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  1. Title: Mississippi River Valley & Ohio River Valley, 1778 (Image 2 of 4) (Raster Image)

    Contributors:

    Summary: This layer is a georeferenced raster image of the historic paper map entitled: A new map of the western parts of Virginia, Pennsylvania, Maryland, and North Carolina : comprehending the River Ohio, and all the rivers, which fall into it; part of the River Mississippi, the whole of the Illinois River, Lake Erie; part of the lakes Huron, Michigan &c. and all the country bordering on these lakes and rivers, by Thos. Hutchins ; engrav'd by T. Cheevers. It was published by T. Hutchins in 1778. Scale [ca. 1:1,270,000]. This layer is image 2 of 4 total images of the four sheet source map, representing the northeast portion of the map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Great Lakes and St. Lawrence Albers (NAD 1983) projected coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities, Native American villages, and other human settlements, forts, territorial boundaries, shoreline features, roads, portages, and more. Relief shown pictorially and by hachures. Includes descriptive and historical notes.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

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  2. Title: Mississippi River Valley & Ohio River Valley, 1778 (Image 4 of 4) (Raster Image)

    Contributors:

    Summary: This layer is a georeferenced raster image of the historic paper map entitled: A new map of the western parts of Virginia, Pennsylvania, Maryland, and North Carolina : comprehending the River Ohio, and all the rivers, which fall into it; part of the River Mississippi, the whole of the Illinois River, Lake Erie; part of the lakes Huron, Michigan &c. and all the country bordering on these lakes and rivers, by Thos. Hutchins ; engrav'd by T. Cheevers. It was published by T. Hutchins in 1778. Scale [ca. 1:1,270,000]. This layer is image 4 of 4 total images of the four sheet source map, representing the southeast portion of the map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Great Lakes and St. Lawrence Albers (NAD 1983) projected coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities, Native American villages, and other human settlements, forts, territorial boundaries, shoreline features, roads, portages, and more. Relief shown pictorially and by hachures. Includes descriptive and historical notes.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

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  3. Title: Mississippi River Valley & Ohio River Valley, 1778 (Image 1 of 4) (Raster Image)

    Contributors:

    Summary: This layer is a georeferenced raster image of the historic paper map entitled: A new map of the western parts of Virginia, Pennsylvania, Maryland, and North Carolina : comprehending the River Ohio, and all the rivers, which fall into it; part of the River Mississippi, the whole of the Illinois River, Lake Erie; part of the lakes Huron, Michigan &c. and all the country bordering on these lakes and rivers, by Thos. Hutchins ; engrav'd by T. Cheevers. It was published by T. Hutchins in 1778. Scale [ca. 1:1,270,000]. This layer is image 1 of 4 total images of the four sheet source map, representing the northwest portion of the map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Great Lakes and St. Lawrence Albers (NAD 1983) projected coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities, Native American villages, and other human settlements, forts, territorial boundaries, shoreline features, roads, portages, and more. Relief shown pictorially and by hachures. Includes descriptive and historical notes.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

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  4. Title: St. Louis, Missouri and vicinity, 1903 (Raster Image)

    Contributors:

    Summary: This layer is a georeferenced raster image of the historic, topographic paper map entitled: Saint Louis quadrangle, Missouri - Illinois, [by the] Department of the Interior, U.S. Geological Survey; H. M. Wilson, geographer; topography by Chas. E. Cooke, Wm. O. Tufts, Gilbert Young and City of St. Louis; control by U.S.C. and G.S. and Geo. T. Hawkins. Ed. of Apr. 1904, reprinted 1932. Surveyed 1903. It was published by U.S.G.S. Scale 1:62,500. Covers City of Saint Louis, and portions of Saint Louis County, Missouri, and Saint Clair and Madison Counties, Illinois. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Missouri East State Plane Coordinate System NAD27 (in Feet) (Fipszone 2401). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This is a typical topographic map portraying both natural and manmade features. It shows and names works of nature, such as mountains, valleys, lakes, rivers, vegetation, etc. It also identify the principal works of humans, such as roads, railroads, boundaries, transmission lines, major buildings, etc. Relief is shown with standard contour intervals of 20 feet and spot heights. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

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  5. Title: View of Fort Wayne Inda

    Contributors:

    Summary: Bird's-eye view. Facsimile. Left and right sides of original cut off creating the following texts: 'lished by J.T. Palmatary' and 'Drawn on stone & printed in oil colors by Middleton, Wallace & 115 wa.' Scale not given. Published by J.T. Palmatary.

