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*Spring 2025*

New maps, data tools, and hazard models mark a season of progress—and 100 years since the Gros Ventre Slide.




* The Director’s Corner—2025 Geology Field Season Kickoff [ #link_2 ]
* The Gros Ventre Slide: A Centennial Retrospective [ #link_3 ]
* Recent Publications from the WSGS: Mapping Progress Across the State [ #link_4 ]





Welcome to the 2025 Spring Newsletter

Taking a radiation reading with the scintillometer

Spring has arrived in Wyoming, and with it comes the start of a new field season for the Wyoming State Geological Survey. As our geologists head into the field and new staff join the team, we remain focused on advancing geologic knowledge and providing public access to high-quality data.

This issue highlights the 100th anniversary of the Gros Ventre Slide and showcases several key publications released since winter, including new geologic maps, updated digital tools, and hazard assessments. We’re proud to share these resources as part of our ongoing mission to serve the people of Wyoming through geoscience.



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The Director’s Corner—2025 Geology Field Season Kickoff

Erin Campbell Director and State Geologist

Spring 2025 marks the beginning of the geology field season, a pivotal time for research and exploration of Wyoming’s geology at the WSGS. With several new staff at the agency, we started this year with a short field excursion intended to familiarize them with safety, preparation, technology, data collection protocols, and post-field data processing. 

In early May, we descended on Baroil, Wyoming with three field vehicles and 12 staff members for a field visit to the Osborne Well 7.5 minute quadrangle. The area is composed almost entirely of the Eocene Battle Spring Formation, making geologic interpretation only a minor component of the mapping effort. The region is just northeast of the Lost Creek Uranium Mine. The quadrangle contains historic evidence of uranium exploration as well as many wells associated with ongoing in-situ uranium mining in the region.


Photo by Katie Lyon

Photo by Katie Lyon

Geologic mapping has evolved considerably since the days of the paper field notebook and map, although some of us still enjoy these traditional methods. Today, field tablets and smartphones are loaded with maps and software to document spatially referenced data and photographs, which can be quickly uploaded upon return to the office. On this trip, the team was able to troubleshoot technical issues and gain proficiency with new software and hardware, in preparation for more extensive fieldwork planned for this summer.  

The majority of geologic fieldwork in the United States is conducted by state geological surveys and funded by the federal government through the USGS STATEMAP program, which currently faces the same funding uncertainties affecting many federal programs. However the WSGS is well-positioned to conduct alternative fieldwork this summer, should federal funding become unavailable during Wyoming’s brief field season. 

Photo by Jim Stafford

Photo by Jim Stafford

Geologic field mapping is a fundamental source of geologic information and is widely recognized as the critical first step in energy and mineral exploration, as well as geologic hazard identification. Less well known are the applications of geologic maps in the construction industry, geohydrology, and regulatory compliance arenas. A recent report on the economic benefit of geological mapping calculated the return on investment for geologic mapping, and it found that every $1 invested in geological mapping returned $7–$10 in economic benefits. The full report is available here:

[link removed]

Of course, the most important aspect of fieldwork is ensuring everyone returns safely. To that end, we held a detailed field safety meeting back at the office, reviewing topics such as weather, gear, wildlife, terrain, driving, and vehicle safety. Additionally, we provide an opportunity for certification in CPR and first aid, in case of emergencies during field operations. 

The WSGS mapping team is now prepared and ready for what is shaping up to be a productive summer field season.

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The Gros Ventre Slide: A Centennial Retrospective

This month marks the 100th anniversary of the Gros Ventre Slide, the largest and one of the most impactful landslides to occur in Wyoming in recorded history. At approximately 4 p.m. on June 23, 1925, an estimated 50 million cubic yards of rock and debris rushed down the north side of Sheep Mountain—14 miles northeast of the town of Jackson—and into the valley of the Gros Ventre River 2,100 feet below. The dramatic event was over within a few minutes, and as the dust settled, it revealed a landscape that was fundamentally changed.

The channel of the Gros Ventre River was buried beneath 225 feet of landslide debris, which extended up the opposite (northern) valley wall to a depth of 350 feet. With the river blocked by the landslide debris, water began filling the upstream valley to form what is today known as Lower Slide Lake. Within three weeks, Lower Slide Lake had reached a depth of 200 feet and inundated about 11,000 acres of the valley bottom. Two years later, on May 18, 1927, the snowmelt-swollen Gros Ventre River overtopped the landslide dam and unleashed a catastrophic flood. This flood destroyed the town of Kelly, four miles downstream from the dam, and resulted in six fatalities.

