Interactive Fault Map
- Interactive fault map
- Database Search
- KML (Google Earth) Files(13 MB KMZ)
- includes 5 fault layers: Historic, Holocene to Latest Pleistocene, Late Quaternary, Mid-Late Quaternary, Quaternary
- GIS files(16 MB ZIP file)
This database contains information on faults and associated folds in the United States that demonstrate geological evidence of coseismic surface deformation in large earthquakes during the past 1.6 million years (Myr). At the time the Quaternary Fault and Fold database was established (1993), the Quaternary time period was defined as <1.6 Myr in the1983 Geologic Time Scale, published in 1983. In 1999, it was updated to 1.8 Myr, and in 2009 it was revised to 2.6 Myr. Most recently, in 2018 it was revised again to 2.58 Myr, seeGSA Geologic Time Scale.
In order to maintain a current and relevant dataset, effective January 12, 2017, the USGS will maintain a limited number of metadata fields that characterize the Quaternary faults and folds of the United States. Archived reports are accessible from the abbreviated record.
- Fault FAQ- select topic "Faults"
About the Quaternary Faults and the National Seismic Hazard Maps
This database was used to create thefault-source characterizationin the National Seismic Hazard Maps. For the hazard maps, both the fault surface trace and the metadata are simplified representations of the geometry and behavior of the fault, based on geologic interpretation.
When you use this data, please provide proper acknowledgment. Because there are many contributors to the database, the citation will depend on which data you are using. Please use the following format according to the USGS Publishing Standards (Memorandum No. 2014.03)
The reference information about a fault in New Mexico viewed online on Jan 9, 2019would look like:
U.S. Geological Survey and New Mexico Bureau of Mines and Mineral Resources, Quaternary fault and fold database for the United States, accessed August 1, 2019, at:https://www.usgs.gov/natural-hazards/earthquake-hazards/faults.
List of cooperators:
- Alaska - Alaska Department of Natural Resources
- Arizona - Arizona Geological Survey
- California - California Geological Survey
- Colorado - Colorado Geological Survey
- Idaho - Idaho Geological Survey
- Illinois - Illinois State Geological Survey
- Louisiana - Louisiana Geological Survey
- Montana - Montana Bureau of Mines and Geology
- Nevada - Nevada Bureau of Mines and Geology
- New Mexico - New Mexico Bureau of Mines and Mineral Resources
- Texas - Texas Bureau of Economic Geology
- Utah - Utah Geological Survey
This website contains information on faults and associated folds in the United States that are believed to be sources of M>6 earthquakes during the Quaternary (the past 1,600,000 years). Maps of these geologic structures are linked to a database containing detailed descriptions and references. The database is intended to be the USGS’s archive for historic and ancient earthquake sources used in current and future probabilistic seismic-hazard analyses.
Our website presents—for the first time—a single source that summarizes important information on paleoseismic (ancient earthquake) parameters. These data are compiled from thousands of journal articles, maps, theses, and other documents, as referenced herein. The database is designed to serve a variety of needs, both in terms of the user community and methods of delivering the data.
Starting in the early 1970s, mainly in response to national concerns about the siting of nuclear reactors, scientists needed to locate active and Quaternary faults and document their characteristics. This broad research initiative resulted in new maps and studies of Quaternary faults. State (Jennings, 1975;Witkind, 1975;1975;1975;1976; Menges and Pearthree, 1983 #2073), regional (Nakata and others, 1982), and NationalHoward and others, 1978)maps were compiled to show the location and relative timing of major faults. These map compilations, however, did not provide much supporting data. Subsequent state-scale compilations, such as those byJohns and others, (1982),Stickney and Bartholemew (1987), andHecker (1993)provided some supporting database and were the first true fault compilations. The Quaternary fault and fold data for the United States has relied heavily on the past contributions, and on new efforts by State geological surveys and the U.S. Geological Survey.
The most recent effort began in 1990 in support of the International Lithosphere Program (ILP), which formed Working Group II-2. Its main objective was to compile a World Map of Active Faults (Vladimir Trifonov, chairman). In 1992, the USGS agreed to help compile maps and fault descriptions for countries in the Western Hemisphere (North, Central, and South America, as well as Australia and New Zealand). This work continues to date, with many of the compilations for Central and South America countries having been published.
In 1993, the U.S. Geological Survey began developing a database for Quaternary faults and folds for the United States in earnest, largely supported by NEHRP but with significant support from many State surveys. This product is more robust than the ILP products, mainly owing to the vast amount of data that has become available within the U.S. in the past 20-30 years and the importance that this data plays in regional and national seismic-hazard assessments (Petersen and others, 1996;Frankel and others, 1996).
The descriptions contain information on geographic, geologic, and paleoseismic parameters that are deemed critical to making geologic-based assessments of seismic hazards. In addition, we provide narrative comments that clarify, justify, or expound upon these parameters. Many of the comments in the database provide justification for the paleoseismic parameters that were chosen to characterize the faults and folds.
For this compilation, we have limited our compilation to synthesis of published literature relevant to the United States. Our definition of published literature includes typical sources (journals and maps), as well as M.S. theses and Ph.D. dissertations, governmental contract reports (which includes many NEHRP-sponsored studies), abstracts, and open-file (preliminary) reports. We generally do not cite unpublished field mapping, field notes, and other gray-literature reports that are not generally available to the public. The data presented in the compilation are extensively referenced using the standard USGS reference style, with the exception of attaching a unique number to each cited reference for convenience. This numeric identifier allows us to clearly cite multiple-same year publications for authors.