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  6. Title: Robinson's standard map of South Africa

    Contributors:

    Summary: Relief shown by hachures.; Title in English and Russian. Text, legend, and place-names in English. Statement in upper margin in English and 2 languages in Arabic alphabet.; "Entered at Stationers Hall, London, Saturday 20th May, 1854."; "Corr. to 1855 from general Schubert's official map."; Originally printed on 10 sheets.; Includes text, notes, population table, and hand col. inset of geology of Crimea and adjacent regions. 164 x 220 centimeters, sheets 88 x 115 centimeters Scale [1:1,267,200] General Map Collection

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  7. Title: India, 1788 (Image 2 of 4) (Raster Image)

    Contributors:

    Summary: This layer is a georeferenced raster image of the historic paper map entitled: A map of Hindoostan, or the Mogul Empire : from the latest authorities. Inscribed to Sir Joseph Banks Bart., President of the Royal Society & c., & c. by his much obliged & faithful friend and servant, J. Rennell, 1st Jany. 1788 ; the map engraved by I. Phillips & W. Harrison ; writing by T. Harmar. It was published by James Rennell in 1788. Scale [ca. 1:3,000,000]. This layer is image 2 of 4 total images of the four sheet source map, covering the southeast portion of the map. Covers primarily India and adjacent portions of Asia.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Asia North Lambert Conformal Conic coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, roads, territorial boundaries, shoreline features, and more. Relief shown pictorially. This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

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  8. Title: India, 1788 (Image 4 of 4) (Raster Image)

    Contributors:

    Summary: This layer is a georeferenced raster image of the historic paper map entitled: A map of Hindoostan, or the Mogul Empire : from the latest authorities. Inscribed to Sir Joseph Banks Bart., President of the Royal Society & c., & c. by his much obliged & faithful friend and servant, J. Rennell, 1st Jany. 1788 ; the map engraved by I. Phillips & W. Harrison ; writing by T. Harmar. It was published by James Rennell in 1788. Scale [ca. 1:3,000,000]. This layer is image 4 of 4 total images of the four sheet source map, covering the northeast portion of the map. Covers primarily India and adjacent portions of Asia. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Asia North Lambert Conformal Conic coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, roads, territorial boundaries, shoreline features, and more. Relief shown pictorially. This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

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  9. Title: India, 1788 (Image 3 of 4) (Raster Image)

    Contributors:

    Summary: This layer is a georeferenced raster image of the historic paper map entitled: A map of Hindoostan, or the Mogul Empire : from the latest authorities. Inscribed to Sir Joseph Banks Bart., President of the Royal Society & c., & c. by his much obliged & faithful friend and servant, J. Rennell, 1st Jany. 1788 ; the map engraved by I. Phillips & W. Harrison ; writing by T. Harmar. It was published by James Rennell in 1788. Scale [ca. 1:3,000,000]. This layer is image 3 of 4 total images of the four sheet source map, covering the northwest portion of the map. Covers primarily India and adjacent portions of Asia. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Asia North Lambert Conformal Conic coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, roads, territorial boundaries, shoreline features, and more. Relief shown pictorially. This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

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  10. Title: India, 1788 (Image 1 of 4) (Raster Image)

    Contributors:

    Summary: This layer is a georeferenced raster image of the historic paper map entitled: A map of Hindoostan, or the Mogul Empire : from the latest authorities. Inscribed to Sir Joseph Banks Bart., President of the Royal Society & c., & c. by his much obliged & faithful friend and servant, J. Rennell, 1st Jany. 1788 ; the map engraved by I. Phillips & W. Harrison ; writing by T. Harmar. It was published by James Rennell in 1788. Scale [ca. 1:3,000,000]. This layer is image 1 of 4 total images of the four sheet source map, covering the southwest portion of the map. Covers primarily India and adjacent portions of Asia.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Asia North Lambert Conformal Conic coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, roads, territorial boundaries, shoreline features, and more. Relief shown pictorially. This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