Guil Huff on house roof. Photo credit: Jackson Hole Historical Society and Museum collection, 1958.0380.001

Guil Huff on house roof. Photo credit: Jackson Hole Historical Society and Museum collection, 1958.0380.001

The Gros Ventre Slide occurred along the northern flank of the Gros Ventre Range, which was uplifted during the Laramide Orogeny approximately 50 million years ago. Whereas a major thrust fault bounds the southern margin of the Gros Ventre Range, the northern flank is characterized by more gently dipping Paleozoic and Mesozoic sedimentary rocks. In the vicinity of the Gros Ventre Slide, these sedimentary units dip roughly 20 degrees northeast, and their bedding planes form the forested valley wall on the south side of the Gros Ventre River. Given the 2,100 feet of topographic relief between the ridge of Sheep Mountain and the valley bottom, the slope-parallel bedding within the sedimentary units, and the undercut toe of the slope from erosion by the Gros Ventre River, this location was primed for slope failure.

The landslide involved rock from the Amsden Formation (Pennsylvanian and Upper Mississippian) and Tensleep Sandstone (Pennsylvanian). The Amsden Formation is characterized by shale and siltstone with dolomite and limestone interbeds, and it is conformably overlain by limestone and dolomite beds of the basal Tensleep that transition upward into a well-indurated, fine-grained sandstone. The contrast between the weak, impermeable shales of the Amsden Formation and the overlying hard, heavily jointed Tensleep Sandstone was a key element in the development of the landslide. This condition allowed groundwater to penetrate through the Tensleep Sandstone and saturate deeply weathered horizons above the impermeable Amsden Formation shales, which increased the pore fluid pressure and decreased the frictional strength of these layers, leaving them susceptible to failure.

Furthermore, the spring of 1925 was unusually warm and wet, and higher-than-normal runoff and meltwater infiltration undoubtedly contributed to the saturated soil conditions that preceded the Gros Ventre Slide. The ultimate trigger of slope failure may have been an earthquake. While there was no instrumental seismic monitoring in Jackson Hole in the 1920s, local residents reported feeling multiple earthquakes in the weeks leading up to June 23rd, including an earthquake of estimated magnitude 3–4 that occurred at 8 p.m. on June 22nd—20 hours prior to the landslide. It is possible that the ground shaking from this earthquake kicked off a chain of events that began with liquefaction of the saturated, weathered horizons at the base of the Tensleep Sandstone and culminated hours later with the total failure of the slope.

The Gros Ventre Slide is often cited as a classic example of a rockslide, where a detached mass of rock slips along a discrete failure plane and slides downslope as a roughly intact mass before subsequently breaking apart. However, it is likely that this mass movement was much more complex and involved a component of flow, where the detached material deformed internally. This aligns with eyewitness accounts that described the front of the mass as “rolling” downslope like a wave of water. Regardless of the movement mechanics, the effect of the Gros Ventre Slide on the landscape was profound and remains unmistakable to this day.

While a lot has changed in Wyoming in the century since the Gros Ventre Slide, the underlying geologic factors that contributed to the event remain the same. The Gros Ventre River valley—like many of the mountainous regions in northwest Wyoming—is characterized by steep slopes and relatively weak rocks, meaning that landslides will continue to occur. The Gros Ventre Slide serves as a reminder of the destructive potential of unstable slopes, and its legacy underscores the importance of studying geologic hazards and communicating their implications to the public—a core component of the WSGS’s mission.

Join the WSGS, Bridger-Teton National Forest, Geologists of Jackson Hole, History Jackson Hole, and other local organizations on Saturday, June 7th to observe the 100th anniversary of the Gros Ventre Slide at the Gros Ventre Geological Site. There will be presentations about the geology and history of the landslide, as well as an unveiling of new interpretive signs. Anyone interested in attending is asked to RSVP to Hannah Jacobsen at [email protected], or 307-739-5587.

