This data release contains data associated with the USGS SIM publication "Stratigraphic Cross Sections of the Lewis Shale in the eastern part of the Southwestern Wyoming Province, Wyoming and Colorado". North-to-southeast (A–A’), west-to-east (B–B’), and southwest-to-northeast (C–C’) cross sections were created from 105 wells throughout the eastern part of the Southwestern Wyoming Province. The cross sections highlight 15 clinothems within the Lewis Shale, Fox Hills Sandstone, and Lance Formation progradational system. Data include well information and depths to key stratigraphic surfaces for 105 wells within the three cross sections. Well information includes the cross section identification, API #, well name, latitude in decimals, longitude in decimals, projection datum, county, state, Kelly Bushing elevation in feet, section, township, and range. Wells 19*, 26*, 69* and 70* are intersection points between the three sections. The stratigraphic data are all listed in measured depth relative to the Kelly bushing elevation and include the depth to the top of the Almond Formation, depth to the top and base of the informal Asquith marker, depth to the tops of 15 flooding surfaces which define the series of clinothems within the Lewis Shale, depth the top of the Lewis Shale, and depth to the top of the Fox Hills Sandstone.

In 2021 the United States Geological Survey (USGS) sampled the lower part of the Upper Cretaceous Lewis Shale in the eastern part of the Southwestern Wyoming Province to better characterize its petroleum source rock potential for an upcoming resource assessment. Ninety-five samples from 24 wells were collected from well cuttings of the lower part of the Lewis Shale stored at the U.S. Geological Survey Core Research Center in Lakewood, Colorado. The selected wells are located near the shallow margins of the basin to obtain samples that were not subjected to the effects of deep burial and subsequent organic carbon loss due to thermal maturation as described by Daly and Edman (1987) (fig, 1). The sample intervals were selected based on high gamma ray responses that Pyles and Slatt (2007) interpreted to be organic-rich condensed sections. Special emphasis was given to the Asquith marker bed which represents the maximum transgression of the Lewis Shale (Pasternack, 2005) (fig. 2).

In 2021 the United States Geological Survey (USGS) sampled the lower part of the Upper Cretaceous Lewis Shale in the eastern part of the Southwestern Wyoming Province to better characterize its petroleum source rock potential for an upcoming resource assessment. Ninety-five samples from 24 wells were collected from well cuttings of the lower part of the Lewis Shale stored at the U.S. Geological Survey Core Research Center in Lakewood, Colorado. The selected wells are located near the shallow margins of the basin to obtain samples that were not subjected to the effects of deep burial and subsequent organic carbon loss due to thermal maturation as described by Daly and Edman (1987) (fig, 1). The sample intervals were selected based on high gamma ray responses that Pyles and Slatt (2007) interpreted to be organic-rich condensed sections. Special emphasis was given to the Asquith marker bed which represents the maximum transgression of the Lewis Shale (Pasternack, 2005) (fig. 2).

The Wind River Basin is a large Laramide (Late Cretaceous through Eocene) structural and sedimentary basin that encompasses about 7,400 square miles in central Wyoming (fig. 1). The basin is bounded by the Washakie Range and Owl Creek and southern Bighorn Mountains on the north, the Casper arch on the east, the Granite Mountains on the south, and Wind River Range on the west (figs. 1). Many important conventional and unconventional oil and gas resources have been discovered and produced from reservoirs ranging from Mississippian through Tertiary in age (Keefer, 1969; Fox and Dolton, 1989, 1996; De Bruin, 1993; Johnson and others, 1996, 2007). It has been suggested by numerous authors including: Keefer, 1969; Meissner and others, 1984; Fox and Dolton, 1989, 1996; Johnson and Rice, 1993; Nuccio and others, 1996; and Schelling and Wavrek, 1999, 2001: that various Upper Cretaceous marine shales are the principal hydrocarbon source rocks for many of these accumulations. With new drilling and well completion technologies, equivalent marine source rock intervals, in particular the Niobrara Formation, are now important continuous (unconventional) shale gas and shale oil objectives in other Rocky Mountain basins ((Matthews, 2011; Sonnenberg, 2011; Williams and Lyle, 2011; Durham, 2012a,b, 2013; Taylor and Sonnenberg, 2014; and Hawkins, 2016). In the Wind River Basin the Niobrara is represented by shales, calcareous shales, marls, siltstones, and sandstones in the lower shaly member of the Upper Cretaceous Cody Shale (Finn, 2017) (fig. 2). Please see supplemental information for associated references. Selected figures have also been included to help describe this data release. These figures are provided in pdf and jpg format. These include: Fig. 1_Rocky Mountain basins.pdf/jpg. Map of Rocky Mountain region showing locations of Laramide sedimentary and structural basins and intervening uplifts. Fig. 2_Regional Cretaceous X section.pdf/jpg. Regional east-west stratigraphic cross section of Cretaceous rocks in the Wind River Basin. Each modified from Finn (2017).