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  11. Title: Map of the town of Michigan

    Contributors:

    Summary: Extent: 1 map Notes: Cadastral map. Oriented with north to the right. Includes area map. Scale 1:3,960. 330 ft. to 1 inch

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  12. Title: A map of Scotland : divided into counties, shewing the principal roads, railways, rivers, canals, lochs, mountains, islands, &c

    Contributors:

    Summary: Cartographic Details: Scale [1:316,800]. 1 in. = 5 mi. (W 8°--W 2°N 60°--N 54°).Relief shown by hachures. Illustration: View of Melrose Abbey / drawn by T. Allom, engraved by H. Griffiths.Originally published in 1 sheet (?). color, dissected, mounted on cloth, and bound in 3 volumes ; 179 x 124 cm.; sheet Scale [1:316,800]. 1 inch = 5 miles General Map Collection

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  13. Title: North America, agreeable to the most approved maps and charts

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    Summary: Scale not given Scale not given. General Map Collection

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  14. Title: View of Indianapolis

    Contributors:

    Summary: Panorama.; Shows view of Indianapolis from the top of the Asylum for the Blind.; Though credited ... as being 'drawn from nature' by E. Sachse, there is evidence that this view was actually done by James T. Palmatary, who is designated only as publisher--Map verso.; Facsimile.; Includes drawings of prominent buildings and views of building facades along Washington Street North East and Washington Street South East surrounding the view. Not drawn to scale

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  15. Title: Map showing oil, gas, and gas storage fields in Indiana

    Contributors:

    Summary: Compilation complete to December 1998.; Base map digitized from 1978 U.S. Geological Survey map of Indiana. Scale 1:500,000. Scale 1:550,000

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  16. Title: Minneapolis, Saint Paul and vicinity

    Contributors:

    Summary: 68 x 87 centimeters Scale approximately 1:36,000. Minneapolis and St. Paul Maps and Atlases

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  17. Title: Pompei, Italy, 1832 (Raster Image)

    Contributors:

    Summary: This layer is a georeferenced raster image of the historic paper map entitled: Pompeii, drawn by W.B. Clarke, Arch.; engraved by T.E. Nicholson. It was published under the superintendence of the Society for the Diffusion of Useful Knowledge [by] Baldwin & Cradock, July 1, 1832. Scale [ca. 1:3,450]. Covers Pompei, Italy. The image inside the map neatline is georeferenced to the surface of the earth and fit to the 'European Datum 1950 UTM Zone 33 North' coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map.This map shows features such as roads, drainage, built-up areas, selected buildings, excavation sites, ancient sites, gates, original shoreline, and more. Relief shown by hachures. Includes index, ill. of principal buildings and sites, a view of Pompeii, 'Plan of the coast in the vicinity of Vesuvius', and 'Domus Pansae.'This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

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  18. Title: Folds: Offshore of Point Reyes, California, 2009

    Contributors:

