stratigraphy and provenance of conglomerate beds in the puente formation near puddingstone...
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STRATIGRAPHY AND PROVENANCE OF CONGLOMERATE BEDS IN THE PUENTE FORMATION NEAR PUDDINGSTONE RESERVOIR,
EASTERN LOS ANGELES COUNTY, CALIFORNIA.
LOCATION MAP OF STUDY AREALOCATION MAP OF STUDY AREA
SANTA AN
A
MO
UN
TAINS
PUENTE HILLS
SAN JOSE H
ILLS
SAN GABRIEL MOUNTAINS
SAN BERNARDINO MOUNTAINS
ONTARIO
CORONA
CHINO VALLEY
POMONA
SANTA ANA
LOS ANGLES
PASADENA
LONG BEACH
SANTA
ANA
RIV
ER
SA
NG
ABR
IEL
RIVER
118° 30' 118° 00'
34° 15'
34° 00'
34° 30'117° 30' 117° 00'
33° 45'
117° 45'
SAN DIMAS
PACIFIC OCEAN
STUDY AREA
KEY:
Known middle to upper Miocene shoreline and mainland area of Miocene sediments (Woodford, 1946)
LOCATION MAP OF FRANK G BONELLI PARKLOCATION MAP OF FRANK G BONELLI PARK
1100
PuddingstoneReservoir
FRANK G BONELLIREGIONAL COUNTY
PARK
SHELTONS TYPE SECTION FOR EASTERN SAN JOSE HILLS
Red area represents the rocks found within the study are
GEOLOGIC MAP OF STUDY AREAGEOLOGIC MAP OF STUDY AREA
12001100
1000
1100
1000
PuddingstoneReservoir
3020
21
30
60
70
39
25
19
22
48
33
3449
41
4630
2021
33
24 30
29
28
20
5
30
35
15
25
17
19
39
A
B
A'
B'
A"
B"
TCg A
TCg A
TCg A
TCg C
TCg C
Tp
Tp
Tp
Tp
Tp
Tgv
Tgv
TCg C
ss
ss
ss
ss
ss
ss
ss
ss
ss
TCg B
ss
4020
10
40
38
16 18
302560
25
35
40
85D
U
Tgv
1
2
3
5
6
457 F
reew
ay
Via Verde Drive
Rag
ing
Wat
ers
Drive
LOCATION 1
LOCATION 2
LOCATION 3
LOCATION 4
LOCATION 5
LOCATION 6
1200 Ft.
1000 Ft.
1200 Ft.
1000 Ft.
CROSS SECTION A - A", ALONG HIGHWAY 57
N 56° W N 41° W
N 10° W N 31° W
A A' A"
B"B'B
1200 Ft.
1000 Ft.
800 Ft.
1200 Ft.
1000 Ft.
800 Ft.
800 Ft.
CROSS SECTION B - B", NEAR PUDDINGSTONE RESERVOIR
EXLPANATION
TCg A
TCg B
TCg C
Tgv
Puente Formation (T p): siltsones, sandstones and shalesSandstone (ss): mapable sandstone beds found in the Puente Formation.
Glendora Volcanics (Tgv): intermediate to felsic volcanics, breccias, flows, and agglomerates. 15 -16 Ma. (weigand, 1994; Nourse, 1998)
Conglomerate (TCg (C)): mostly basement clasts with minor amounts of volcanics depending on location. All found in sandy matrix.
Conglomerate TCg (B)): Mostly porphyritic andesite seprated by sandstone horizon. All in sandy matrix.
Conglomerate (TCg (A)): Mostly rhyolite to dacite. Found in well cemented sandy matrix.
Tp
ss
GEOLOGIC MAP OF BONELLI PARK NEAR PUDDINGSTONE RESERVOIR, CALIFORNIA
GEOLOGIC SYMBOLS
0 500 1000 ft
1 inch equals 500 feet. Or, 1 inch equals 150 meters. no vertical exaggeration
N14°
magnetic north declination, center of map
12001100
1000
1100
1000
PuddingstoneReservoir
3020
21
30
60
70
39
25
19
22
48
33
3449
41
4630
2021
33
24 30
29
28
20
5
30
35
15
25
17
19
39
A
B
A'
B'
A"
B"
TCg A
TCg A
TCg A
TCg C
TCg C
TC
g C
Tp
Tp
Tp
Tp
Tp
Tgv
Tgv
TCg C
ss
ss
ss
ss
ss
ss
ss
ss
ss
TCg A
ss
4020
10
40
38
1618
302560
25
35
40
85D
U
Tgv
150 m il es050
l ocat i on of study area
122° 120° 118° 116°
42°
40°
38°
36°
34°
CALIFORNIA
A B
25°
Strike and dip of beds
Syncline, with plunge direction, dashed where approximately located
Anticline, with plunge direction, dashed where approximately located
Contact
Contact where approximatly located
Fault, showing dip, dashed where approximately located
Park roads
Highways
Stream and Lake line locations
Conglomerate clast sampling locations
Cross section lines
U
D
Geology by: McLarty, Andrew H. and Nourse, Jonathan A. Department of geologic sciences, California State Polytechnic University. Pomona California. 2000.
