quadrangles, california x 60 geologic map of the … · klhs kl kwsr kwps kwst ktr klt khqd klmp...
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Qh
Qsh
Tcv6
QTsb
Tcv5
Tcv4
Tcv3
Tcv2
Tcv1
Tcv5a
Tw
Tdg
TKmg
Wils
on C
reek
Fau
lt
}ga
}<m }<l
<su
<sq
<scq
<sc
cgm ms
QUATERNARY
PLIOCENE
MIOCENE
OLIGOCENEAND EOCENE
CRETACEOUSOR JURASSIC
CRETACEOUS
JURASSIC
TRIASSIC
PALEOZOIC
PROTEROZOIC
AGE UNKNOWN
SAN GABRIEL MOUNTAINS ASSEMBLAGE SAN BERNARDINO MOUNTAINS ASSEMBLAGE
}c}ir }gu }gy
Tgbt
Tcc
Tpp2
QTpp3
Tpp1
QTpp
Tss
Qb
Rocks between SAN ANDREAS FAULT, and MILL CREEK and WILSON CREEK FAULTS
}og
mmc mms mq mxmm
KJos KJsp
Ds
_bk
_c
_wc
_z
K^mm
Kmg
Mm
}|m
gg
}dy}fg}mg
*bs
<m
|mb
Tcf
Td
Tv
gn
PALEOCENE
Tcu
}gr }ug }sl }mx
? ? ? ? ? ?
Tmm
Tms
Tma
TmcpTms
Tmm
Tmcv
Tb
Tgtp
<gn
<gn2 <gm <gc
<gn1
Tg
Tgb
Tgr
Tga
Tgj
Ttbp
Tp
Tgf
Tgi
Tmd Tr
Tsf
}<b
|gs |mg |qg
<gd
<gn4
<gn3
<gn5
<gn6
<gnd
gnm gnb
<gu
Tdc
Tvc
Tcd
Kch
KsgrKssm
Jgf
Kgc
Ksa
Kdd
Klg Kgl
KlvKss
J^gb^lq ^ll ^lh ^lb
??
K<m
? ?? ?
TKtp
??Kpu
??Kpg
??Kps
??Kpa
??Kpb
??
^lu
Tvv Tvt
Tsfs
}pr
Qh
Between San Andreas andnorthern Nadeau Faults
Between northern andsouthern Nadeau Faults
South of PunchbowlFault
Juni
per
Hil
lsFo
rmat
ion
? ?
Tav
Tavb Tavc
TavrTavw
Ana
verd
e Fo
rmat
ion
Juni
per
Hil
lsFo
rmat
ion
Tpbv
Tpbb
Jhc
dgm
Kcs Kpf
KdcKgp
Tsfc Tsfl
}ggm
grg
Kcsl
Kpm??
Kmm
}hg
Kpq??
}h
<a
<gt<pv
<pva
QTjhs
QTjhb
QTjh
QTjhr
QTjhc
QTjhf
QTjh
QTjhsb
QTjhv
QTjhcsQTjha
QTjhp
^dg
cru
Ttd
QTfz
Shay Mountain metamorphic complex
grb
Tgh
Tpsc
Tpscc
Tpsq
Tpsqc
TplvTpls
Tgc
Tpbd
Tgry
Tsfb
CORRELATION OF MAP UNITS
Mixed metamorphic rocks of Ord Mountains area
Tsg
? ?