    Summary: This line shapefile contains geologic folds within the offshore region of Point Reyes map area, California. Folds in the Point Reyes map area are identified on seismic-reflection data based on abrupt truncation or warping of reflections and (or) juxtaposition of reflection panels with different seismic parameters such as reflection presence, amplitude, frequency, geometry, continuity, and vertical sequence. The Point Reyes Fault Zone runs through the map area and is an offshore curvilinear reverse fault zone with predominantly north-side-up motion (Hoskins and Griffiths, 1971; McCulloch, 1987; Heck and others, 1990; Stozek, 2012) that likely connects with the western San Gregorio fault further to the south (Ryan and others, 2008), making it part of the San Andreas Fault System. The Point Reyes Fault Zone is characterized by a 5 to 11 km-wide zone of deformation in the shallow subsurface that is associated with two main fault structures, the Point Reyes Fault and the western Point Reyes Fault. Near the Point Reyes headland, vertical displacement of granitic basement across the Point Reyes Fault is at least 1.4 km (McCulloch, 1987). Offshore Double Point, vertical displacement on the Point Reyes Fault is difficult to assess because subsurface age constraints from nearby wells are lacking, and there are few offset horizons across the fault imaged on available seismic data. However, warping and folding of Neogene strata are clearly visible on high-resolution seismic data. The western Point Reyes Fault is defined by a broad anticlinal structure visible in both industry and high-resolution seismic datasets that exhibits that same sense of vergence (north-side-up) as the Point Reyes Fault. Folds were primarily mapped by interpretation of seismic reflection profile data (see field activity S-8-09-NC). The seismic reflection profiles were collected in 2009. The map that show these data are published in Open-File Report 2015-1114, "California State Waters Map Series—Offshore of Point Reyes, California." This layer is part of USGS Data Series 781. In 2007, the California Ocean Protection Council initiated the California Seafloor Mapping Program (CSMP) to create a comprehensive seafloor map of high-resolution bathymetry, marine benthic habitats and geology within the 3-nautical-mile limit of California's State Waters. CSMP has divided coastal California into 110 map blocks, each to be published individually as United States Geological Survey Open-File Reports (OFRs) or Scientific Investigations Maps (SIMs) at a scale of 1:24,000. Maps display seafloor morphology and character, identify potential marine benthic habitats and illustrate both the seafloor geology and shallow (to about 100 m) subsurface geology. Data layers for bathymetry, bathymetric contours, acoustic backscatter, seafloor character, potential benthic habitat and offshore geology were created for each map block, as well as regional-scale data layers for sediment thickness, depth to transition, transgressive contours, isopachs, predicted distributions of benthic macro-invertebrates and visual observations of benthic habitat from video cruises over the entire state. This coverage can be used to to aid in assessments and mitigation of geologic hazards in the coastal region and to provide sufficient geologic information for land-use and land-management decisions both onshore and offshore. These data are intended for science researchers, students, policy makers, and the general public. This information is not intended for navigational purposes.The data can be used with geographic information systems (GIS) software to display geologic and oceanographic information. Watt, J.T., Manson, M.W., and Greene, H.G. (2014). Folds: Offshore of Point Reyes, California, 2009. California State Waters Map Series Data Catalog: U.S. Geological Survey Data Series 781. Available at: http://purl.stanford.edu/mr840rd2952. Map political location: Marin County, California Compilation scale: 1:24,000 Base maps used are hillshades generated from IfSAR, LiDAR, and multibeam mapping both onshore and offshore see see Bathymetry--Offshore Point Reyes, California, DS 781 for more information, California, DS 781, for more information). References Cited Heck, R.G., Edwards, E.B., Kronen, J.D., Jr., and Willingham, C.R., 1990, Petroleum potential of the offshore outer Santa Cruz and Bodega basins, California, in Garrison, R.E., Greene, H.G., Hicks, K.R., Weber, G.E., and Wright, T.L., eds. Geology and tectonics of the central California coastal region, San Francisco to Monterey: Pacific Section, American Association of Petroleum Geologists Bulletin GB67, p. 143-164. Hoskins E.G., Griffiths, J.R., 1971, Hydrocarbon potential of northern and central California offshore: American Association of Petroleum Geologists Memoir 15, p. 212-228. McCulloch, D.S., 1987, Regional geology and hydrocarbon potential of offshore central California, in Scholl, D.W., Grantz, A., and Vedder, J.G., eds., Geology and Resource Potential of the Continental Margin of Western North America and Adjacent Oceans Beaufort Sea to Baja California: Houston, Texas, Circum-Pacific Council for Energy and Mineral Resources, Earth Science Series, v. 6., p. 353-401. Ryan, H.F., Parsons, T., and Sliter, R.W., 2008, Vertical tectonic deformation associated with the San Andreas Fault offshore of San Francisco, California: Tectonophysics, v. 475, p. 209-223. Stozek, B.A., 2012, Geophysical evidence for Quaternary deformation within the offshore San Andreas fault system, northern California: Masters Thesis, San Francisco State University, 141 p. This layer is presented in the WGS84 coordinate system for web display purposes. Downloadable data are provided in native coordinate system or projection.

