20090205 13380800 FALSE 20090115 12255000 20090205 10044700 {FB0CC897-BBDD-4B12-A8AD-A6E9D44F9891} Microsoft Windows XP Version 5.1 (Build 2600) Service Pack 2; ESRI ArcCatalog 9.2.6.1500 en The Earth's bedrock is overlain in many places by a loosely compacted and mostly unconsolidated blanket of sediments in which soils commonly are developed. These sediments generally were eroded from underlying rock, and then were transported and deposited. In places, they exceed 1000 ft (330 m) in thickness. Where the sediment blanket is absent, bedrock is either exposed or has been weathered to produce a residual soil. For the conterminous United States, a map by Soller and Reheis (2004, scale 1:5,000,000; http://pubs.usgs.gov/of/2003/of03-275/) shows these sediments and the weathered, residual material; for ease of discussion, these are referred to as "surficial materials." That map was produced as a PDF file, from an Adobe Illustrator-formatted version of the provisional GIS database. The provisional GIS files were further processed without modifying the content of the published map, and are here published. A detailed understanding of the Earth's blanket of sediment and weathered bedrock is critical to our society, because nearly all human activities occur on or within these materials. Homeowners, communities, and governments can make improved decisions about hazard, resource, and environmental issues, when they understand the nature of surficial materials and how they vary from place to place. For example, are the surficial materials upon which a home is built stable enough to resist subsidence or lateral movement during an earthquake? Do these materials support a ground water resource adequate for new homes? Can they adequately filter contaminants and protect buried aquifers both in underlying sediments and in bedrock? Are they suitable for development of a new wetland? Where can we find materials suitable for aggregate? The USGS National Cooperative Geologic Mapping Program (NCGMP) works with the State geological surveys to identify priority areas for mapping of surficial materials (for example, in areas of complex and poorly understood deposits of various sediment types, where metropolitan areas are experiencing rapid growth). To help establish these priorities, a quickly prepared, modern, synoptic overview of the geology was needed. The Soller and Reheis (2004) map was made in response to that need, and provides an overview of current knowledge of the composition and distribution of surficial materials in the conterminous United States (the map covers only the conterminous U.S. because similar geologic information in digital form was not readily available for Alaska and Hawaii). Before its publication, the best available map had been a highly generalized depiction at 1:7,500,000-scale (about 120 miles to the inch), prepared for the USGS National Atlas (Hunt, C.B., 1979, Surficial geology of the conterminous United States: U.S. Geological Survey, National Atlas of the United States of America, scale 1:7,500,000). The Soller and Reheis map was compiled at a slightly more detailed scale (about 80 miles to the inch) than Hunt's map, and used digital methods, which enabled rapid incorporation of the variety of available source maps. State-scale geologic maps from the western United States were brought directly into the map, without expending the time needed to resolve interpretive differences among them. Therefore, abrupt changes in surficial materials are indicated along many State boundaries. This of course is an artifact of the compilation technique, and a limitation on its utility. However, this approach supports the basic premise of the map -- to provide an overview of surficial materials, and to identify areas where additional work may be needed in order to resolve scientific issues that can, in turn, lead to improved mapping. The map also serves to illustrate for educational and planning purposes the general nature and distribution of the Nation's surficial materials at land surface, but does not offer information useful for local decisions because it is not intended to be used at a larger (greater detail) scale than 1:5,000,000. Users who wish to display the geologic map symbolization and color palettes similar to those used in the published version of the map (Soller and Reheis, 2004) are encouraged to open the map document (Surficial_Mtls_US.mxd) included in the data package. Many of the processes that create surficial materials (especially those involving wind or mass movement of materials) tend to vary over small distances, and so the delineation of map areas large enough to be visible at the scale of this map (1 inch on the map equals about 80 miles on the ground) is highly problematic. To improve map legibility and comprehension, a classification system was required that assigned the many complex units on source maps into units much more broadly and simply defined. In some cases, units on source maps could not be readily assigned to our classification. As an example, a geologic unit found mostly in the southeastern U.S. is a residual material that developed mostly in metamorphosed sedimentary rocks and, to a lesser extent, in sedimentary rocks. Rather than define a new map unit, we decided to classify it as "Residual materials developed in sedimentary rocks" to distinguish it from "Residual materials formed in igneous and metamorphic rocks". As another example, the source map for New York and New Jersey classified a unit as "Ice-contact deposits and glacial lake deposits -- A complex of ice-contact sand and gravel and glacial lake sediments." This unit could not readily be assigned in our classification to either a coarse- or a fine-grained unit. Therefore, we decided to assign it to a genetically-related unit, glacial till, whose texture ranges from coarse to fine. This decision certainly is imperfect, and illustrates the difficulties in reinterpreting source map information. A further challenge is presented where map units from different source maps abut. When compiling a map from numerous published sources, many instances occur where, especially along the edges of adjoining source maps, the materials are described and mapped in different ways. Normally, these inconsistencies can be resolved by additional field mapping or through discussions with the geologists who created the source maps, and this is an especially effective approach when mapping at a relatively detailed scale. Lacking such avenues for resolution, units shown on adjacent source maps could not always be reconciled. Therefore, this map shows numerous instances where different map units meet along straight lines, commonly at state or latitude boundaries. For example, in North Dakota, a map unit extends westward where it seems to correspond to a unit from the adjacent source map. However, on that adjacent map, the surficial materials were not shown; there, it must be assumed that the bedrock is exposed and has been weathered to produce residual materials. The residual materials that are inferred from that map are classified differently than the materials described on the map to the east, hence there appears to be a sharp discontinuity in surficial materials. Because this map is an overview, essentially a "snapshot" of current knowledge that can be represented