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Figure 2. Map showing geography of Mono Basin and surrounding area, shorelines of Lake Russell and Lake Adobe, and locations of lacustrine deposits higher than the last overflow altitudes of these lakes. Diagonal lines are modern lakes. Light dashed lines show areas of Figures 3 and 5. KS—Kirkwood Spring, BC—mouth of Bridgeport Canyon, AHS—Adobe Hills spillway, MHS—Mount Hicks spillway

Figure 2. Map showing geography of Mono Basin and surrounding area, shoreli... Available to Purchase

Published: 01 August 2002
Figure 2. Map showing geography of Mono Basin and surrounding area, shorelines of Lake Russell and Lake Adobe, and locations of lacustrine deposits higher than the last overflow altitudes of these lakes. Diagonal lines are modern lakes. Light dashed lines show areas of Figures 3 and 5 . KS
Journal Article

Drainage reversals in Mono Basin during the late Pliocene and Pleistocene Available to Purchase

Marith C. Reheis, Scott Stine, Andrei M. Sarna-Wojcicki
Journal: GSA Bulletin
Published: 01 August 2002
GSA Bulletin (2002) 114 (8): 991–1006.
DOI: https://doi.org/10.1130/0016-7606(2002)114<0991:DRIMBD>2.0.CO;2
...Figure 2. Map showing geography of Mono Basin and surrounding area, shorelines of Lake Russell and Lake Adobe, and locations of lacustrine deposits higher than the last overflow altitudes of these lakes. Diagonal lines are modern lakes. Light dashed lines show areas of Figures 3 and 5 . KS...
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View PDF for article title, Drainage reversals in Mono Basin during the late Pliocene and Pleistocene
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(a) Map of California and Nevada showing the Walker Lane tectonic region (WL) in the black dashed line and the Sierra Nevada Mountains (SN) in the gray dashed line. Thin gray lines are the U.S. Geological Survey (USGS) faults and folds with the San Andreas fault (SAF) and Garlock fault (GF) labeled. Blue box denotes area of (b). (b) Overall Map of the central Walker Lane along the California–Nevada border showing seismicity from 2001 to 2020 colored with time near the Nine Mile Ranch (NMR) sequence area (seismicity south of Mina Deflection and near Long Valley Caldera (LVC) not shown for this time period). The purple triangles indicate seismic stations. The solid gray box is area of Figure 2a,b. Mina Deflection area is shown within the gray dashed box. LVC is labeled at the southern end of the map area, with Mono Lake above that. The Nine Mile Ranch house, location of ground cracking, and the city of Hawthorne, Nevada are all labeled with red boxes. The orange square shows the location of spring that flowed after the event, then subsided. In addition, the Pine Grove Hills and Wassuk fault zones are labeled. USGS faults and folds are shown in gray. East of Mono Lake, Adobe Hills 2020 sequence in blue; Hawthorne 2011 swarm shown in yellow. (c) Photo of the Nine Mile Ranch house damage due to the main events. (d) Photo of a sand blow due to the Nine Mile Ranch events. (e) Photo of a large surface crack with a motorcycle for scale.

(a) Map of California and Nevada showing the Walker Lane tectonic region (W... Available to Purchase

Published: 28 February 2022
cracking, and the city of Hawthorne, Nevada are all labeled with red boxes. The orange square shows the location of spring that flowed after the event, then subsided. In addition, the Pine Grove Hills and Wassuk fault zones are labeled. USGS faults and folds are shown in gray. East of Mono Lake, Adobe
Journal Article

Pliocene sinistral slip across the Adobe Hills, eastern California–western Nevada: Kinematics of fault slip transfer across the Mina deflection Open Access

Sarah Nagorsen-Rinke, Jeffrey Lee, Andrew Calvert
Journal: Geosphere
Published: 01 February 2013
Geosphere (2013) 9 (1): 37–53.
DOI: https://doi.org/10.1130/GES00825.1
... of the Long Valley Caldera, transfer a portion of dextral Owens Valley fault slip northwestward onto the sinistral faults in the Adobe Hills. Dextral slip distributed across faults between the White Mountains fault zone and the Sierra Nevada and east of the Fish Lake Valley fault zone may account...
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View PDF for article title, Pliocene sinistral slip across the <span class="search-highlight">Adobe</span> Hills, eastern California–western Nevada: Kinematics of fault slip transfer across the Mina deflection
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Journal Article

Central California earthquakes of the 1830's Available to Purchase

George D. Louderback
Published: 01 January 1947
Bulletin of the Seismological Society of America (1947) 37 (1): 33–74.
DOI: https://doi.org/10.1785/BSSA0370010033
...—Late in June, just after noon. X. Comparable with the earthquake of April 18, 1906. Originated in the San Andreas fault, and violent fault-trace phenomena described by Charles Brown as observed in the hills behind Palo Alto near the present Searsville Lake: a great fissure which he describes as ten...
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Journal Article