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  19. Title: Faults: Offshore of Bolinas, California, 2009

    Contributors:

    Summary: This line shapefile contains fault lines for the offshore area of Bolinas, California. The map area straddles the right-lateral transform boundary between the North American and Pacific plates and is cut by several active faults that cumulatively form a distributed shear zone, including the San Andreas Fault, the eastern strand of the San Gregorio Fault, the Golden Gate Fault, and the Potato Patch Fault (Bruns and others, 2002; Ryan and others, 2008). These faults are covered by sediment (mostly unit Qms) with no seafloor expression, and are mapped using seismic-reflection data (see field activities S-8-09-NC and L-1-06-SF). The San Andreas Fault is the primary plate-boundary structure and extends northwest through the southern part of the map area before passing onshore at Bolinas Lagoon. This section of the San Andreas Fault has an estimated slip rate of 17 to 24 mm/yr (U.S. Geological Survey, 2010), and the devastating Great 1906 California earthquake (M 7.8) is thought to have nucleated on the San Andreas a few kilometers south of this map area offshore of San Francisco (e.g., Bolt, 1968; Lomax, 2005). The San Andreas Fault forms the boundary between two distinct basement terranes, Upper Jurassic and Lower Cretaceous melange and graywacke sandstone of the Franciscan Complex to the east, and Late Cretaceous granitic and older metamorphic rocks of the Salinian block to the west. Franciscan Complex rocks (unit KJf, undivided) form seafloor outcrops adjacent to the shoreline southeast of Stinson Beach that are commonly continuous with onshore coastal outcrops. Faults were primarily mapped by interpretation of seismic reflection profile data (see field activities S-8-09-NC and L-1-06-SF). The seismic reflection profiles were collected between 2006 and 2009. In 2007, the California Ocean Protection Council initiated the California Seafloor Mapping Program (CSMP) to create a comprehensive seafloor map of high-resolution bathymetry, marine benthic habitats and geology within the 3-nautical-mile limit of California's State Waters. CSMP has divided coastal California into 110 map blocks, each to be published individually as United States Geological Survey Open-File Reports (OFRs) or Scientific Investigations Maps (SIMs) at a scale of 1:24,000. Maps display seafloor morphology and character, identify potential marine benthic habitats and illustrate both the seafloor geology and shallow (to about 100 m) subsurface geology. Data layers for bathymetry, bathymetric contours, acoustic backscatter, seafloor character, potential benthic habitat and offshore geology were created for each map block, as well as regional-scale data layers for sediment thickness, depth to transition, transgressive contours, isopachs, predicted distributions of benthic macro-invertebrates and visual observations of benthic habitat from video cruises over the entire state. These data are intended for science researchers, students, policy makers, and the general public. This information is not intended for navigational purposes.The data can be used with geographic information systems (GIS) software to display geologic and oceanographic information. Additionally, this coverage can provide a geologic map for the public and geoscience community to aid in assessments and mitigation of geologic hazards in the coastal region and sufficient geologic information for land-use and land-management decisions both onshore and offshore. This information is not intended for navigational purposes. Johnson, S.Y., Greene, H.G., Manson, M.W., Hartwell, S.R., Endris, C.A., and Watt, J.T. (2014). Faults: Offshore of Bolinas, California, 2009. California State Waters Map Series Data Catalog: U.S. Geological Survey Data Series 781. Available at: http://purl.stanford.edu/hv220sb1684. Map political location: Marin County, California Compilation scale: 1:24,000 Base maps used are hillshades generated from IfSAR, LiDAR, and multibeam mapping both onshore and offshore (see Bathymetry Hillshade--Offshore Bolinas, California, DS 781, for more information). References Cited Bolt, B.A., 1968, The focus of the 1906 California earthquake: Bulletin of the Seismological Society of America, v. 58, p. 457-471. Bruns, T.R., Cooper, A.K., Carlson, P.R., and McCulloch, D.S., 2002, Structure of the submerged San Andreas and San Gregorio fault zones in the Gulf of Farallones as inferred from high-resolution seismic-reflection data, in Parsons, T. (ed.), Crustal structure of the coastal and marine San Francisco Bay region, California: U.S. Geological Survey Professional Paper 1658, p. 77-117. Lomax, A., 2005, A reanalysis of the hypocentral location and related observations for the Great 1906 California earthquake: Bulletin of the Seismological Society of America, v. 95, p. 861-877. Ryan, H.F., Parsons, T., and Sliter, R.W., 2008. Vertical tectonic deformation associated with the San Andreas fault zone offshore of San Francisco, California. Tectonphysics, 429 (1-2), p. 209-224. U.S. Geological Survey and California Geological Survey, 2010, Quaternary fault and fold database for the United States, accessed April 5, 2012, from USGS website: http://earthquake.usgs.gov/hazards/qfaults/. This layer is presented in the WGS84 coordinate system for web display purposes. Downloadable data are provided in native coordinate system or projection.

