr
Takiv
[Boxes without color show ages of correlative stratigraphicformations on adjacent islands not depicted on this map]
SURFICIAL DEPOSITS COMMON TO SEVERAL OF THE ISLANDS
Qf Fill (Holocene)
Qa Alluvium (Holocene)
Qbd Beach deposits (Holocene)
Qdy Younger dune deposits (Holocene)
Qdo Older dune deposits (Holocene and Pleistocene)
Qcrs Calcareous reef rock and marine sediment (Pleistocene)
QTao Older alluvium (Pleistocene and Pliocene)
Conformable and interbedded to disconformable
VOLCANIC AND INTRUSIVE ROCKS ON THE ISLAND OF O‘AHU
Honolulu Volcanics (Pleistocene)—Divided into:
Deposits from Koko fissure system—Consists of:
Qokl Lava flows
Qokt Tuff
Qoks Spatter
Deposits from Tantalus Peak and Sugar Loaf vents—Consists of:
Qotl Lava Flows
Qott Tuff
Qol Lava flows
Qov Cinder vent deposits
Qobr Breccia
Qot Tuff cone deposits
Disconformity
Ko‘olau Basalt (Pleistocene(?) and Pliocene)—Divided into:
QTkl Lava flows
QTkt Vitric and lithic tuff
QTkdc Dike complex
QTki Intrusive rocks
Kailua Member—Divided into:
QTkkl Lava flows
QTkkdc Dike complex within Kailua Member
QTkkbr Breccia deposits
Conformable, possibly interbedded
Wai‘anae Volcanics (Pliocene)—Divided into:
Kolekole Member—Divided into:
Talel Lava flows
Talev Vent deposits
Talec Debris flows
Pālehua Member—Divided into:
Tapl Lava flows
Tapv Vent deposits
Kamaile‘unu Member—Divided into:
Takl Lava flows
Takv Vent deposits
Takbr Breccia
Takmk Mauna Kūwale Rhyodacite Flow
Takil Icelandite lava flows
Takiv Icelandite vent deposits
Lualualei Member—Divided into:
Tall Lava flows
Talv Vent deposits
Tai Intrusive rocks
Contact—Approximately located
Fault—Dashed where approximately located; dotted where concealed; queried where extent uncertain
Dike—Showing trend of intrusions in units Tai and QTki. Depiction partly schematic owing to exposure mostly in cliffs
LIST OF MAP UNITS ON SHEET 3 (THIS MAP)See explanatory pamphlet for complete descriptions
Qott
Qdo
2
5.33
0.78
Pliocene
Miocene
TERTIARY
2.58
0.78
0.9881.0721.1731.185
1.7781.9452.1282.148
3.0323.1163.2073.330
4.1874.300
4.4934.631
4.7994.8964.9975.235
Normal polarity (shaded) and reversed polarity (white) shown for subchrons through end of Gilbert time
(nonlinear scale)
Matuyama Reversed-Polarity Chron
Gilbert Reversed-Polarity Chron
Gauss Normal-Polarity Chron
Brunhes Normal-Polarity Chron
Holocene
Pleistocene
QUATERNARY
0.011
0
0.150
3.60
6.03
Approximate age, in millions of years*
PolarityChrons
*Time scale from Gradstein and others (2006)
1.81