1
1
2
3
5
6
4
1200 Ft.
1000 Ft.
1200 Ft.
1000 Ft.
CROSS SECTION A - A", ALONG HIGHWAY 57
N 56° W N 41° W
N 10° W N 31° W
A A' A"
B"B'B
1200 Ft.
1000 Ft.
800 Ft.
1200 Ft.
1000 Ft.
800 Ft.
800 Ft.
CROSS SECTION B - B", NEAR PUDDINGSTONE RESERVOIR
STRATIGRAPHY
PU
EN
TE
FO
RM
AT
ION
UP
PE
R M
IOC
EN
E -
LO
WE
R P
LIO
CE
NE
GLE
ND
OR
A V
OL.
KMz
Q
Th.Fm.Per. STRATIGRAPHIC SECTION DESCRIPTION
STRATIGRAPHIC SECTION, EASTERN PUENTE - SAN JOSE HILLS NEAR PUDDINGSTONE RESERVOIR
Conglomerate (TCg (C)): mostly basement clasts with abundant volcanic clasts in higest and lowest levels, all in sandy maxrix.
Puente Formation (Tp): siltstone, sandstone, and shale
Conglomerate (TCg (B)): Two beds with predominantly porphyritic andesite clasts separated by sandstone horizon, all in sandy matrix.
Puente Formation (Tp): siltstone, sandstone, and shale
Conglomerate (TCg (A)): Mostly rhyolite to dacite clasts, all in sandy maxrix.
Glendora Volcanics (Tgv): intermediate to felsic volcanic, breccias, flows, and agglomerates. 15 - 16 Ma. (Weigand et al, 1994; Nourse et al. 1998)
Basement complex (bc), late Cretaceous, quartz diorite / tonalite
Alluvium (Qal) and thick soil horizon.
100
- 1
55
Ft.
700
-14
00 F
t.1
00
-20
0 F
t.2
80
- 3
44
Ft.
100
-2
40
Ft.
787
- 3
49
7 F
t.
McLarty, 2000
OLIG
. Mountian Meadow dacite, 27 28 Ma (Hazelton, pers. comm.)
MID
DLE
MIO
CE
NE
STEREONET RESULTS
NEqual Area
Equal Area
N
Figure 5b. - poles to bedding of small fold found in the Puente Formation near south shoreline, Puddingstone Reservoir.
Figure 5a. - poles to bedding in Puente Formation south and west Puddingstone Reservoir.
conglomerate
sandstone
siltstone
KEY
Plunging fold axis : 235° / 3°SW
Plunging fold axis : 125° / 31°SE
Name of Clast Location 1 Location 2 Location 3 Location 4 Location 5 Location 6 Rhyolite - dacite 53.6 7 0 9.7 8.8 47.7 Porphyritic andesite 21.7 47.1 9.2 4 5.6 28.2 Aphanitic andesite 18.3 0 5.7 0 0 16.5 Basaltic andesite 6 6.4 0 0 0 6.8 Porphyritic basalts 0.4 0 0 0 0 0.8 Andesite 0 26.7 0 7.6 6.3 0 Flow banded rhyolite 0 9.3 0 3 4.8 0 Basalt - vasicular basalts 0 3.5 0 5.9 0 0 Agglomerate 0 0 0 10.7 0 0 Granitoids (granite, tonolite, aplite) 0 0 25.3 13.6 15.9 0 Diorite - gabbro 0 0 13.8 6.8 8 0 Quartzite 0 0 6.9 4.9 4.8 0 Gneiss 0 0 5.7 8.8 18.3 0 Amphiblite schist 0 0 0 0 1.3 0 Mylonite 0 0 33.4 25 26.2 0
total % 100 100 100 100 100 100N number of clasts collected 235 172 157 104 126 103
SUMMARY OF ALL CLAST COUNTS FROM SIX CONGLOMERATE BEDS IN THE SUMMARY OF ALL CLAST COUNTS FROM SIX CONGLOMERATE BEDS IN THE STUDY AREASTUDY AREA
PERCENT OF TOTAL CLASTS AT 6 CONGLOMERATE LOCATIONS
Abundance of Clasts at 6 Conglomerate Locations
0
15
30
45
Location 1 Location 2 Location 3 Location 4 Location 5 Location 6
Rhyolite - dacite Porphyritic andesite Aphanitic andesite
Basaltic andesite Porphyritic basalts Andesite
Flow banded rhyolite Basalt - vasicular basalts Agglomerate
Granitoids (granite, tonolite, aplite) Diorite - gabbro Quartzite
Gneiss Amphiblite schist agglomerate