James Mauch *James Mauch*

James joined the Wyoming State Geological Survey in 2019 as a geologist in the Hazards and Groundwater division. He holds a B.S. in earth sciences from Montana State University and an M.S. in geology from Utah State University. He specializes in geologic hazards, geologic mapping, and geomorphology, and is especially fond of any project that takes him into the field to study geologically active landscapes. In his free time, James enjoys exploring wild places under his own power, generally via skis, bike, or a pair of hiking shoes.



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Recent Publications from the WSGS: Mapping Progress Across the State

Since the release of our Winter 2024 newsletter, the WSGS has published a number of important new products that further our mission to characterize Wyoming’s geology and provide accessible geoscience information to the public. These publications span topics from data standardization and geologic hazard modeling to resource development and infrastructure mapping. Below, we highlight four key releases from the past season.

Standardizing the State: GeMS Conversions Enhance Access to Bedrock Mapping Data

In May 2025, the WSGS completed a major data modernization effort by converting 28 legacy 1:100,000-scale bedrock geologic maps into the Geologic Map Schema (GeMS), a standardized format developed by the U.S. Geological Survey (USGS) for the digital publication of geologic map data. These updates span maps originally published between 1992 and 2011 and represent decades of geological fieldwork conducted across a broad range of Wyoming's geologic provinces.

The transition to GeMS format is a foundational step in building a seamless, statewide 1:100,000-scale geologic database—an essential tool for everything from academic research and natural resource development to infrastructure planning and environmental assessments. Prior to this conversion, each map existed as a standalone product with unique formatting and symbology, making integration difficult and prone to misinterpretation.

Map of 1:100,000-scale bedrock maps in Wyoming

Map of 1:100,000-scale bedrock maps in Wyoming

*What is GeMS?*

The Geologic Map Schema (GeMS) is a nationally adopted data model that standardizes the way geologic map information is stored and shared. Developed through collaboration between the USGS and state geological surveys, GeMS defines a consistent set of database tables, field names, and coding rules that improve interoperability across platforms and between organizations. It bridges the gap between traditional cartography and modern GIS, allowing users to more easily query, visualize, and analyze geological features.

Adopting GeMS allows the WSGS to:


* Provide geologic data in widely used GIS formats (shapefiles and file geodatabases)
* Harmonize geologic unit terminology and symbology across disparate datasets
* Reduce the need for manual reconciliation of map inconsistencies
* Establish a consistent framework for future mapping projects

*Project Scope and Impact*

As of spring 2025, the WSGS has completed GeMS conversions for 28 quadrangles—roughly half of the published 1:100,000-scale geologic maps in the state. These maps cover diverse geological settings, including the Bighorn Basin, Wind River Basin, Powder River Basin, and Laramide uplifts, and represent some of the most heavily studied and economically significant areas of Wyoming.

“Standardizing these maps in a digital format makes them significantly more useful for a wide range of users—from local planners and engineers to academic researchers and exploration geologists,” said Dr. Erin Campbell, WSGS Director and Wyoming State Geologist. “It supports better decision-making through more accessible, high-quality geologic data.”

Each dataset includes an abstract, metadata, and fully attributed GIS files. These products are available individually and are intended to support both standalone and regional-scale geologic investigations. The effort was partially funded by the USGS National Cooperative Geologic Mapping Program (NCGMP), which promotes collaboration between federal and state agencies to improve geologic mapping nationwide.

To explore the converted data or download individual map packages, visit wsgs.wyo.gov [ [link removed] ].

New Quadrangle Maps: Rawlins and Red Desert Basin
Portion of WSGS Map Series 111, Geologic map of the Red Desert Basin 30' x 60' quadrangle, Sweetwater County, Wyoming

Portion of WSGS Map Series 111, Geologic map of the Red Desert Basin 30' x 60' quadrangle, Sweetwater County, Wyoming

In early 2025, the WSGS released updated geologic maps of the Rawlins and Red Desert Basin 30′ x 60′ quadrangles—two cornerstone regions in Wyoming’s central southern corridor. These maps represent a significant advancement in both geologic accuracy and data resolution, shedding new light on the complex structures and resources found within the greater Great Divide Basin region.

Together, these quadrangles cover a broad area extending from the Killpecker Sand Dunes in the north to Miller Hill and the Delaney Rim in the south, and from Rock Springs in the west to beyond Rawlins in the east. These maps now serve as some of the most up-to-date regional references available for this part of the state.