at a national scale, these inconsistencies are retained to indicate what is actually known about the materials, and to indicate where additional mapping may be beneficial. Regarding the thickness of these surficial materials, scant information at a regional or national scale is available, except within the glaciated area. In most places, this is not a significant problem because these materials generally fall within our lower thickness category (<100 ft). However, for large expanses of alluvial and lacustrine materials (for example, in the Mississippi River Valley, the Platte River Valley, and in internally drained valleys of the western United States), thicknesses may exceed 100 ft, even where not so indicated on the map. In most places, especially in areas not covered by glacially-deposited sediment, the uppermost material generally constitutes most (and in places, all) of the total thickness of sediment overlying bedrock. However, where sediment is shown exceeding 100 feet in thickness, the surficial material mapped at land surface does not necessarily extend downward to bedrock. In many places the uppermost material may be only a few feet thick, but the total thickness of sediment overlying bedrock is much greater. This is especially common in the glaciated area where the peat or loess shown on the map is only a thin veneer that overlies a complex package of other surficial materials which, in places, exceeds 1000 ft in thickness. Please refer to the "Description of Map Units" section for further information. Soller, D.R. 2009 Surficial_materials vector digital data http://pubs.usgs.gov/ds/425 Reheis, M.C. Garrity, C.P. Van Sistine, D.R. Unknown 1.0 publication date 2009115 unknown Complete As needed -127.884613 -65.342960 51.606043 22.941934 -2355930.492200 2258477.249400 277057.046200 3172633.833800 ISO 19115 Topic Category Geoscientific Information Geology Surficial materials United States North America Alabama Alaska Arizona Arkansas California Colorado Connecticut Delaware District of Columbia Florida Georgia Hawaii Idaho Illinois Indiana Iowa Kansas Kentucky Louisiana Maine Maryland Massachusetts Michigan Minnesota Mississippi Missouri Montana Nebraska Nevada New Hampshire New Jersey New Mexico New York North Carolina North Dakota Ohio Oklahoma Oregon Pennsylvania Rhode Island South Carolina South Dakota Tennessee Texas Utah Vermont Virginia Washington West Virginia Wisconsin Wyoming None None This digital publication was prepared by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, make any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report, or represents that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. Any views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. Although all data published in this Data Series have been used by the USGS, no warranty, expressed or implied, is made by the U.S. Geological Survey as to the accuracy of the data and related materials and/or the functioning of the software. The act of distribution shall not constitute any such warranty, and no responsibility is assumed by the USGS in the use of this data, software, or related materials. Graphical map depictions are intended to be used within the map scale limits applicable to the source data. Although software enables the user to view data at various scales, the user is cautioned to refer to the source documentation for the appropriate map scale limitations. File Geodatabase Feature Class David Soller U.S. Geological Survey Project Chief physical address

MS 926-A National Center

Reston VA 20192 USA 703-648-6907 703-648-6907 703-648-6977 drsoller@usgs.gov 9:00AM - 6:00PM Preferred contact method is electronic mail. Soller, D.R. Reheis, M.C. 2004 Unknown 1.0 map Open File Report 03-275 Reston, VA U.S. Geological Survey http://pubs.usgs.gov/of/2003/of03-275/ None Unclassified None Microsoft Windows XP Version 5.1 (Build 2600) Service Pack 2; ESRI ArcCatalog 9.2.6.1500 Surficial_materials -2355930.4922 2258477.2494 3172633.8338 277057.0462 1 -127.884613 -65.34296 51.606043 22.941934 1 en FGDC Content Standards for Digital Geospatial Metadata FGDC-STD-001-1998 local time http://www.esri.com/metadata/esriprof80.html ESRI Metadata Profile Christopher Garrity U.S. Geological Survey mailing address Reston VA 20192

12201 Sunrise Valley Drive

Mail Stop 956

USA Cartographer 703-648-6426 703-648-6426 703-648-6419 cgarrity@usgs.gov 9:00 AM - 6:00 PM Electronic mail is preferred method of contact 20090205 ISO 19115 Geographic Information - Metadata DIS_ESRI1.0 dataset U.S. Geological Survey Data Series, Report Number 425, 2009 mailing and physical address

Box 25286

Denver CO 80225 USA 1-888-ASK-USGS 1-888-ASK-USGS 303-202-4693 http://store.usgs.gov/ USGS Information Services This digital publication was prepared by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, make any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report, or represents that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. Any views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. Although all data published in this Data Series have been used by the USGS, no warranty, expressed or implied, is made by the U.S. Geological Survey as to the accuracy of the data and related materials and/or the functioning of the software. The act of distribution shall not constitute any such warranty, and no responsibility is assumed by the USGS in the use of this data, software, or related materials. Graphical map depictions are intended to be used within the map scale limits applicable to the source data. Although software enables the user to view data at various scales, the user is cautioned to refer to the source documentation for the appropriate map scale limitations. For those who wish to order this publication on Compact Disc, call 1-888-ASK-USGS (1-888-275-8747), visit http://ask.usgs.gov, contact any USGS Earth Science Information Center (ESIC), or write: USGS Information Services Box 25286 Denver, CO 80225 ArcGIS Desktop 9.X is required to open the map document (Surf_Mtls_US.mxd). GDB 9.2 ESRI File Geodatabase Polygon, line, and point feature classes File Geodatabase compression (uncompress with ArCatalog) 100 MB 100 MB http://pubs.usgs.gov/ds/425 None http://pubs.usgs.gov/ds/425 N/A 002 file:// Local Area Network File Geodatabase Feature Class Vector Simple Polygon FALSE 23893 TRUE FALSE G-polygon 23893 GCS_Clarke_1866 Clarke_1866_Albers Albers Conical Equal Area 29.500000 45.500000 -96.000000 23.000000 0.000000 0.000000 coordinate pair meters 0.000100 0.000100 D_Clarke_1866 Clarke 1866 6378206.400000 294.978698 Explicit elevation coordinate included with horizontal coordinates 0.000100 Clarke_1866_Albers 23893 Surficial_materials Feature Class 23893 Geologic unit polygons. Units are defined on the basis of composition, age, and origin. Soller, D.R., and Reheis, M.C. (2004) OBJECTID OBJECTID OID 4 0 0 Internal feature number. ESRI Sequential unique whole numbers that are automatically generated. Shape Shape Geometry 0 0 0 Feature geometry. ESRI Coordinates defining the features. UNIT_CODE UNIT_CODE Integer 4 0 0 Geologic unit code, composed of two to three digits that are systematically assigned. Used for map symbolization and as a quick indicator of the material's characteristics. Soller, D.R., and Reheis, M.C., (2004) The code's rightmost