Sierra Nevada-Great Basin boundary zone: Earthquake hazard related to structure, active tectonic processes, and anomalous patterns of earthquake occurrence Available to Purchase

J. D. VanWormer, Alan S. Ryall
Published: 01 October 1980
Bulletin of the Seismological Society of America (1980) 70 (5): 1557–1572.
DOI: https://doi.org/10.1785/BSSA0700051557
... low-velocity zone; seismicity in this area appears to be related to volcanic processes that produced thick Pliocene basalt flows in the Adobe Hills and minor historic activity in Mono Lake. In the Garfield Hills between Walker Lake and the Excelsior Mountains, there is some clustering of epicenters...
View PDF for article title, Sierra Nevada-Great Basin boundary zone: Earthquake hazard related to structure, active tectonic processes, and anomalous patterns of earthquake occurrence
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Journal Article

Crustal Structure in the Elko-Carlin Region, Nevada, during Eocene Gold Mineralization: Ruby-East Humboldt Metamorphic Core Complex as a Guide to the Deep Crust Available to Purchase

Keith A. Howard
Journal: Economic Geology
Published: 01 April 2003
Economic Geology (2003) 98 (2): 249–268.
DOI: https://doi.org/10.2113/gsecongeo.98.2.249
...-dipping normal-sense shear system, may have underlain the Piñon and Adobe Ranges about 50 km to the west before Tertiary extension, close to or under part of the Carlin trend. Eocene lakes formed on the hanging wall of the fault system during an early phase of extension and may have been linked...
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View PDF for article title, Crustal Structure in the Elko-Carlin Region, Nevada, during Eocene Gold Mineralization: Ruby-East Humboldt Metamorphic Core Complex as a Guide to the Deep Crust
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Journal Article

Geologic and seismologic aspects of the Managua, Nicaragua, earthquakes of December 23, 1972: U.S. Geological Survey Professional Paper 838, 1973 Available to Purchase

R. D. Brown, Jr., P. L. Ward, George Plafker
Published: 01 August 1974
Bulletin of the Seismological Society of America (1974) 64 (4): 1031.
DOI: https://doi.org/10.1785/BSSA0640041031
... of these northeast-trending faults extends from the surface to a depth of 8 to 10 km over a maximum length of about 15 km. The faults are mappable on land for 1.6, 5.1, 5.9 and 2.7 km; aftershock data indicate that faulting extends at least 6 km northeast of the city beneath Lake Managua. Horizontal displacements...
View PDF for article title, Geologic and seismologic aspects of the Managua, Nicaragua, earthquakes of December 23, 1972: U.S. Geological Survey Professional Paper 838, 1973
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Journal Article

Geological aspects of the May 31, 1970, Perú earthquake Available to Purchase

George Plafker, George E. Ericksen, Jaime Fernández Concha
Published: 01 June 1971
Bulletin of the Seismological Society of America (1971) 61 (3): 543–578.
DOI: https://doi.org/10.1785/BSSA0610030543
... of the region extensively damaged transportation routes and irrigation canals and temporarily dammed some rivers and lakes. The geologically most important and spectacular of these, a cataclysmic debris avalanche from between 5,500 and 6,400 m altitude on the north peak of Huascarán Mountain, buried the city...
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Core photos and stratigraphic interpretation of piston cores recovered from Lake Crescent, Washington, USA, arranged from west to east. Core photos have been processed using histogram equalization in Adobe Photoshop in order to enhance the visibility of stratigraphic features. Dates shown are the 2 sigma calibrated radiocarbon ages (cal yr B.P.) with respect to A.D. 1950.

Core photos and stratigraphic interpretation of piston cores recovered from... Available to Purchase

Published: 20 March 2019
Figure 7. Core photos and stratigraphic interpretation of piston cores recovered from Lake Crescent, Washington, USA, arranged from west to east. Core photos have been processed using histogram equalization in Adobe Photoshop in order to enhance the visibility of stratigraphic features. Dates
Image
Map of northeastern Ontario – western Quebec, Canada, showing the location of Frederick House Lake, and the varve series mentioned in the paper. All of these varve series are located at single or several closely spaced sites, except for the Lac Matagami series, which is based on 15 locations along Matagami and Soscumica lakes (see Hardy 1976). A rectangle delineates the map area shown in Fig. 2. (Base map derived from canvec_5M_CA_Hydro_shp.zip and created using Global Mapper version 20.0 and Adobe Illustrator CS6; base map data, Natural Resources Canada.)