*Modern Tools for Complex Geology*

The updated maps incorporate extensive new fieldwork, detailed stratigraphic reinterpretation, and high-resolution lidar data to refine bedrock contacts, fault traces, and surficial unit delineations. Geologists placed particular emphasis on unraveling the complex structural relationships within the Rawlins and Rock Springs uplifts, along with sedimentary basin-fill relationships in the Great Divide Basin, northern Atlantic Rim, and parts of the Washakie Basin.

Geologic formations in this area range primarily from Cretaceous to Quaternary in age, though exposures of Paleozoic, Mesozoic, and even Precambrian rocks occur, especially in uplifted zones. This broad temporal span makes the region an important resource for understanding the tectonic and depositional history of southern Wyoming.

“These maps reflect some of the most challenging and geologically rich terrain in the state,” said WSGS Director and State Geologist Dr. Erin Campbell. “They provide a better foundation for understanding energy resources, stratigraphy, and structure in an area where multiple basins and uplifts converge.”

*Applications for Industry and Infrastructure*

The updated quadrangles are particularly valuable for energy and mineral resource evaluations. The region is known to host deposits of uranium, coal, and hydrocarbon resources, and is also under evaluation for carbon dioxide (CO₂) sequestration potential. The maps improve subsurface correlation and provide important context for ongoing and future exploration.

The area’s significance is amplified by its infrastructure: it encompasses a major segment of U.S. Interstate 80, portions of U.S. Highway 287, and the Union Pacific Railroad corridor. Accurate geologic mapping in this region is critical for planning around geologic hazards, land-use decisions, and transportation development.

Both maps are published as part of the WSGS Map Series and are accompanied by (GeM) Level 3-compliant geodatabases that allow users to interact with and analyze the data digitally. Supporting documentation includes map pamphlets with detailed descriptions of units, structure, and mapping methods.

The Rawlins [ [link removed] ] and Red Desert Basin [ [link removed] ] quadrangle maps are available for download from the WSGS website, along with metadata, geodatabases, and printable map plates.

Mapping Landslide Risk: New Teton County Susceptibility Model Released
Map plate showing deep-seated landslide susceptibility in central and southern Teton County.

Map plate from WSGS Open File Report 2025-1 showing deep-seated landslide susceptibility in central and southern Teton County. Darker red colors symbolize regions of higher susceptibility.

In March 2025, the WSGS released a landmark geologic hazard product: a high-resolution susceptibility map identifying areas most prone to deep-seated landslides in central and southern Teton County. Published as Open File Report 2025-1, the study is the most detailed statewide effort to date for this landslide type and provides essential tools for emergency planners, local governments, engineers, and landowners in one of Wyoming’s most geologically active regions.

Teton County has long been synonymous with landslide risk. From the massive Gros Ventre Slide of 1925, which destroyed the town of Kelly, to more recent events like the Budge Drive and Big Fill landslides, slope instability continues to pose a threat to property, infrastructure, and public safety. This report helps fill a critical knowledge gap by identifying exactly where deep-seated landslides are most likely to occur and under what geologic conditions.

*A New Standard for Landslide Modeling*

The mapping effort was led by James Mauch, WSGS geologist and lead author, and James Stafford, WSGS geohydrologist. The team used a combination of 57 geologic maps and high-resolution lidar elevation data to build a susceptibility model with a 10-meter raster resolution—a level of detail rarely achieved in regional landslide hazard mapping. The model evaluates the relationship between slope angle and bedrock strength to predict areas of increased landslide potential.

The resulting susceptibility raster was validated against an independent dataset of more than 2,100 mapped landslides, ensuring the model’s reliability and relevance to real-world conditions. The analysis found that approximately 84 percent of the study area is at least marginally susceptible to deep-seated landslides, reflecting the widespread presence of steep slopes, weak lithologies, and geologically young terrain across the region.

“This is an excellent example of how geoscience can support public safety and smart land-use decisions,” said Dr. Erin Campbell, WSGS Director and State Geologist. “Landslide susceptibility maps are a powerful way to translate complex geologic data into something practical and actionable.”