This table includes the definitions of classes used in the compilation of Quaternary faults, liquefaction features, and deformation (Crone and Wheeler,2000).
|Class A||Geologic evidence demonstrates the existence of a Quaternary fault of tectonic origin, whether the fault is exposed for mapping or inferred from liquefaction or other deformational features.|
|Class B||Geologic evidence demonstrates the existence of a fault or suggests Quaternary deformation, but either (1) the fault might not extend deeply enough to be a potential source of significant earthquakes, or (2) the currently available geologic evidence is too strong to confidently assign the feature to Class C but not strong enough to assign it to Class A.|
|Class C||Geologic evidence is insufficient to demonstrate (1) the existence of tectonic fault, or (2) Quaternary slip or deformation associated with the feature.|
|Class D||Geologic evidence demonstrates that the feature is not a tectonic fault or feature; this category includes features such as demonstrated joints or joint zones, landslides, erosional or fluvial scarps, or landforms resembling fault scarps, but of demonstrable non-tectonic origin.|
Although seismicity maps and earthquake catalogs show the past 100 to 150 years of felt and instrumental earthquakes, many faults in the United States have return times of thousands to tens of thousands of years for surface faulting events. Clearly the short seismic record will not image all the active faults that exist. Thus, this collection of data on faults and folds that record ancient earthquakes will help augment the rather short felt and instrumental seismic record that is typical of the United States and other recently developed countries.
The database is primarily a text-based collection of descriptive data that will serve a wide and varied audience. The search capabilities described below will allow the user to sort the data on a variety of fields (geographic, structural, time of movement, slip rate, etc.). The basic strategy in classifying the data has been to create a variety of bins (categories) to characterize these potential seismic sources in terms of their activity rates. You can sort the data by time of most recent movement (4 inclusive categories) or slip rate (4 exclusive categories). For example, if you want to see the youngest and most active prehistoric faults, one would search for faults that have moved in the past 15,000 years at rates>5 mm/yr.
The database has two search forms. TheQuick Searchform is very simple with only four search options available. Two options permit searches onNameandNumberof a particular fault or fold. The other two options permit geographic searches byStateandCounty.
TheAdvanced Searchform can be used to further limit the search results. The Advanced Search form allows queries on the above four parameters and on geographic options, paleoseismic characteristics, and structural characteristics. The additional geographic search options areAMS sheetandphysiographic province. The searchable paleoseismic characteristics includetimeof most recent prehistoric deformation,yearof historic deformation, andslip-ratecategory. Searchable structural characteristics includelengthof fault or fault section,averagestrikeof fault or fault section,sense of movement, anddip directionof the fault.
Complete as few or many of the fields as you wish. The narrower the search; the quicker the results will be available. If you expect that your search will result in a large number of results (more than 40), you can reduce the amount of time to obtain those results by limiting the number of results on each page at the bottom of the search form.
There are three basic types of search fields: those with (1) pull-down menus, (2) text, and (3) numeric. The fields having pull-down menus provide all available options. Text fields like Name, County, and AMS sheet are not case sensitive and will search on partial words. The numeric fields such as Number, Year of historic deformation, Length, and Average strike should only contain numeric expressions. The Number field will not find specific sections (a, b, c, etc.); instead search for the fault number only. The Year of historic deformation requires a four-digit year in each field; use values that would encompass the historical record (such as 1600 and 2005) to search for all entries in this field. The length and average-strike searches will yield all records with inclusive values and show all sections of a fault if one of those sections has the desired value.
Many modern web browsers have an “auto complete” function that will fill in data fields based on the first several characters or digits from your browser profile. You should turn off this feature prior to conducting searches that require entering characters or digits.
The database structure was created byKathy Haller(USGS) and an early version of the web interface and search engines were created by Larry Mayer (formerly of the University of Miami at Oxford, Ohio). The GIS data was engineered by Richard Dart and maintained by Jerry Mayer (USGS). The fault and fold traces were digitized mainly by Richard Dart, with help from Dean Hancock*. Static maps were made by Susan Rhea (USGS), Richard Dart, and Damon Sather*. The graphic web browser and ArcIMS module (still under development) were created by Susan Rhea, Damon Sather*, Karen Morgan*, and John Cox*. Much of the reference database and entry of data into the text database was done with the able assistance of Philly Morrow, Meredith Frey, and Kelli Clark (*, all former student interns or contractors to the USGS).
- Hecker, S., 1993, Quaternary tectonics of Utah with emphasis on earthquake-hazard characterization: Utah Geological Survey Bulletin 127, 157 p., 6 pls., scale 1:500,000.
- Jennings, C.W., 1975, Fault map of California with locations of volcanoes, thermal springs, and thermal wells: California Division of Mines and Geology California Geologic Data Map 1, scale 1:750,000.
- Johns, W.M., Straw, W.T., Bergantino, R.N., Dresser, H.W., Hendrix, T.E., McClernan, H.G., Palmquist, J.C., and Schmidt, C.J., 1982, Neotectonic features of southern Montana east of 112°30' west longitude: Montana Bureau of Mines and Geology Open-File Report 91, 79 p., 2 sheets.
- Menges, C.M., and Pearthree, P.A., 1983, Map of neotectonic (latest Pliocene-Quaternary) deformation in Arizona: Arizona Bureau of Geology Mineral Technology Open-File Report 83-22, 48 p., scale 1:500,000.
- Stickney, M.C., and Bartholomew, M.J., 1987, Preliminary map of late Quaternary faults in western Montana: Montana Bureau of Mines and Geology Open-File Report 186, 1 pl., scale 1:500,000.