digit refers to the map unit's thickness, whereas as the other digits refer to the map unit's genesis and texture. UNIT_NAME UNIT_NAME String 80 0 0 Alluvial sediments, thick Clay- to gravel-sized sediment, with minor coarser materials, generally moderate- to well-bedded, deposited by perennial and intermittent streams and rivers and by sheetwash flow on uplands. Locally includes associated lake and estuarine sediments. Along perennial streams and rivers, relatively well-sorted sediment underlies floodplains, natural levees, and alluvial terraces that parallel modern or former drainage courses. Alluvial sediments within the glaciated area commonly overlie or are mixed with sediment deposited by water that flowed from the glaciers (see "Glaciofluvial ice-contact sediments", below). On steeper slopes and especially in the arid western U.S., relatively poorly sorted sediment (including debris-flow and debris-avalanche material) underlies alluvial fans and fan piedmonts deposited by intermittent streams. In many places, notably in the Mississippi River Valley, in the glaciated area, on the uplands near the Platte River in Nebraska, and in fault-bounded valleys of the western U.S., these sediments may greatly exceed 100 ft in thickness. Soller, D.R., and Reheis, M.C., (2004). Name of geologic map unit, as shown on map, or as compiled by reading the map unit description (and parent map unit description, if any). Soller, D.R., and Reheis, M.C., (2004) Alluvial sediments, thin Clay- to gravel-sized sediment, with minor coarser materials, generally moderate- to well-bedded, deposited by perennial and intermittent streams and rivers and by sheetwash flow on uplands. Locally includes associated lake and estuarine sediments. Along perennial streams and rivers, relatively well-sorted sediment underlies floodplains, natural levees, and alluvial terraces that parallel modern or former drainage courses. Alluvial sediments within the glaciated area commonly overlie or are mixed with sediment deposited by water that flowed from the glaciers (see "Glaciofluvial ice-contact sediments", below). On steeper slopes and especially in the arid western U.S., relatively poorly sorted sediment (including debris-flow and debris-avalanche material) underlies alluvial fans and fan piedmonts deposited by intermittent streams. These materials generally form a continuous cover less than 100 feet thick. Soller, D.R., and Reheis, M.C., (2004). Basaltic and andesitic volcanic rocks Ranges from generally coarse-grained sediment to rocks, formed by volcanic eruptions. Includes dominantly volcanic sediment reworked from original depositional setting by fluvial processes. Character is largely dependent on magma composition: andesitic eruptions along the western plate boundary produce large stratovolcanoes, and basaltic eruptions produce cinder cones and sheet-like flows. Generally between 10 and 100 ft (3 and 30m) thick, except in stratovolcanoes and in the Snake River Plain region (southern Idaho), where stacked basalt flows may be hundreds of feet thick. Modified from Soller, D.R., and Reheis, M.C., (2004). Calcareous biological sediments Calcareous materials such as algal mats, marl, oolitic and coralline limestone, and shelly sand, deposited in beach and nearshore environments. These sediments, and any underlying sediments, are generally less than 100 ft thick, forming a continuous cover on underlying rocks. Mapped mostly in South Florida. Soller, D.R., and Reheis, M.C., (2004). Coastal zone sediments, mostly fine-grained Generally fine-grained sediment deposited in lagoons, tidal flats, backbarriers, and coastal marshes. Deposited along the coastal margins of the Atlantic, Gulf of Mexico, and Pacific. Mapped according to sediment texture and environment. These sediments, and any underlying sediments, are generally less than 100 feet thick, forming a continuous cover on underlying rocks (except on Long Island, where the sediments are considerably thicker). Soller, D.R., and Reheis, M.C., (2004). Coastal zone sediments, mostly medium-grained Generally medium-grained sediment deposited on beaches and dunes, and in shallow marine and related alluvial environments. Deposited along the coastal margins of the Atlantic, Gulf of Mexico, and Pacific. Mapped according to sediment texture and environment. These sediments, and any underlying sediments, are generally less than 100 ft thick, forming a continuous cover on underlying rocks (except on Long Island, where the sediments are considerably thicker). Soller, D.R., and Reheis, M.C., (2004). Colluvial and alluvial sediments Poorly sorted and stratified sediment ranging from clay to boulders in size; may contain organic material. Formed by weathering and breakdown of underlying rock in areas of steep to moderate slopes. The weathered and broken material has undergone some downslope transport and has been deposited as colluvium, landslides, talus, and rock avalanches. In places, this map unit includes the following: alluvial sediments; residual materials; especially on lower slopes; and fine-grained eolian sediments (loess) overlying the colluvium. These sediments generally are patchy in distribution, especially on steeper slopes where rock can be found exposed amongst these sediments. However, in many areas they do form a continuous cover and, locally in some debris flows and slope failures, they exceed 100 feet in thickness. Soller, D.R., and Reheis, M.C., (2004). Colluvial sediments and loess Poorly sorted and stratified sediment ranging from clay to boulders in size; may contain organic material. Formed by weathering and breakdown of underlying rock in areas of steep to moderate slopes. The weathered and broken material has undergone some downslope transport and has been deposited as colluvium, landslides, talus, and rock avalanches. In places, this map unit includes the following: fine-grained eolian sediments (loess) overlying the colluvium; residual materials, especially on lower slopes; and alluvial sediments. These sediments generally are patchy in distribution, especially on steeper slopes where rock can be found exposed amongst these sediments. However, in many areas they do form a continuous cover and, locally in some debris flows and slope failures, they exceed 100 feet in thickness. Soller, D.R., and Reheis, M.C., (2004). Colluvial sediments and residual material Poorly sorted and stratified sediment ranging from clay to boulders in size; may contain organic material. Formed by weathering and breakdown of underlying rock in areas of steep to moderate slopes. The weathered and broken material has undergone some downslope transport and has been deposited as colluvium, landslides, talus, and rock avalanches. In places, this map unit includes the following: residual materials, especially on lower slopes; alluvial sediments; and fine-grained eolian sediments (loess) overlying the colluvium. These sediments generally are patchy in distribution, especially on steeper slopes where rock can be found exposed amongst these sediments. However, in many areas they do form a continuous cover and, locally in some debris flows and slope failures, they exceed 100 feet in thickness. Soller, D.R., and Reheis, M.C., (2004). Colluvial sediments, discontinuous Poorly sorted and stratified sediment ranging from clay to boulders in