Map of northeastern Ontario – western Quebec, Canada, showing the location ... Available to Purchase

Published: 13 May 2021
locations along Matagami and Soscumica lakes (see Hardy 1976 ). A rectangle delineates the map area shown in Fig. 2 . (Base map derived from canvec_5M_CA_Hydro_shp.zip and created using Global Mapper version 20.0 and Adobe Illustrator CS6; base map data, Natural Resources Canada.)
Image
Map showing the locations of the sub-bottom acoustic profiles collected during the 2018 reconnaissance survey of Frederick House Lake, Ontario, and the two coring sites. Inset map shows the locations of the profiles depicted on Figs. 4A and 4B. (Base map derived from OntQue_Waterbodies_250k.shp and created using Global Mapper version 20.0 and Adobe Illustrator CS6; base map data, Natural Resources Canada.)

Map showing the locations of the sub-bottom acoustic profiles collected dur... Available to Purchase

Published: 13 May 2021
Fig. 3. Map showing the locations of the sub-bottom acoustic profiles collected during the 2018 reconnaissance survey of Frederick House Lake, Ontario, and the two coring sites. Inset map shows the locations of the profiles depicted on Figs. 4A and 4B . (Base map derived from
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Megaturbidite A in cores 6A and 2C from the southern and northern lake basins of Lake Crescent, Washington, USA, respectively. Photographs have been processed using histogram equalization in Adobe Photoshop in order to enhance the visibility of stratigraphic features. Particle size distributions show normal grading in the sandy basal interval, the homogeneous nature of the thick, silty central interval, and the abrupt basal contact of the upper clay cap. Magnetic susceptibility (MS in SI units) measurements at 0.5 cm intervals reveal details of lamination in the basal sand, and contacts between the sand, silt, and clay dominated intervals of the megaturbidite. Normalized micro-X-ray fluorescence (XRF) counts reflect the content of Ca-rich lithic sand and K-rich clay.

Megaturbidite A in cores 6A and 2C from the southern and northern lake basi... Available to Purchase

Published: 20 March 2019
Figure 9. Megaturbidite A in cores 6A and 2C from the southern and northern lake basins of Lake Crescent, Washington, USA, respectively. Photographs have been processed using histogram equalization in Adobe Photoshop in order to enhance the visibility of stratigraphic features. Particle size
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Redrawn regional geological map created using Adobe Illustrator version 24.2 and created using data from Kraus and Williams (1998, 1999). The base map was provided from Kraus and Williams (1999). (a) Geological map redrawn after Kraus and Williams (1998), illustrating their interpretation of the Burntwood panel as the southern limb of the F2 McLeod Lake synform whose hinge was truncated by the McLeod Road Thrust Fault. (b) Structural orientation of the S1 and S2 cleavage after Kraus and Williams (1999). The S1 cleavage is the dominant foliation in the volcanic rocks of the McLeod Road – Birch Lake sequence and the S2 cleavage is the dominant foliation in the Burntwood turbidites. The S1 and S2 foliation trajectories are drawn using the data and map by Kraus and Williams (1999). [Colour online.]

Redrawn regional geological map created using Adobe Illustrator version 24.... Available to Purchase

Published: 05 November 2020
Fig. 22. Redrawn regional geological map created using Adobe Illustrator version 24.2 and created using data from Kraus and Williams (1998 , 1999 ). The base map was provided from Kraus and Williams (1999) . ( a ) Geological map redrawn after Kraus and Williams (1998) , illustrating
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Figure 3. Simplified geologic map of the Gaspé-Témiscouata segment of the Québec EMA—Eaux-Mortes Lake area; GA—Gastonguay anticline; MAS—Mount Alexandre Appalachians showing distribution of Upper Ordovician to lowermost Devonian rocks. syncline; MB—Maria belt; NOB—Northern outcrop belt; RS— Ristigouche syncline; Circled numbers refer to summary stratigraphic columns of Figure 4. ADOB—Angers-SCS—Squatec-Cabano syncline; SGS—Saint-Guy syncline; SJA—Saint-Jean River an-Dugal outcrop belt; AOB—Auclair Lake outcrop belt; APA—Aroostook-Percé anticliticline; LMS—Lake Matapédia syncline. norium; CBS—Chaleurs Bay synclinorium; ECOB—East-central outcrop belt; EMA—Eaux-Mortes Lake area; GA—Gastonguay anticline; MAS—Mount Alexandre syncline; MB—Maria belt; NOB—Northern outcrop belt; RS— Ristigouche syncline; SCS—Squatec-Cabano syncline; SGS—Saint-Guy syncline; SJA—Saint-Jean River anticline; LMS—Lake Matapédia syncline.