The Wind River Basin is a large Laramide (Late Cretaceous through Eocene) structural and sedimentary basin that encompasses about 7,400 square miles in central Wyoming (fig. 1). The basin is bounded by the Washakie Range and Owl Creek and southern Bighorn Mountains on the north, the Casper arch on the east, the Granite Mountains on the south, and Wind River Range on the west (figs. 1). Many important conventional and unconventional oil and gas resources have been discovered and produced from reservoirs ranging from Mississippian through Tertiary in age (Keefer, 1969; Fox and Dolton, 1989, 1996; De Bruin, 1993; Johnson and others, 1996, 2007). It has been suggested by numerous authors including: Keefer, 1969; Meissner and others, 1984; Fox and Dolton, 1989, 1996; Johnson and Rice, 1993; Nuccio and others, 1996; and Schelling and Wavrek, 1999, 2001: that various Upper Cretaceous marine shales are the principal hydrocarbon source rocks for many of these accumulations. With new drilling and well completion technologies, equivalent marine source rock intervals, in particular the Niobrara Formation, are now important continuous (unconventional) shale gas and shale oil objectives in other Rocky Mountain basins ((Matthews, 2011; Sonnenberg, 2011; Williams and Lyle, 2011; Durham, 2012a,b, 2013; Taylor and Sonnenberg, 2014; and Hawkins, 2016). In the Wind River Basin the Niobrara is represented by shales, calcareous shales, marls, siltstones, and sandstones in the lower shaly member of the Upper Cretaceous Cody Shale (Finn, 2017) (fig. 2). Please see supplemental information for associated references. Selected figures have also been included to help describe this data release. These figures are provided in pdf and jpg format. These include: Fig. 1_Rocky Mountain basins.pdf/jpg. Map of Rocky Mountain region showing locations of Laramide sedimentary and structural basins and intervening uplifts. Fig. 2_Regional Cretaceous X section.pdf/jpg. Regional east-west stratigraphic cross section of Cretaceous rocks in the Wind River Basin. Each modified from Finn (2017).

The Bighorn Basin is a large Laramide structural and sedimentary basin that encompasses about 10,400 square miles in north-central Wyoming and south-central Montana (fig. 1). The basin is bounded on the northeast by the Pryor uplift, on the east by the Bighorn uplift and on the south by the Owl Creek uplift. The northern margin is formed by a zone of faulting and folding referred to as the Nye-Bowler lineament. The western and northwestern margins are formed by the Absaroka volcanics and Beartooth uplift, respectively (fig. 1). Commercial hydrocarbon production was first established in the Bighorn Basin when oil was discovered from Cretaceous reservoirs at Garland field in 1906 (Biggs and Espach, 1960). Since then, many important conventional oil and gas resources have been discovered and produced from reservoirs ranging from Cambrian through Tertiary in age (De Bruin, 1993; Fox and Dolton, 1989,1996). In addition, a potential basin-centered gas accumulation may be present in Cretaceous reservoirs in the deeper parts of the basin (Spencer, 1987; Ryder, 1987; Surdam and others, 1997; Johnson and Finn, 1998; Johnson and others, 1999; and Finn and others, 2010). It has been suggested that various Upper Cretaceous marine shales are the principal hydrocarbon source rocks for many of these accumulations (Geis, 1923; Burtner and Warner, 1984; Hagen and Surdam, 1984; Meissner and others, 1984; Ryder, 1987). With new drilling and well completion technologies, equivalent marine source rock intervals, in particular the Niobrara Formation, are now important continuous (unconventional) shale gas and shale oil objectives in other Rocky Mountain basins (Matthews, 2011; Sonnenberg, 2011; Williams and Lyle, 2011; Durham, 2012a,b, 2013; Taylor and Sonnenberg, 2014; and Hawkins, 2016). In the Bighorn Basin the Niobrara is represented by shales, calcareous shales, marls, siltstones, and sandstones in the lower part of the Upper Cretaceous Cody Shale (Finn, 2014) (fig. 2). Please see supplemental information for associated references. Selected figures have also been included to help describe this data release. These figures are provided in pdf and jpg format. These include: Fig. 1_Rocky Mountain basins.pdf/jpg. Map of Rocky Mountain region showing locations of Laramide sedimentary and structural basins and intervening uplifts. Fig. 2_Xsection.pdf/jpg. Regional east-west stratigraphic cross section of Cretaceous rocks in the Wind River Basin. Each modified from Finn (2014). Please see data dictionary sheet in the excel file for detailed table column/attribute information.