size; may contain organic material. Formed by weathering and breakdown of underlying rock in areas of steep to moderate slopes. The weathered and broken material has undergone some downslope transport and has been deposited as colluvium, landslides, talus, and rock avalanches. In places, this map unit includes the following: residual materials, especially on lower slopes; alluvial sediments; and fine-grained eolian sediments (loess) overlying the colluvium. These sediments generally are patchy in distribution, especially on steeper slopes where rock can be found exposed amongst these sediments. However, in some areas they do form a continuous cover and, locally in some debris flows and slope failures, they exceed 100 feet in thickness. Soller, D.R., and Reheis, M.C., (2004). Colluvial sediments, thin Poorly sorted and stratified sediment ranging from clay to boulders in size; may contain organic material. Formed by weathering and breakdown of underlying rock in areas of steep to moderate slopes. The weathered and broken material has undergone some downslope transport and has been deposited as colluvium, landslides, talus, and rock avalanches. In places, this map unit includes the following: residual materials, especially on lower slopes; alluvial sediments; and fine-grained eolian sediments (loess) overlying the colluvium. In the eastern U.S., the unit has been subdivided to indicate where these other constituents occur. These sediments generally are patchy in distribution, especially on steeper slopes where rock can be found exposed amongst these sediments. However, in many areas they do form a continuous cover and, locally in some debris flows and slope failures, they exceed 100 feet in thickness. Soller, D.R., and Reheis, M.C., (2004). Eolian sediments on southern High Plains Silt- and sand-sized sediment deposited by wind. On Southern High Plains in Texas and Oklahoma, the eolian sediments are somewhat different in texture and origin from typical dune sands or loess, forming a complex silty to sandy sediment. In general, the eolian sediments are more sandy in the west or southwest and more silty and clayey in the east or northeast. Soller, D.R., and Reheis, M.C., (2004). Eolian sediments, mostly dune sand, thick Sand-sized sediment deposited by wind. These sediments, and any underlying sediments, are generally more than 100 feet thick, forming a continuous cover on underlying rocks. Notably thick in the Nebraska Sand Hills. Soller, D.R., and Reheis, M.C., (2004). Eolian sediments, mostly dune sand, thin Sand-sized sediment deposited by wind. These sediments, and any underlying sediments, are generally less than 100 feet thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Eolian sediments, mostly loess, thick Mostly loess (a silty material deposited by winds near the glacial margin). Includes minor areas of alluvium and colluvium. These sediments, and any underlying sediments, are generally more than 100 feet thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Eolian sediments, mostly loess, thin Mostly loess (a silty material deposited by winds near the glacial margin). Includes minor areas of alluvium and colluvium. Loess forms a thin cover over much of the central United States, but is shown on this map only where it is thicker than 20 ft. Maximum thickness of loess and any underlying sediment in this map unit is 100 feet. Soller, D.R., and Reheis, M.C., (2004). Glacial till sediments, mostly clayey, discontinuous Glacial till is unsorted material ranging in grain size from clay to boulders, deposited by glacial ice; sediment in this unit is dominantly clayey. Includes minor areas of ice-contact and lake sediment. Patchy in distribution; bedrock commonly is exposed at land surface. Soller, D.R., and Reheis, M.C., (2004). Glacial till sediments, mostly clayey, thick Glacial till is unsorted material ranging in grain size from clay to boulders, deposited by glacial ice; sediment in this unit is dominantly clayey. Includes minor areas of ice-contact and lake sediment. These sediments, and any underlying sediments, are generally more than 100 feet thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Glacial till sediments, mostly clayey, thin Glacial till is unsorted material ranging in grain size from clay to boulders, deposited by glacial ice; sediment in this unit is dominantly clayey. Includes minor areas of ice-contact and lake sediment. These sediments, and any underlying sediments, are generally less than 100 feet thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Glacial till sediments, mostly sandy, discontinuous Glacial till is unsorted material ranging in grain size from clay to boulders, deposited by glacial ice; sediment in this unit is dominantly sandy. Includes minor areas of ice-contact and lake sediment. Patchy in distribution; bedrock commonly is exposed at land surface. Soller, D.R., and Reheis, M.C., (2004). Glacial till sediments, mostly sandy, thin Glacial till is unsorted material ranging in grain size from clay to boulders, deposited by glacial ice; sediment in this unit is dominantly sandy. Includes minor areas of ice-contact and lake sediment. These sediments, and any underlying sediments, are generally less than 100 feet thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Glacial till sediments, mostly silty, discontinuous Glacial till is unsorted material ranging in grain size from clay to boulders, deposited by glacial ice; sediment in this unit is dominantly silty or loamy. Includes minor areas of ice-contact and lake sediment. Patchy in distribution; bedrock commonly is exposed at land surface. Soller, D.R., and Reheis, M.C., (2004). Glacial till sediments, mostly silty, thick Glacial till is unsorted material ranging in grain size from clay to boulders, deposited by glacial ice; sediment in this unit is dominantly silty or loamy. Includes minor areas of ice-contact and lake sediment. These sediments, and any underlying sediments, are generally more than 100 feet thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Glacial till sediments, mostly silty, thin Glacial till is unsorted material ranging in grain size from clay to boulders, deposited by glacial ice; sediment in this unit is dominantly silty or loamy. Includes minor areas of ice-contact and lake sediment. These sediments, and any underlying sediments, are generally less than 100 feet thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Glaciofluvial ice-contact sediments, mostly sand and gravel, discontinuous Mostly sand and gravel with lesser silt, deposited by running water essentially in contact with glacial ice. Includes sediment deposited into water bodies adjacent to the glacial ice margin. Patchy in distribution; bedrock commonly is exposed at land surface. Mapped as small areas within the glaciated region in the eastern U.S., notably in eastern Massachusetts. Soller, D.R., and Reheis, M.C., (2004). Glaciofluvial ice-contact sediments, mostly sand and gravel, thick Mostly sand and gravel with lesser silt, deposited by running water essentially in contact with glacial ice. Includes sediment deposited into water bodies adjacent to the glacial ice margin. These sediments, and any underlying sediments, are generally more than 100 feet thick, forming a continuous cover on underlying rocks. Mapped as small areas within