KssgKssm1
K|sg K|st
KJhs
}<d
MESOZOIC
PLEISTOCENE
TERTIARY
CENOZOIC
Mill
Cre
ek F
ault
San
And
reas
Fau
lt
Age bars for all units except those in the Peninsular Ranges assemblage
Age bars only for units in the Peninsular Ranges assemblage
Mill
Cre
ek F
ault
San
And
reas
Fau
lt
Cuc
amon
ga-S
an J
acin
to F
ault
Zon
es
Generic Quaternary units common to all assemblages
Qyf Qyf4
Qyf3
Qyf2
Qyf1
Qyls
Qoa Qoc
Qvof1
Qypt
Qoa1
QolsQow
QvolsQvof
Qov
Qyv1
Qya Qyv
Qof
Qof1
Qoa7
Qoa3
Qop7
Qop6
Qop2
Qop1
Qop3
Qop4 Qop2-6Qop3-6
Qop Qopf
Qvoa
Qvoa1
Qvoa2
Qvoa3
Qvoa4
Qvoa5
Qvop
Qyf7
Qyf6
Qyf5
Qof3
Qos
Qvof3 Qvov
Qya4
Qya3
Qya6
Qya5
QesQm
Qofv
Qvor
Qyc QyeQyw
QTws
Qlh
Tm Tvsr Tvtb
Kgbd
Kld
^mqg
Lakeview Mountains pluton
Box Springs plutoniccomplex
Val Verde Pluton
Green Acres gabbro Complex
Gavilan ring complex
Cajalco Pluton
Domenigoni Valley Pluton
Pleistocene
Pliocene
Miocene
Oligocene
Eocene
TERTIARY
CRETACEOUS
CENOZOIC
MESOZOIC
PALEOZOIC(?)
JURASSIC
Kp
Generic Cretaceous rocks of the PeninsularRanges Batholith*
Rocks of the PeninsularRanges Batholith
Qch
Qsp
QTs QTnQTc
Tta
Tn Tns
Tch
Tplv
Tpsq
Tp
Tvh
Tvep
TsobTtp
Ttb
Tt
Tvem Tvema Tvemb
Tv TvsTsTcga
Tsi
Tsa
Klbc
KlhsKl
Kwsr
Kwps
Kwst
Ktr
Klt Khqd
Klmp
Klmm
Klmg
Krct
Kbpm
Kpd
Kbfg Kbg Kbft
KvtiKvtk
Kgg Kgti
Krg
Ktd
Kgbf
Kpvgb
Kpvp
Kgu
Kgb
Jbc
Ks
Jbcm
Kc
Kvsp Kvspi Kvem
^mq ^ms^mgp ^mp^mu ^mm^mg ^mi
|mp|q |c|sgp|u m
TcgTcgr
Tlm
|ms
Paloma Valley ring complex
Kght
Klct Kmeg Kthgd Ktcg
Klmt KlmlKlmtg
Kbpg
Kbt Kbfgi Kbhg Kbht Kbgt
Kvt
Kgr
Kgab Kgao Kgah Kgat Kgaa
Kgt Kgtf Kgct
KmpKmpc
Kmrg
Kmhg
Klst
Katg
KctKcgq Kcgb
Kdvg
Kg
Kgd
Kt
Ktm
Kqd
Kdqd
Kd
Khg
Kpvg Kpvt
Ksmg
Kgh
Kgam
Kbhg1
Kba
Klmc
KvrKvsKsv
Kcto
Kcg
QTwc
Ttlt
TiemaTvemt
Ktbh
?
Kg|
?Kts
Kcgd
Tfu
Tfuc
Tfl
Tflc
Tpy
Tpyc
Kwl
Klhsc
Kpvgr
Tvss
QTt
QUATERNARY
Tcs
Tco
Kg}
Tsicg
Tsis
Kwps1
Kwsru
Kwsrl
Jbc1
^mgn
Qsp1
Qsp3
Qsp4
Qsp2
Paleocene
Ktru
Ktrl
^mdx
^mdc
^mds
^msgn
^msm
^ma
TpscTpscc
Kmgt
? ?
* These units are mapped as undivided generic, because they represent common rock types associated with more than one specific pluton. Some of these units may appear on the Correlation of Map Units chart at more than one place to indicate their association with particular plutons and to show their relative age relations with other rock types that characterize those plutons.