Name of Clast location 1 location 2 location 3 location 4 location 5 location 6 Volcanics 100 100 14.9 40.9 25.5 100 Plutonics 0 0 39.1 20.4 23.9 0 Metamorphics 0 0 46 38.7 50.6 0
total % 100 100 100 100 100 100N number of clasts collected 235 172 157 104 126 103
SUMMARY OF ONLY VOLCANIC, PLUTONIC, AND METAMORPMIC CLAST SUMMARY OF ONLY VOLCANIC, PLUTONIC, AND METAMORPMIC CLAST COUNTS FROM SIX CONGLOMERATE BEDS IN STUDY AREACOUNTS FROM SIX CONGLOMERATE BEDS IN STUDY AREA
PERCENT OF TOTAL CLASTS AT 6 CONGLOMERATE LOCATIONS
Percent of total clasts at 6 conglomerate locations.
0
20
40
60
80
100
location 1 location 2 location 3 location 4 location 5 location 6
Locations within study area
Pe
rce
nt
of
tota
l c
las
ts c
ou
nte
d
Volcanics Plutonics Metamorphics
Location 1
0
5
10
15
20
25
30
35
40
45
50
55
Rhyolite -dacite
Porphyriticandesite
Aphaniticandesite
Basalticandesite
Porphyriticbasalts
Andesite Flowbandedrhyolite
Basalt -vasicularbasalts
Agglomerate
Granitoids(granite,tonolite,aplite)
Diorite -gabbro
Quartzite Gneiss Amphibliteschist
Mylonite
Clast lithologies
Pe
rce
nt
of
235
tota
l cla
sts
cou
nte
d
VOLCANICS PLUTONICS METAMORPHICS
Location 2
0
5
10
15
20
25
30
35
40
45
50
55
Rhyolite -dacite
Porphyriticandesite
Aphaniticandesite
Basalticandesite
Porphyriticbasalts
Andesite Flowbandedrhyolite
Basalt -vasicularbasalts
Agglomerate
Granitoids(granite,tonolite,aplite)
Diorite -gabbro
Quartzite Gneiss Amphibliteschist
Mylonite
Clasts lithologies
Per
cent
of 1
72 to
tal c
last
s co
unte
d VOLCANICS PLUTONICS METAMORPHICS
Location 3
0
5
10
15
20
25
30
35
40
45
50
55
Rhyolite -dacite
Porphyriticandesite
Aphaniticandesite
Basalticandesite
Porphyriticbasalts
Andesite Flowbandedrhyolite
Basalt -vasicularbasalts
Agglomerate
Granitoids(granite,tonolite,aplite)
Diorite -gabbro
Quartzite Gneiss Amphibliteschist
Mylonite
Clast lithologies
Per
cent
of 1
57 c
last
s co
unte
d
VOLCANICS PLUTONICS MEATMORPHICS
Location 4
0
5
10
15
20
25
30
35
40
45
50
55
Rhyolite -dacite
Porphyriticandesite
Aphaniticandesite
Basalticandesite
Porphyriticbasalts
Andesite Flowbandedrhyolite
Basalt -vasicularbasalts
Agglomerate
Granitoids(granite,tonolite,aplite)
Diorite -gabbro
Quartzite Gneiss Amphibliteschist
Mylonite
Clast lithologies
Per
cent
of 1
04 to
tal c
last
s co
unte
d VOLCANICS PLUTONICS MEATMORPHICS
Location 5
0
5
10
15
20
25
30
35
40
45
50
55
Rhyolite -dacite
Porphyriticandesite
Aphaniticandesite
Basalticandesite
Porphyriticbasalts
Andesite Flowbandedrhyolite
Basalt -vasicularbasalts
Agglomerate
Granitoids(granite,tonolite,aplite)
Diorite -gabbro
Quartzite Gneiss Amphibliteschist
Mylonite
Clast lithologies
Per
cent
of 1
26 to
tal c
last
s co
unte
d VOLCANICS PLUTONICS METAMORPHICS
Location 6
0
5
10
15
20
25
30
35
40
45
50
55
Rhyolite -dacite
Porphyriticandesite
Aphaniticandesite
Basalticandesite
Porphyriticbasalts
Andesite Flowbandedrhyolite
Basalt -vasicularbasalts
Agglomerate
Granitoids(granite,tonolite,aplite)
Diorite -gabbro
Quartzite Gneiss Amphibliteschist
Mylonite
Clast lithologies
perc
ent o
f 103
tota
l cla
sts
coun
ted VOLCANICS PLUTONICS METAMORPHICS
BLOCK DIAGRAM DURING RELIZIAN TIMEBLOCK DIAGRAM DURING RELIZIAN TIME
18 - 15 Ma.