the glaciated region in the eastern U.S., notably in eastern Massachusetts. Soller, D.R., and Reheis, M.C., (2004). Glaciofluvial ice-contact sediments, mostly sand and gravel, thin Mostly sand and gravel with lesser silt, deposited by running water essentially in contact with glacial ice. Includes sediment deposited into water bodies adjacent to the glacial ice margin. These sediments, and any underlying sediments, are generally less than 100 feet thick, forming a continuous cover on underlying rocks. Mapped as small areas within the glaciated region in the eastern U.S., notably in eastern Massachusetts. Soller, D.R., and Reheis, M.C., (2004). Lacustrine sediments Generally well sorted and well bedded material ranging in grain size from clay to coarse gravel, deposited in perennial to intermittent lakes commonly in undrained valleys of the Great Basin. Because these lakes mostly are a response to lower evaporation and increased precipitation rather than to the melting of glaciers, much of the sediment is derived from stream erosion. Locally includes material deposited in playas, mudflats, salt flats, and adjacent saline marshes. Generally interbedded with playa sediment deposited during drier climatic periods; commonly intertongues upslope with sediment deposited by alluvial fans. These sediments, and any underlying sediments, commonly form a continuous cover less than 100 feet thick along valley margins, and may exceed several hundred feet in thickness in long-lived sedimentary basins. Soller, D.R., and Reheis, M.C., (2004). Organic-rich muck and peat, thick Organic-rich muck and peat deposited in poorly drained and swampy areas. These sediments, and any underlying sediments, are generally more than 100 ft thick, forming a continuous cover on underlying rocks. This map unit occurs in the glaciated region, and much of the unit thickness is composed of the underlying glacially-deposited sediment. Soller, D.R., and Reheis, M.C., (2004). Organic-rich muck and peat, thin Organic-rich muck and peat deposited in poorly drained and swampy areas. These sediments, and any underlying sediments, are generally less than 100 ft thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Playa sediments Fine-grained sediment and evaporite salts deposited in ephemeral lakes in the centers of undrained basins. Includes material deposited in playas, mudflats, salt flats, and adjacent saline marshes. Generally interbedded with eolian sand and with lacustrine sediment deposited during wetter climatic periods; commonly intertongue upslope with sediment deposited by alluvial fans. These sediments, and any underlying sediments, commonly form a continuous cover less than 100 feet thick, and may exceed several hundred feet in thickness in long-lived sedimentary basins. Soller, D.R., and Reheis, M.C., (2004). Proglacial sediments, mostly coarse-grained, discontinuous Generally coarse-grained sediment mostly deposited in terraces, river floodplains, buried valleys, and as sheet deposits during intervals when glacial ice was melting. Common in glaciated region and the Pacific Northwest. In the northwest U.S., includes coarse-grained flood sediments from the breaching of glacial Lake Missoula. Includes fine-grained deposits, especially in slackwater areas. In places, interfingers with alluvial sediments. Patchy in distribution; bedrock commonly is exposed at land surface. Soller, D.R., and Reheis, M.C., (2004). Proglacial sediments, mostly coarse-grained, thick Generally fine-grained sediment melted from glaciers and deposited in lakes and marine environments. In the eastern U.S., these lakes are commonly small and related to ice and sediment damming of waters near the margin of the continental glaciers. In the western U.S., these lakes may be considerably larger (e.g., Lake Missoula in western Montana). Includes some areas of Glacial till and well-sorted glaciofluvial sediment. These sediments, and any underlying sediments, are generally more than 100 feet thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Proglacial sediments, mostly coarse-grained, thin Generally coarse-grained sediment mostly deposited in terraces, river floodplains, buried valleys, and as sheet deposits during intervals when glacial ice was melting. Common in glaciated region and the Pacific Northwest. In the northwest U.S., includes coarse-grained flood sediments from the breaching of glacial Lake Missoula. Includes fine-grained deposits, especially in slackwater areas. In places, interfingers with alluvial sediments. These sediments, and any underlying sediments, are generally less than 100 feet thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Proglacial sediments, mostly fine grained, discontinuous Generally fine-grained sediment melted from glaciers and deposited in lakes and marine environments. In the eastern U.S., these lakes are commonly small and related to ice and sediment damming of waters near the margin of the continental glaciers. In the western U.S., these lakes may be considerably larger (e.g., Lake Missoula in western Montana). Includes some areas of Glacial till and well-sorted glaciofluvial sediment. Patchy in distribution; bedrock commonly is exposed at land surface. Soller, D.R., and Reheis, M.C., (2004). Proglacial sediments, mostly fine grained, thick Proglacial sediments, mostly fine grained, thick Soller, D.R., and Reheis, M.C., (2004). Proglacial sediments, mostly fine grained, thin Generally fine-grained sediment melted from glaciers and deposited in lakes and marine environments. In the eastern U.S., these lakes are commonly small and related to ice and sediment damming of waters near the margin of the continental glaciers. In the western U.S., these lakes may be considerably larger (e.g., Lake Missoula in western Montana). Includes some areas of Glacial till and well-sorted glaciofluvial sediment. These sediments, and any underlying sediments, are generally less than 100 feet thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Residual materials developed in alluvial sediments These materials formed by the partial chemical dissolution and physical disintegration of alluvial sediments; they include the modern soil profile and extend downward to unweathered alluvial material. Depending on the composition of the source alluvium, these materials can be generally fine- to coarse-grained, and commonly are poorly sorted. Unlike mass-movement sediments (e.g., colluvium), these materials were not transported. In some areas this map unit includes alluvial and colluvial sediments. This material is generally less than 10 feet thick and, in many places, is patchy in distribution. Particularly in mountainous areas, exposed rock can more commonly be found than residual material. Mapped mostly on the Atlantic and Gulf coastal margins, adjacent to Coastal zone deposits. Soller, D.R., and Reheis, M.C., (2004). Residual materials developed in bedrock, discontinuous These materials formed by the partial chemical dissolution and physical disintegration of bedrock and, to a lesser extent, of colluvial sediments; they include the modern soil profile and extend downward to unweathered rock. Depending on the composition of the source rock or colluvium, these materials can be generally fine- to coarse-grained, and commonly are poorly sorted. Unlike mass-movement sediments (e.g., colluvium), these materials were not transported. This material is generally less than 10 feet thick, and is patchy in distribution. Particularly in mountainous areas, exposed rock can more commonly be found than residual material. Soller, D.R., and Reheis, M.C., (2004). Residual materials developed in bedrock, thin These materials formed by the partial chemical dissolution and physical disintegration of bedrock and, to a lesser extent, of colluvial sediments; they include the modern soil profile and extend downward to unweathered rock. Depending on the composition of the source rock or colluvium, these materials can be generally fine- to coarse-grained, and commonly are poorly sorted. Unlike mass-movement sediments (e.g., colluvium), these materials were not transported. This material is generally less than 10 feet thick and, in many places, is patchy in distribution. Particularly in mountainous areas, exposed rock can more commonly be found than residual material. Soller, D.R., and Reheis, M.C., (2004). Residual materials developed in bedrock, with alluvial sediments, discontinuous These materials formed by the partial chemical dissolution and physical disintegration of bedrock and, to a lesser extent, of sheetwash alluvial sediments; they include the modern soil profile and extend downward to unweathered rock. Depending on the composition of the source rock or alluvium, these materials can be generally fine- to coarse-grained, and commonly are poorly sorted. Unlike mass-movement sediments (e.g., colluvium), these materials were not transported. This material is generally less than 10 feet thick, and is patchy in distribution. Particularly in mountainous areas, exposed rock can more commonly be found than residual material. Soller, D.R., and Reheis, M.C., (2004). Residual materials developed in bedrock, with alluvial sediments, thin These materials formed by the partial chemical dissolution and physical disintegration of bedrock and, to a lesser extent, of sheetwash alluvial sediments; they include the modern soil profile and extend downward to unweathered rock. Depending on the composition of the source rock or alluvium, these materials can be generally fine- to coarse-grained, and commonly are poorly sorted. Unlike mass-movement sediments (e.g., colluvium), these materials were not transported. This material is generally less than 10 feet thick and, in many places, is patchy in distribution. Particularly in mountainous areas, exposed rock can more commonly be found than residual material. Soller, D.R., and Reheis, M.C., (2004). Residual materials developed in carbonate rocks, discontinuous These materials formed by the partial chemical dissolution and physical disintegration of limestone and other carbonate rocks; they include the modern soil profile and extend downward to unweathered rock. Depending on the composition of the source rock, these materials can be generally fine- to coarse-grained, and commonly are poorly sorted. Unlike mass-movement sediments (e.g., colluvium), these materials were not transported. This material is generally less than 10 feet thick, and is patchy in distribution. Particularly in mountainous areas, exposed rock can more commonly be found than residual material. Soller, D.R., and Reheis, M.C., (2004). Residual materials developed in carbonate rocks, thin These materials formed by the partial chemical dissolution and physical disintegration of limestone and other carbonate rocks; they include the modern soil profile and extend downward to unweathered rock. Depending on the composition of the source rock, these materials can be generally fine- to coarse-grained, and commonly are poorly sorted. Unlike mass-movement sediments (e.g., colluvium), these materials were not transported. This material is generally less than 10 feet thick and, in many places, is patchy in distribution. Particularly in mountainous areas, exposed rock can more commonly be found than residual material. Soller, D.R., and Reheis, M.C., (2004). Residual materials developed in fine-grained sedimentary rocks These materials formed by the partial chemical dissolution and physical disintegration of fine-grained sedimentary rocks (e.g., shale) that contain smectite (a clay mineral responsible for "swelling soil"); they include the modern soil profile and extend downward to unweathered rock. These materials are generally fine-grained, and commonly are poorly sorted. Unlike mass-movement sediments (e.g., colluvium), these materials were not transported. This material is generally less than 10 feet thick and, in many places, is patchy in distribution. Particularly in mountainous areas, exposed rock can more commonly be found than residual material. Soller, D.R., and Reheis, M.C., (2004). Residual materials developed in igneous and metamorphic rocks These materials formed by the partial chemical dissolution and physical disintegration of igneous and metamorphic rock; they include the modern soil profile and extend downward to unweathered rock. Depending on the composition of the source rock or colluvium, these materials can be generally fine- to coarse-grained, and commonly are poorly sorted. Unlike mass-movement sediments (e.g., colluvium), these materials were not transported. This material is generally less than 10 feet thick and, in many places, is patchy in distribution. Particularly in mountainous areas, exposed rock can more commonly be found than residual material. Soller, D.R., and Reheis, M.C., (2004). Residual materials developed in sedimentary rocks, discontinuous These materials formed by the partial chemical dissolution and physical disintegration of sedimentary rocks; they include the modern soil profile and extend downward to unweathered rock. Depending on the composition of the source rock, these materials can be generally fine- to coarse-grained, and commonly are poorly sorted. Unlike mass-movement sediments (e.g., colluvium), these materials were not transported. This material is generally less than 10 feet thick, and is patchy in distribution. Particularly in mountainous areas, exposed rock can more commonly be found than residual material. Soller, D.R., and Reheis, M.C., (2004). Residual materials developed in sedimentary rocks, thin These materials formed by the partial chemical dissolution and physical disintegration of sedimentary rocks; they include the modern soil profile and extend downward to unweathered rock. Depending on the composition of the source rock, these materials can be generally fine- to coarse-grained, and commonly are poorly sorted. Unlike mass-movement sediments (e.g., colluvium), these materials were not transported. This material is generally less than 10 feet thick and, in many places, is patchy in distribution. Particularly in mountainous areas, exposed rock can more commonly be found than residual material. Soller, D.R., and Reheis, M.C., (2004). Rhyolitic volcanic rocks Ranges from generally coarse-grained sediment to rocks, formed by volcanic eruptions. Includes dominantly volcanic sediment reworked from original depositional setting by fluvial processes. Eruptions produce domes and ash-flow rhyolite tuffs. Generally between 10 and 100 ft (3 and 30 m) thick. Modified from Soller, D.R., and Reheis, M.C., (2004). Water Water covers the surficial materials, which were not mapped