Tgb
Tgr
Tga
Tgj
Tgrb
Tpsqc
Keh
Kgdt
Kht
Qdg Qaf
Qw Qw2
Qw1
Qf Qf2
Qf1
Qa Qc Qt Qsw Qls Qpl
Qpl1
Qe
Qs1
Qw3
Qa1
Qs
Qyw2
Qyw1
Qyw3
Qya1
Qya2
Qv QlvQl
Qyt Qysw Qypl Qys
Qyed1
Qyes1
Qvof2
Qof2 Qoa2
Qolb QoeQoed3
Qoes3
Qvosw Qvos
Qpf
Qps
_<gsq _<qc _<lsm _<sm_<cc
JUR
AS
SIC
CR
ETA
CE
OU
S O
R J
UR
AS
SIC
PAL
EO
ZO
IC
PAL
EO
CE
NE
OL
IGO
CE
NE
AN
D E
OC
EN
EM
IOC
EN
EP
LIO
CE
NE
PL
EIS
TO
CE
NE
CR
ETA
CE
OU
S
Tcr5
Tcr Tcr3
Tcr2
Tcr1
Tcr4
Cuc
amon
ga-S
an J
acin
to F
ault
Zon
es
HOLOCENE
Kgbh
Tsx
Tal
Tiemd
Klu Krl Khl
Kdp
Kml Kcr
Kkc
KbpKk Kh Krp
Kmc
Kdh
Khc Kwc
^f ^fl ^lm
^a
^fp
^sp
^h
^rl
^cp
Khr KpbmKcc
Kcm Kmx
Kwcy
^m
KJgm KJdd KJqd KJscKJdgKJta KJhb
Kao
Kbf
Kmbb
KJc
Kgdc
KcdKcdc
Kgdb
Jsc
Jwm
Jcr
Jc Ja
Jrr Jd
Js
Kaw
Kbm
Kr
Kms
PENINSULAR RANGES ASSEMBLAGE
|a
}gd
Tf
|sg
??
(Includes rocks of Peninsular Ranges andSan Gabriel Mountains assemblages)
^mn
PENNSYLVANIAN
MISSISSIPPIAN
DEVONIAN
CAMBRIAN
TstlTstl1
Tstl2
Tstd Tstm
Tmec
Tmeh
Tmea TmebTme
QstuQstcq
QstsQstr
Tc
EXPLANATION
Contact—Solid where accuracy of location ranges from well located to approximately located; dashed where very poorly located or inferred.
Fault—Solid where accurately located, dashed where approximately located, dotted where concealed. Includes strike slip, normal, reverse, oblique, and unspecified slip. Arrow and number indicate direction and amount of dip.
Thrust fault—Teeth on upper plate; solid where accurately located, dashed where approximately located, dotted where concealed. Arrow and number indicate direction and amount of dip.
Rotational slip normal fault—Bars on hanging wall side; solid where accurately located, dashed where approximately located, dotted where concealed.
Topographic lineaments— Aligned saddles, swales, and canyons.
Suture—Location approximate
Ground fissures—San Jacinto Valley area
Anticline—Solid where accurately located; dashed where approximately located; dotted where concealed. Arrowhead on axis shows direction of plunge
Syncline—Solid where accurately located; dashed where approximately located; dotted where concealed. Arrowhead on axis shows direction of plunge
Overturned anticline—Solid where accurately located; dashed where approximately located; dotted where concealed. Arrowhead on axis shows direction of plunge
Overturned syncline—Solid where accurately located; dashed where approximately located; dotted where concealed. Arrowhead on axis shows direction of plunge
Monocline—Well located
70
20
70
70
70
70
Strike and dip of bedding
Horizontal
Inclined
Vertical
Overturned
Strike and dip of foliation, primary igneous
Inclined
Vertical
Strike and dip of foliation, metamorphic
Inclined
Vertical
Bearing and plunge of linear features
Inclined70
TstrlTstf
U.S. DEPARTMENT OF THE INTERIORU.S. GEOLOGICAL SURVEY
OPEN-FILE REPORT 2006-1217Sheet 4 of 4
TadTad
GEOLOGIC MAP OF THE SAN BERNARDINO AND SANTA ANA 30′ x 60′ QUADRANGLES, CALIFORNIA
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