N
W
BLOCK DIAGRAM DURING LUISIAN-MOHNIAN TIMEBLOCK DIAGRAM DURING LUISIAN-MOHNIAN TIME
N
W
Erosion and deposition of silt and mud from distal source.
15 - 11 Ma.
BLOCK DIAGRAM DURING LATE MIOCENE TIMEBLOCK DIAGRAM DURING LATE MIOCENE TIME
N
W
11 - 7 Ma.
Erosion and deposition of silt and mud from distal source.
BLOCK DIAGRAM DURING LATE MIOCENE-EARLY PLIOCENE TIMEBLOCK DIAGRAM DURING LATE MIOCENE-EARLY PLIOCENE TIME
N
W
Erosion and deposition of silt and mud from distal source.
7 - 4 Ma.
LOCATION MAP OF STUDY AREALOCATION MAP OF STUDY AREA
SANTA AN
A
MO
UN
TAINS
PUENTE HILLS
SAN JOSE H
ILLS
SAN GABRIEL MOUNTAINS
SAN BERNARDINO MOUNTAINS
ONTARIO
CORONA
CHINO VALLEY
POMONA
SANTA ANA
LOS ANGLES
PASADENA
LONG BEACH
SANTA
ANA
RIV
ER
SA
NG
ABR
IEL
RIVER
118° 30' 118° 00'
34° 15'
34° 00'
34° 30'117° 30' 117° 00'
33° 45'
117° 45'
SAN DIMAS
PACIFIC OCEAN
STUDY AREA
KEY:
Known middle to upper Miocene shoreline and mainland area of Miocene sediments (Woodford, 1946)
STRATIGRAPHY
PU
EN
TE
FO
RM
AT
ION
UP
PE
R M
IOC
EN
E -
LO
WE
R P
LIO
CE
NE
GLE
ND
OR
A V
OL.
KMz
Q
Th.Fm.Per. STRATIGRAPHIC SECTION DESCRIPTION
STRATIGRAPHIC SECTION, EASTERN PUENTE - SAN JOSE HILLS NEAR PUDDINGSTONE RESERVOIR
Conglomerate (TCg (C)): mostly basement clasts with abundant volcanic clasts in higest and lowest levels, all in sandy maxrix.
Puente Formation (Tp): siltstone, sandstone, and shale
Conglomerate (TCg (B)): Two beds with predominantly porphyritic andesite clasts separated by sandstone horizon, all in sandy matrix.
Puente Formation (Tp): siltstone, sandstone, and shale
Conglomerate (TCg (A)): Mostly rhyolite to dacite clasts, all in sandy maxrix.
Glendora Volcanics (Tgv): intermediate to felsic volcanic, breccias, flows, and agglomerates. 15 - 16 Ma. (Weigand et al, 1994; Nourse et al. 1998)
Basement complex (bc), late Cretaceous, quartz diorite / tonalite
Alluvium (Qal) and thick soil horizon.
100
- 1
55
Ft.
700
-14
00 F
t.1
00
-20
0 F
t.2
80
- 3
44
Ft.
100
-2
40
Ft.
787
- 3
49
7 F
t.
McLarty, 2000
OLIG
. Mountian Meadow dacite, 27 28 Ma (Hazelton, pers. comm.)
MID
DLE
MIO
CE
NE
1200 Ft.
1000 Ft.
1200 Ft.
1000 Ft.
CROSS SECTION A - A", ALONG HIGHWAY 57
N 56° W N 41° W
N 10° W N 31° W
A A' A"
B"B'B
1200 Ft.
1000 Ft.
800 Ft.
1200 Ft.
1000 Ft.
800 Ft.
800 Ft.
CROSS SECTION B - B", NEAR PUDDINGSTONE RESERVOIR
THE END