owing to lack of readily-accessible (digital) information on their characteristics. Soller, D.R., and Reheis, M.C., (2004). UNIT_THICK UNIT_THICK String 40 0 0 Discontinuous The sediments shown in this map unit are patchy in distribution; bedrock commonly is exposed at land surface. Soller, D.R., and Reheis, M.C., (2004). Generalized thickness of the mapped unit. Soller, D.R., and Reheis, M.C., (2004). <100 The sediments shown in this map unit, and any underlying sediments, are generally less than 100 feet thick, forming a continuous cover on underlying rocks. Soller, D.R., and Reheis, M.C., (2004). Soller, D.R., and Reheis, M.C., (2004). >100 The sediments shown in this map unit, and any underlying sediments, are generally more than 100 feet thick, forming a continuous cover on underlying rocks. GEOL_AGE GEOL_AGE String 35 0 0 Holocene to late Pleistocene Deposition occurred sometime between the present day (which is included in the Holocene) and very approximately 122,000 years ago (the beginning of the late Pleistocene). This is the time range for all sediments in the map unit; the age of deposits at a specific location may be significantly more restricted in time. See Attribute_Definition_Source. The maximum span of geologic time during which geologic materials in the map unit were deposited. The deposits of any given area may be significantly restricted in age (i.e., less than this maximum span). By convention, the age range is specified as <younger age> to <older age>. Soller, D.R., and Reheis, M.C., (2004); U.S. Geological Survey, 2007, Divisions of Geologic Time - Major Chronostratigraphic and Geochronologic Units: U.S. Geological Survey Fact Sheet 2007-3015, 2 p., http://pubs.usgs.gov/fs/2007/3015/; Richmond, G.M., and Fullerton, D.S., 1986, Introduction to Quaternary glaciations in the United States of America, in V. Sibrava, D.Q. Bowen, and G.M. Richmond, Quaternary Glaciations in the Northern Hemisphere: New York, Pergamon Press, p. 3-10. Holocene to middle Pleistocene Deposition occurred sometime between the present day (which is included in the Holocene) and very approximately 790,000 years ago (the beginning of the middle Pleistocene). This is the time range for all sediments in the map unit; the age of deposits at a specific location may be significantly more restricted in time. See Attribute_Definition_Source. Holocene to Pleistocene Deposition occurred sometime between the present day (which is included in the Holocene) and approximately 1.8 million years ago (the beginning of the Pleistocene). This is the time range for all sediments in the map unit; the age of deposits at a specific location may be significantly more restricted in time. See Attribute_Definition_Source. Holocene to Pliocene Deposition occurred sometime between the present day (which is included in the Holocene) and approximately 5.3 million years ago (the beginning of the Pliocene). This is the time range for all sediments in the map unit; the age of deposits at a specific location may be significantly more restricted in time. See Attribute_Definition_Source. Holocene to Tertiary Deposition occurred sometime between the present day (which is included in the Holocene) and approximately 65.5 million years ago (the beginning of the Tertiary). This is the time range for all sediments in the map unit; the age of deposits at a specific location may be significantly more restricted in time. See Attribute_Definition_Source. late Wisconsinan to Illinoian Deposition occurred sometime between the end of the last glacial episode (late Wisconsinan, which ended about 11,000 years ago) and about 198,000 years ago (the beginning of the Illinoian glacial episode). This is the time range for all sediments in the map unit; the age of deposits at a specific location may be significantly more restricted in time. See Attribute_Definition_Source. late Wisconsinan to pre-Illinoian Deposition occurred sometime between the end of the last glacial episode (late Wisconsinan, which ended about 11,000 years ago) and the beginning of "pre-Illinoian" time (age uncertain, but roughly coinciding with the beginning of the Quaternary, 1.8 million years ago). This is the time range for all sediments in the map unit; the age of deposits at a specific location may be significantly more restricted in time. See Attribute_Definition_Source. MIN_AGE MIN_AGE String 20 0 0 Holocene The youngest formal subdivision of time, extending from the present to approximately 11,000 years ago. See Attribute_Definition_Source. Minimum (youngest) geologic age during which materials in the map unit were deposited. This is the minimum age for all sediments in the map unit; the deposits at a specific location may be significantly older. Soller, D.R., and Reheis, M.C., (2004); U.S. Geological Survey, 2007, Divisions of Geologic Time - Major Chronostratigraphic and Geochronologic Units: U.S. Geological Survey Fact Sheet 2007-3015, 2 p., http://pubs.usgs.gov/fs/2007/3015/; Richmond, G.M., and Fullerton, D.S., 1986, Introduction to Quaternary glaciations in the United States of America, in V. Sibrava, D.Q. Bowen, and G.M. Richmond, Quaternary Glaciations in the Northern Hemisphere: New York, Pergamon Press, p. 3-10. late Pleistocene An informal subdivision of time, extending from about 11,000 to 122,000 years ago. See Attribute_Definition_Source. MAX_AGE MAX_AGE String 20 0 0 early Pleistocene An informal subdivision of time, extending from about 788,000 to 1.8 million years ago. See Attribute_Definition_Source. Maximum (oldest) geologic age during which materials in the map unit were deposited. This is the maximum age for all sediments in the map unit; the deposits at a specific location may be significantly younger. Soller, D.R., and Reheis, M.C., (2004); U.S. Geological Survey, 2007, Divisions of Geologic Time - Major Chronostratigraphic and Geochronologic Units: U.S. Geological Survey Fact Sheet 2007-3015, 2 p., http://pubs.usgs.gov/fs/2007/3015/; Richmond, G.M., and Fullerton, D.S., 1986, Introduction to Quaternary glaciations in the United States of America, in V. Sibrava, D.Q. Bowen, and G.M. Richmond, Quaternary Glaciations in the Northern Hemisphere: New York, Pergamon Press, p. 3-10. late Pleistocene An informal subdivision of time, extending from about 11,000 to 122,000 years ago. See Attribute_Definition_Source. middle Pleistocene An informal subdivision of time, extending from about 122,000 to 788,000 years ago. See Attribute_Definition_Source. Pleistocene The first epoch of the Quaternary Period. It extended from about 11,000 to 1.8 million years ago. See Attribute_Definition_Source. Pliocene The last epoch of the Tertiary Period. It extended from about 1.8 to 5.3 million years ago. See Attribute_Definition_Source. Tertiary The first period of the Cenozoic Era. It extended from about 1.8 to 65.5 million years ago. See Attribute_Definition_Source. DMU_HIER DMU_HIER String 15 0 0 A set of unique arbitrary number sequences assigned, one to each of the geologic material types. The number sequence is essentially an outline format. When the number sequences are sorted in ascending order, the map units are arranged as in the hierarchical, ordered format shown on the source map's Description of Map Units. Soller, D.R., and Reheis, M.C., (2004). Arbitrary number sequences arranged in outline form (e.g., "001", "001-001", "001-002", "002", "003", etc.). Shape_Length Shape_Length Double 8 0 0 Length of feature in internal units. ESRI Positive real numbers that are automatically generated. Shape_Area Shape_Area Double 8 0 0 Area of feature in internal units squared. ESRI Positive real numbers that are automatically generated. 20090205 Soller, D.R. Reheis, M.C. 2004 Unknown 1.0 map http://pubs.usgs.gov/of/2003/of03-275/ Open File Report 03-275 Reston, VA U.S. Geological Survey 5,000,000 paper Soller, D.R., and Reheis, M.C., (2004) Hard copy of the Surficial Materials in the Conterminous United States. 2004 unknown publication date