The Bighorn Basin is a large Laramide structural and sedimentary basin that encompasses about 10,400 square miles in north-central Wyoming and south-central Montana (fig. 1). The basin is bounded on the northeast by the Pryor uplift, on the east by the Bighorn uplift and on the south by the Owl Creek uplift. The northern margin is formed by a zone of faulting and folding referred to as the Nye-Bowler lineament. The western and northwestern margins are formed by the Absaroka volcanics and Beartooth uplift, respectively (fig. 1). Commercial hydrocarbon production was first established in the Bighorn Basin when oil was discovered from Cretaceous reservoirs at Garland field in 1906 (Biggs and Espach, 1960). Since then, many important conventional oil and gas resources have been discovered and produced from reservoirs ranging from Cambrian through Tertiary in age (De Bruin, 1993; Fox and Dolton, 1989,1996). In addition, a potential basin-centered gas accumulation may be present in Cretaceous reservoirs in the deeper parts of the basin (Spencer, 1987; Ryder, 1987; Surdam and others, 1997; Johnson and Finn, 1998; Johnson and others, 1999; and Finn and others, 2010). It has been suggested that various Upper Cretaceous marine shales are the principal hydrocarbon source rocks for many of these accumulations (Geis, 1923; Burtner and Warner, 1984; Hagen and Surdam, 1984; Meissner and others, 1984; Ryder, 1987). With new drilling and well completion technologies, equivalent marine source rock intervals, in particular the Niobrara Formation, are now important continuous (unconventional) shale gas and shale oil objectives in other Rocky Mountain basins (Matthews, 2011; Sonnenberg, 2011; Williams and Lyle, 2011; Durham, 2012a,b, 2013; Taylor and Sonnenberg, 2014; and Hawkins, 2016). In the Bighorn Basin the Niobrara is represented by shales, calcareous shales, marls, siltstones, and sandstones in the lower part of the Upper Cretaceous Cody Shale (Finn, 2014) (fig. 2). Please see supplemental information for associated references. Selected figures have also been included to help describe this data release. These figures are provided in pdf and jpg format. These include: Fig. 1_Rocky Mountain basins.pdf/jpg. Map of Rocky Mountain region showing locations of Laramide sedimentary and structural basins and intervening uplifts. Fig. 2_Xsection.pdf/jpg. Regional east-west stratigraphic cross section of Cretaceous rocks in the Wind River Basin. Each modified from Finn (2014). Please see data dictionary sheet in the excel file for detailed table column/attribute information.