Figure 3. Simplified geologic map of the Gaspé-Témiscouata segment of the... Available to Purchase

Published: 01 January 2000
— Ristigouche syncline; Circled numbers refer to summary stratigraphic columns of Figure 4 . ADOB—Angers-SCS—Squatec-Cabano syncline; SGS—Saint-Guy syncline; SJA—Saint-Jean River an-Dugal outcrop belt; AOB—Auclair Lake outcrop belt; APA—Aroostook-Percé anticliticline; LMS—Lake Matapédia syncline. norium
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Generalized map showing locations referenced in the text. Tan shaded area is the approximate distribution of Mississippian mud-rock formations. Dashed line shows the limits of the area where separate mud-rock formations can be distinguished. Green areas are oil fields. AR = Adobe Range; CR = Confusion Range; DM = Diamond Mountains; KSW = Kane Springs Wash; NNSS = Nevada National Security Site (formerly Nevada Test Site); PR = Piñon Range; PS = Peers Spring; PV = Pine Valley; RMA = eastern limit of Roberts Mountains allochthon, principal feature of Antler orogenic belt; RV = Railroad Valley. Inset map: LV = Las Vegas; SLC = Salt Lake City.

Generalized map showing locations referenced in the text. Tan shaded area i... Available to Purchase

Published: 15 February 2020
Figure 1. Generalized map showing locations referenced in the text. Tan shaded area is the approximate distribution of Mississippian mud-rock formations. Dashed line shows the limits of the area where separate mud-rock formations can be distinguished. Green areas are oil fields. AR = Adobe Range
Journal Article

The Salvador earthquakes of December, 1936 Available to Purchase

S. Benedict Levin
Published: 01 October 1940
Bulletin of the Seismological Society of America (1940) 30 (4): 377–407.
DOI: https://doi.org/10.1785/BSSA0300040377
... photographs, by flying over the dis- trict, by examining the records of the Seismological Observatory at San Salva- dor, and finally by visiting the near-by Lake Ilopango, considered by some to be a factor in the seismic disturbance. This impromptu investigation, while necessarily incomplete, nevertheless...
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Journal Article

The Cusco, Peru, Earthquake of May 21, 1950 Available to Purchase

George E. Ericksen, Jaime Fernández Concha, Enrique Silgado
Published: 01 April 1954
Bulletin of the Seismological Society of America (1954) 44 (2A): 97–112.
DOI: https://doi.org/10.1785/BSSA04402A0097
... and the age of buildings. The buildings that were most seriously damaged were colonial churches 250 to 350 years old, old adobe houses, and new houses of combined adobe and rock or brick construction. Many of the buildings that were destroyed in this earthquake had previously been damaged during an earthquake...
View PDF for article title, The Cusco, Peru, Earthquake of May 21, 1950
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Peru earthquake of May 31, 1970; engineering geology observations Available to Purchase

Lloyd S. Cluff
Published: 01 June 1971
Bulletin of the Seismological Society of America (1971) 61 (3): 511–533.
DOI: https://doi.org/10.1785/BSSA0610030511
... vibrational effects was severe. The most intense vibrational damage occurred along the coast at Chimbote and Casma where most houses and buildings of adobe construction were destroyed or severely damage. Severe vibrational damage also occurred in cities and villages located in the Santa Valley at epicentral...
View PDF for article title, Peru earthquake of May 31, 1970; engineering geology observations
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Particle size distributions of protopyroclasts. (A) Three-dimensional rendering of X-ray computed tomography slices. On each slice shown, protopyroclasts were manually individualized using Adobe® Photoshop® and highlighted using different colors. (B) Smaller protopyroclasts individualized on scanning electron microscope images (raw image at left, binary image at right). Protopyroclasts appearing entirely surrounded by epoxy are sintered in third dimension. (C) Protopyroclast size distributions obtained in four clasts from Medicine Lake (California, USA) and Newberry (Oregon, USA) volcanoes compared with total grain size distributions (TGSDs) of four typical Plinian eruptions (Rust and Cashman, 2011). Best fits to Plinian TGSDs using a power-law distribution N = λd – D (where N is the number of particles greater than size d, λ is a scaling factor, and D is the power-law exponent), give D = 3.0–3.3, whereas protopyroclast size distributions are best fit with D = 2.4–2.6 (2.40 and 2.56 for Newberry clast 6 and clast 5, respectively; 2.40 and 2.47 for Medicine Lake clast 8 and clast 86D). The two black reference lines illustrate the difference in slope between power-law distributions with fractal dimension of 2.4 and 3.0.

Particle size distributions of protopyroclasts. (A) Three-dimensional rende... Open Access

Published: 23 July 2021
Figure 3. Particle size distributions of protopyroclasts. (A) Three-dimensional rendering of X-ray computed tomography slices. On each slice shown, protopyroclasts were manually individualized using Adobe ® Photoshop ® and highlighted using different colors. (B) Smaller protopyroclasts