*Supporting Smart Growth and Risk Mitigation*

The susceptibility map is intended to support a range of applications, including:


* Land-use planning and zoning decisions by local governments
* Emergency management preparedness and hazard mitigation
* Engineering site assessments for residential and commercial development
* Insurance risk evaluations for geologic hazards

Importantly, the authors emphasize that the model focuses exclusively on deep-seated landslides, which typically involve large, slow-moving masses of rock or soil. It does not account for shallow landslides, rockfalls, or debris flows—hazards that may still be present in some areas but require different modeling approaches.

The report includes a technical discussion of the model’s limitations, such as its exclusion of external triggering mechanisms like seismic events or intense rainfall. This transparency helps users apply the data appropriately and understand its scope.

*Access and Interactivity*

The full report, GIS raster data, and printable map plate are available for free download on the WSGS website [ [link removed] ]. The landslide susceptibility data can also be viewed on the Wyoming Geologic Hazards Map, an interactive web-based tool that allows users to explore hazard data by region, scale, and land parcel.

With development pressure increasing in mountainous regions of northwest Wyoming, this new map is a timely and important tool for reducing landslide risk and promoting resilient communities.

Oil and Gas, Online and Updated: Interactive Map Adds New Data and Capabilities
Screenshot of the WSGS Interactive Oil and Gas Map of Wyoming, showing current infrastructure layers across the state.

Screenshot of the WSGS Interactive Oil and Gas Map of Wyoming, showing current infrastructure layers across the state. The web-based platform allows users to explore well data, pipelines, production facilities, and subsurface interpretations with downloadable geospatial datasets

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In April 2025, the Wyoming State Geological Survey released the seventh major update to its interactive oil and gas map—a web-based platform that delivers public access to thousands of wells, fields, facilities, and supporting geologic data across the state. The update brings not only new data but also greater detail and improved accuracy, solidifying the map’s reputation as one of WSGS’s most widely used digital tools.

Originally launched in 2016, the interactive map was developed to build on the legacy of the WSGS’s traditional printed oil and gas maps, which have been in production since 1915. The digital version has since become indispensable for industry professionals, land managers, private citizens, academic researchers, and state and federal agencies, offering the flexibility and functionality of modern GIS technology.

“This platform allows us to keep Wyoming’s vital energy data current and accessible,” said Dr. Erin Campbell, WSGS Director and State Geologist. “While I still appreciate the value of a printed map, having this resource available in real-time is much more practical for today’s users.”

*What’s New in This Release?*

The 2025 update includes:


* 450+ new wells in named oil and gas fields
* 1,650+ new and historical wildcat wells
* Updated facility data, including pipelines, gas plants, and refineries
* Cross-verified well status and production information using datasets from the Wyoming Oil and Gas Conservation Commission (WOGCC)

Much of the effort behind this update involved data cleaning and quality control. WSGS geologists compared WOGCC well data with historical maps, reports, and records to ensure accurate well locations, production histories, and status classifications.

“It may look like a subtle change to the interface, but each update involves hundreds of hours of data validation and integration,” said Jeremy Ring, WSGS geologist and one of the map’s curators. “The accuracy of these datasets is crucial for decisions that affect exploration, permitting, and land management.”

*A Public Resource with Powerful Tools*

The map allows users to:


* Filter and query by location, field, operator, or status
* Download data within user-defined boundaries in formats including .csv, GeoJSON, and ArcGIS feature collections
* Access production data, horizontal and vertical well locations, and infrastructure footprints
* Visualize trends in field development, well density, and resource distribution

The update reinforces WSGS’s commitment to transparency and public service. All map layers and supporting data are free to access and download through the WSGS Oil and Gas Resources portal [ [link removed] ]. Users can explore statewide trends or zero in on a particular township, range, or field of interest with ease.

*Supporting Resource Management and Energy Education*

Beyond its technical capabilities, the interactive map also plays an important role in supporting Wyoming’s energy literacy. By making complex geologic and production data readily accessible, the platform enables better understanding of how oil and gas resources are developed, where infrastructure is located, and what changes have occurred over time.

“The interactive map is part of a broader mission to make geoscience more approachable and usable,” said Dr. Raul Ochoa, WSGS geologist and data reviewer for the project. “We want to give people the tools to ask informed questions and engage with the state’s energy future.”

With this latest release, the WSGS continues to provide critical infrastructure for understanding and responsibly managing Wyoming’s vast hydrocarbon resources.

Visit the WSGS website to access the interactive oil and gas map [ [link removed] ] and download the latest datasets.








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