The Bighorn Basin is a large Laramide structural and sedimentary basin that encompasses about 10,400 square miles in north-central Wyoming and south-central Montana (fig. 1). The basin is bounded on the northeast by the Pryor uplift, on the east by the Bighorn uplift and on the south by the Owl Creek uplift. The northern margin is formed by a zone of faulting and folding referred to as the Nye-Bowler lineament. The western and northwestern margins are formed by the Absaroka volcanics and Beartooth uplift, respectively (fig. 1). Commercial hydrocarbon production was first established in the Bighorn Basin when oil was discovered from Cretaceous reservoirs at Garland field in 1906 (Biggs and Espach, 1960). Since then, many important conventional oil and gas resources have been discovered and produced from reservoirs ranging from Cambrian through Tertiary in age (De Bruin, 1993; Fox and Dolton, 1989,1996). In addition, a potential basin-centered gas accumulation may be present in Cretaceous reservoirs in the deeper parts of the basin (Spencer, 1987; Ryder, 1987; Surdam and others, 1997; Johnson and Finn, 1998; Johnson and others, 1999; and Finn and others, 2010). It has been suggested that various Upper Cretaceous marine shales are the principal hydrocarbon source rocks for many of these accumulations (Geis, 1923; Burtner and Warner, 1984; Hagen and Surdam, 1984; Meissner and others, 1984; Ryder, 1987). With new drilling and well completion technologies, equivalent marine source rock intervals, in particular the Niobrara Formation, are now important continuous (unconventional) shale gas and shale oil objectives in other Rocky Mountain basins (Matthews, 2011; Sonnenberg, 2011; Williams and Lyle, 2011; Durham, 2012a,b, 2013; Taylor and Sonnenberg, 2014; and Hawkins, 2016). In the Bighorn Basin the Niobrara is represented by shales, calcareous shales, marls, siltstones, and sandstones in the lower part of the Upper Cretaceous Cody Shale (Finn, 2014) (fig. 2). Please see supplemental information for associated references. Selected figures have also been included to help describe this data release. These figures are provided in pdf and jpg format. These include: Fig. 1_Rocky Mountain basins.pdf/jpg. Map of Rocky Mountain region showing locations of Laramide sedimentary and structural basins and intervening uplifts. Fig. 2_Xsection.pdf/jpg. Regional east-west stratigraphic cross section of Cretaceous rocks in the Wind River Basin. Each modified from Finn (2014). Please see data dictionary sheet in the excel file for detailed table column/attribute information.

This data release contains the boundaries of assessment units and input data for the assessment of undiscovered oil and gas resources in the Mesaverde Group and Lance Formation in the Southwestern Wyoming Province, Wyoming, Utah, and Colorado. The assessment unit is the fundamental unit used in the National Assessment Project for the assessment of undiscovered oil and gas resources. The assessment unit is defined within the context of the higher-level Total Petroleum System. The assessment unit is shown herein as a geographic boundary interpreted, defined, and mapped by the geologist responsible for the province and incorporates a set of known or postulated oil and (or) gas accumulations sharing similar geologic, geographic, and temporal properties within the Total Petroleum System, such as source rock, timing, migration pathways, trapping mechanism, and hydrocarbon type. The assessment unit boundary is defined geologically as the limits of the geologic elements that define the assessment unit, such as reservoir rock, geologic structures, source rock, and seal lithologies. The only exception to this are assessment units that border a Federal-State water boundary. In these cases, the Federal-State water boundary forms part of the assessment unit boundary. In addition to the shapefile, for U.S. assessments, allocation tables are provided that enumerate percentages assigned to various land categories. Machine-readable tables are also provided that contain the input and results for each assessment unit summarized in the USGS Fact Sheet. Methodology for assessments are documented in USGS Data Series 547 for continuous assessments (https://pubs.usgs.gov/ds/547) and USGS DDS69-D, Chapter 21 for conventional assessments (https://pubs.usgs.gov/dds/dds-069/dds-069-d/REPORTS/69_D_CH_21.pdf). See supplemental information for a detailed list of files included in this data release.

The Wyoming statewide time-stamped oil and gas wells shapefile was developed to provide a historical perspective of drilling activity for the Wyoming Landscape Conservation Initiative (WLCI). This product approximates start and stop dates for each well in Wyoming based on database attributes. These data originated from the Wyoming Oil and Gas Conservation Commission (WOGCC). Data represent 120 years of oil and gas drilling (1900 to 2020) and will facilitate a landscape-level approach to integrated science-based assessments, resource management, and land-use decision making. Oil and gas data from WOGCC were used in a dataset previously published by Biewick in 2010 (https://pubs.usgs.gov/ds/625/). This product expands the timeframe of drilling acitivity to 2020, compared to the earlier publication end date of 2010. We extended start and stop dates through 2020 and used a different process to extract start and stop information (detailed in the Process Description portion of Data Quality Information). We did not have access to last completion date (date of the last completion report filing) and did not include production information.