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  20. Title: Geology: Offshore of Pacifica, California, 2010

    Contributors:

    Summary: This polygon shapefile depictss geologic features in the offshore area of Pacifica, California. The continental shelf within California's State waters in the Pacifica area is shallow (water depths of 0 to about 40 m) and flat continental shelf with a very gentle (less than 0.5 degrees) offshore dip. The morphology and geology of this shelf result from the interplay between local tectonics, sea-level rise, sedimentary processes, and oceanography. Tectonic influences are related to local faulting and uplift (see below). Sea level has risen about 125 to 130 m over the last about 21,000 years (for example, Lambeck and Chappel, 2001; Gornitz, 2009), leading to progressive eastward migration (a few tens of km) of the shoreline and wave-cut platform, and associated transgressive erosion and deposition (for example, Catuneanu, 2006). The Offshore of Pacifica map area is now mainly an open shelf that is subjected to full, and sometimes severe, Pacific Ocean wave energy and strong currents. Most of the offshore map area is covered by marine sediments; artificial fill (unit af) occurs only at the site of the Pacifica Pier. Given their relatively shallow depths and exposure to high wave energy, modern shelf deposits are mostly sand (unit Qms). More coarse-grained sands and gravels (units Qmss and Qmsc) are primarily recognized on the basis of bathymetry and high backscatter (Bathymetry--Offshore of Pacifica map area, California, and Backscatter--Offshore of Pacifica map area, California). Unit Qmsc occurs as nearshore bars (less than 12 m water depth) for about two kilometers north of Mussel Rock and more locally offshore Pacifica, and in two isolated patches farther offshore at about 25 m water depth. Unit Qmss forms erosional lags in features known as ârippled scour depressionsâ (for example, Cacchione and others, 1984) or âsorted bedformsâ (for example, Trembanis and Hume, 2011), at water depths of about 15 to 25 m, in contact with offshore bedrock uplifts and unit Qms. Such features are common along this stretch of the California coast where offshore sandy sediment can be relatively thin (thus unable to fill the depressions) due to both lack of sediment supply from rivers and to significant sediment erosion and offshore transport during large winter storms. Although the general areas in which both unit Qmss scour depressions and unit Qmsc bars occur are not likely to change substantially, the boundaries of the unit(s) are likely ephemeral, changing seasonally and during significant storm events. Areas where shelf sediments form thin (less than 2 m) veneers over low relief bedrock of the Franciscan Complex (see below) occur in the northern half of the map and are mapped as unit Qms/KJf. This hybrid unit is recognized and delineated based on the combination of flat relief, continuity with moderate to high relief onshore or offshore bedrock outcrops, high-resolution seismic-reflection data, and in some cases moderate to high backscatter. The thin sediment layer is regarded as ephemeral and dynamic, and may or may not be present at a specific location based on storms, seasonal to annual patterns of sediment movement, or longer-term climate cycles. In a nearby, similarly high-energy setting, Storlazzi and others (2011) have described seasonal burial and exhumation of submerged bedrock in northern Monterey Bay. Offshore bedrock exposed at the seafloor is mapped as Jurassic and Cretaceous Franciscan Complex, undivided (unit KJf); Cretaceous granite (unit Kgr); Tertiary and (or) Cretaceous rock, undivided (unit TKu); unnamed sansdstone, shale and conglomerate of Paleocene age (unit Tss); and the Upper Miocene and Pliocene Purisima Formation (unit Tp). These units are delineated by extending outcrops and trends from mapped onshore geology and from their distinctive surface textures as revealed by high-resolution bathymetry (Bathymetry--Offshore of Pacifica map area, California). Purisima Formation outcrops in the southernmost part of the offshore map area form distinctive "ribs," caused by differential erosion of variably resistant, interbedded