12201 Sunrise Valley Drive

mailing and physical address

Mail Stop 956

Reston VA 20192 USA Christopher Garrity U.S. Geological Survey Cartographer 703-648-6426 703-648-6426 703-648-6419 cgarrity@usgs.gov 9:00AM - 6:00PM Preferred contact method is electronic mail. ArcInfo 9.2 20081201 Unknown Geologic maps and digital files that were used to create this map database are listed in the "References and Compilation Sources" section of the published map (Soller and Reheis, 2004; see http://pubs.usgs.gov/of/2003/of03-275/). David R. Soller (for the eastern States) and Marith C. Reheis (for the western States) compiled and generalized the map units from the source materials. Darren Van Sistine (for the western States) and David R. Soller (for the eastern States) performed the digital processing of map data for the published map, and Christopher P. Garrity performed the final processing for this database. The compilation of this map began with an inventory of available source maps. We used maps that met the following criteria: were statewide or larger in area; showed surficial materials at land surface (or could be interpreted to derive such information); and were Geographic Information System (GIS) files in ArcInfo (v.7) format. For the conterminous U.S. east of 102 degrees West Longitude, we principally used a 1:2,500,000-scale recompilation (Fullerton and others, written communication) of the "Quaternary Geologic Atlas of the United States" series (U.S. Geological Survey, Map I-1420, scale 1:1,000,000). That recompilation contained more than 150 different types of surficial materials. For the conterminous U.S. west of 102 degrees West Longitude, we principally used published statewide geologic maps, which mostly were at 1:500,000-scale. Those maps emphasized the bedrock geology, although they also showed some of the major unconsolidated units such as alluvium in major river valleys and large deposits of lake sediment. Significant interpretation therefore was required in order to identify the appropriate residual surficial material developed in each mapped bedrock unit. The disparity in information content among source maps argued for a broad classification with few units. We began with a simple classification based on that of the British Geological Survey (McMillan, A.A., and Powell, J.H., 1999, BGS Rock Classification Scheme, Volume 4, Classification of artificial (man-made) ground and natural superficial deposits -- applications to geological maps and datasets in the UK: British Geological Survey Research Report, RR 99-04, 65 p.). For the eastern source map (Fullerton and others, written communication), each of the 150 source map unit descriptions were interpreted and manually parsed into various attribute fields in a spreadsheet. Attributes included: unit name, dominant sediment texture, geologic age, environment of deposition, and thickness. After using these attributes to classify the map units, the map was displayed and evaluated and, iteratively, a revised classification emerged that adequately displayed and highlighted the broad variations in surficial materials. This classification emphasizes sediment texture and depositional environment. See Supplemental_Information for discussion of the classification system and its limitations. For each source map in the western part of the Nation, unconsolidated units were assigned to the appropriate category in our classification, and bedrock units were assigned to the surficial materials category most appropriate to their rock composition; for example, a sedimentary rock unit predominantly comprised of limestone was assigned to the category "Residual materials developed in limestone and other carbonate rocks". These source maps then were appended into a single digital map file of the western States, and additional source information for lake and eolian deposits was added (see References and Compilation Sources section of published map by Soller and Reheis, 2004). We then combined the eastern and western GIS map files into a single Postscript file and, using Adobe Illustrator, published the map in PDF format, without an accompanying GIS database. The decision to not simultaneously publish the database was not made lightly, but was necessitated by budget and time constraints. In the course of preparing the map in Adobe Illustrator, certain map units were revised in order to address peer review comments that were received after the export from ArcInfo. To prepare the GIS database for publication, these edits needed to be incorporated. The two ArcInfo files (east and west parts of the map) were written to Export format, and ESRI shapefiles were generated in ArcMap. Harumi Warner (USGS, Denver) incorporated the edits and submitted to the senior author the two shapefiles (east and west parts of the map), for verification. East and west polygon shapefiles were merged and converted to a file geodatabase. Geodatabase topology was created and topological error logs were generated. Logs listed numerous areas where problems in topological relationships existed. Common topological problems included polygons which overlapped or had gaps between them, overlying line layers (contacts, faults, etc.) which were not coincident with polygon boundaries, and line features that self overlapped. Topology rules were set in ArcMap to remove errors and create a topologically clean layer. For attribution purposes, subtypes were assigned to the geologic contacts layer. The use of subtypes ensured data consistency during the editing stages of the project. Feature class symbolization was created to closely resemble the printed version of surficial materials map and was exported to ESRI layer files. Dataset copied. \\IGSAAAHMWSG642\C$\SurfMtlsMap\Surficial_materials.gdb 20090205 13380800 Attribute accuracy was tested by manual comparison of the source with hard copy printouts and/or symbolized display of the digital geologic data on an interactive computer graphic system. In addition, attributes were compared to a master set of valid geologic unit attributes. Topological accuracy was tested using topology validation tools via ArcGIS 9.2. Specific errors that were checked included: Polygon overlaps and gaps, coincident contact lines and geologic unit borders, self overlapping lines and superfluous pseudo nodes. No duplicate features exist nor duplicate points in a data string. Intersecting lines are separated into individual line segments at the point of intersection. Feature classes in the geodatabase are topologically clean. Data set complete. No data was intentionally omitted from the hard copy source map. Not applicable. Uncertain. 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