lithologies (for example, sandstone and mudstone). In contrast, granitic rocks have a densely cross-fractured, rough surface texture, and both the Franciscan Complex and the unnamed Paleocene sedimentary unit have a more masssive, irregular, and smoother surface texture. Purisima Formation outcrops occur in water as deep as 35 m, whereas other bedrock units occur in shallower (less than 20 m) water depths, most commonly adjacent to coastal points underlain by bedrock (for example, Pedro Point and Montara Point). Map unit polygons were digitized over underlying 2-meter base layers developed from multibeam bathymetry and backscatter data. The bathymetry and backscatter data were collected between 2006 and 2010. A map which shows these data is published in Scientific Investigations Map 3302, "California State Waters Map Series--Offshore of Coal Oil Point, California." This layer is part of USGS Data Series 781. In 2007, the California Ocean Protection Council initiated the California Seafloor Mapping Program (CSMP) to create a comprehensive seafloor map of high-resolution bathymetry, marine benthic habitats and geology within the 3-nautical-mile limit of California's State Waters. CSMP has divided coastal California into 110 map blocks, each to be published individually as United States Geological Survey Open-File Reports (OFRs) or Scientific Investigations Maps (SIMs) at a scale of 1:24,000. Maps display seafloor morphology and character, identify potential marine benthic habitats and illustrate both the seafloor geology and shallow (to about 100 m) subsurface geology. Data layers for bathymetry, bathymetric contours, acoustic backscatter, seafloor character, potential benthic habitat and offshore geology were created for each map block, as well as regional-scale data layers for sediment thickness, depth to transition, transgressive contours, isopachs, predicted distributions of benthic macro-invertebrates and visual observations of benthic habitat from video cruises over the entire state. These data are intended for science researchers, students, policy makers, and the general public. This information is not intended for navigational purposes.The data can be used with geographic information systems (GIS) software to display geologic and oceanographic information. Additionally, this coverage can provide a geologic map for the public and geoscience community to aid in assessments and mitigation of geologic hazards in the coastal region and sufficient geologic information for land-use and land-management decisions both onshore and offshore. This information is not intended for navigational purposes. Greene, H.G., Hartwell, S.R., Manson, M.W., Johnson, S.Y., Dieter, B.E., Phillips, E.L., and Watt, J.T. (2014). Geology: Offshore of Pacifica, California, 2010. California State Waters Map Series Data Catalog: U.S. Geological Survey Data Series 781. Available at: http://purl.stanford.edu/zg982fx5597. Map political location: San Mateo County, California Compilation scale: 1:24,000 Base maps used are hillshades generated from IfSAR, LiDAR, and multibeam mapping both onshore and offshore (Bathymetry--Offshore of Pacifica map area, California, DS 781, for more information). References Cited Cacchione, D.A., Drake, D.E., Grant, W.D., and Tate, G.B., 1984. Rippled scour depressions of the inner continental shelf off central California: Journal of Sedimentary Petrology, v 54, p. 1280-1291. Catuneanu, O., 2006, Principles of Sequence Stratigraphy: Amsterdam, Elsevier, 375 p. Gornitz, V., 2009, Sea level change, post-glacial, in Gornitz, V., ed., Encyclopedia of Paleoclimatology and Ancient Environments: Encyclopedia of Earth Sciences Series. Springer, pp. 887-893. Lambeck, K., and Chappell, J., 2001, Sea level change through the last glacial cycle: Science, v. 292, p. 679-686. Trembanis, A.C., and Hume, T.M., 2011, Sorted bedforms on the inner shelf off northeastern New Zealand: spatiotemporal relationships and potential paleo-evironmental implications: Geo-Marine Letters, v. 31, p. 203-214. This layer is presented in the WGS84 coordinate system for web display purposes. Downloadable data are provided in native coordinate system or projection.

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