Series: National Park Service Geodiversity Atlas

NPS Geodiversity Atlas—Bandelier National Monument, New Mexico

Geodiversity refers to the full variety of natural geologic (rocks, minerals, sediments, fossils, landforms, and physical processes) and soil resources and processes that occur in the park. The NPS Geodiversity Atlas delivers information in support of education, Geoconservation, and integrated management of living (biotic) and non-living (abiotic) components of the ecosystem.

bandelier report cover with landscape image
In-depth geologic information is contained in the baseline inventory products of the Geologic Resources Inventory, see table below.

Geologic Features and Processes

The prehispanic culture that occupied Bandelier National Monument was strongly influenced by the geologic features and processes of the area. The rock that forms the majority of the mesas and sheer-walled canyons within the monument erupted from nearby Valles Caldera one to two million years ago and was a well-suited home for the Ancestral Puebloans. The volcanic tuff rock is strong enough to support steep canyons but also weak enough for the ancient people to excavate dwellings with hand tools. These canyons and mesas also supported a rich ecosystem that provided water and food. The geologic history of the area resulted in the landscape of the monument that allowed for successful early human settlement.

Bandelier is located on the west side of the Rio Grande Rift, a fault zone that is the center of both earthquake and volcanic activity.

Volcanic Landforms: Extrusive Igneous

Bandelier National Monument hosts a world-class example of welded tuff volcanic rock (National Park Service, 2005). Bandelier is located on the Pajarito Plateau and is part of a volcanic complex that has been active for over 13 million years. This volcanic complex is situated at the intersection of the Rio Grande rift and the Jemez Mountains volcanic field.

Geologically recent, large and violent volcanic eruptions dominate the geologic story of Bandelier. Between 1.61 and 1.25 million years ago, two massive explosive eruptions spewed out a combined 160 cubic miles of rock, ash, pumice, and tuff over Bandelier and the surrounding region (National Park Service, 2005).

The Bandelier Tuff - a deposit composed primarily of volcanic ash hardened by superheated gas - is the most significant rock unit at the Monument, because it is widespread and forms its unique canyon and mesa topography that was so well suited for early human occupation. The Bandelier Tuff contributed to the development of the Puebloan civilization at Bandelier, because the people were able to carve into this rock to create dwellings, they utilized its water retaining properties for farming, and the unique topography formed in this rock supports a thriving ecosystem and associated food and water resources.

Paleontological Resources

Paleontological resources at Bandelier National Monument occur in the rocks and sediments that postdate the Bandelier Tuff. Holocene terraces in the Frijoles Canyon have limited in situ fossils in these deposits, which include a packrat midden and detrital charcoal. Many packrat middens exist in the park, but the maximum ages are not completely known. One midden found in the Frijoles Canyon yielded a calibrated age of between 3,680 and 3,290 years old (Tweet et al., 2012).

All NPS fossil resources are protected under the Paleontological Resources Preservation Act of 2009 (Public Law 111-11, Title VI, Subtitle D; 16 U.S.C. §§ 470aaa - 470aaa-11).

Geohazards

Natural geologic processes continue to shape the park on time scales ranging from seconds to years. Natural materials and processes can create geologic hazards and associated risks. Be cautious and alert to geohazards that may be present in the park, including:

Flash Flooding and Debris Flows
Fire has had a tremendous effect on the landscape of Bandelier. Fires over the last two decades have led to extraordinary flooding and debris flow events that have impacted park staff, visitors, and resources such as trails, bridges, and buildings.

Rockfall
Rockfall is an ongoing process in the canyons of Bandelier and can occur sporadically or be triggered by earthquakes, frost weathering, diurnal heating and cooling cycles, or precipitation events that generally are accentuated for a time following wildfires. Rockfall could impact virtually all park facilities located in canyons, could impact cultural resources and is a significant safety concern.

Seismic Activity
The Pajarito Fault is a major active fault located within Bandelier. This fault and others located along the western margin of the Rio Grande Rift are capable of generating earthquakes greater than magnitude 5.0. The U.S. Geological Survey estimates the probability of a magnitude 5.0 earthquake or greater in the next century at more than 50%. An earthquake of this size or greater near Bandelier would cause significant damage to park facilities and likely widespread rockfall in the canyons.

Geology FieldNotes

Students and teachers of college-level (or AP) introductory geology or earth science teaching courses will find that each park's Geologic Resource Inventory report includes the Geologic History, Geologic Setting, and Geologic Features & Processes for the park which provides a useful summary of their overall geologic story. See Maps and Reports, below.

Regional Geology

Bandelier is a part of the Rocky Mountain System Physiographic Province and shares its geologic history and some characteristic geologic formations with a region that extends well beyond park boundaries.

link to geologic map

Maps and Reports

Geologic Resources Inventory

The Geologic Resources Inventory produces digital geologic maps and reports for more than 270 natural resource parks. The products listed below are currently available for this park, check back often for updates as many maps, reports, and posters are still in progress.
  • Scoping summaries are records of scoping meetings where NPS staff and local geologists determined the park’s geologic mapping plan and what content should be included in the report.
  • Digital geologic maps include files for viewing in GIS software, a guide to using the data, and a document with ancillary map information. Newer products also include data viewable in Google Earth and online map services.
  • Reports use the maps to discuss the park’s setting and significance, notable geologic features and processes, geologic resource management issues, and geologic history.
  • Posters are a static view of the GIS data in PDF format. Newer posters include aerial imagery or shaded relief and other park information. They are also included with the reports.
  • Projects list basic information about the program and all products available for a park.

Source: Data Store Saved Search 2714. To search for additional information, visit the Data Store.

Soil Resources inventory

NPS Soil Resources Inventory project has been completed for Bandelier National Monument and can be found on the NPS Data Store.

Source: Data Store Saved Search 2781. To search for additional information, visit the Data Store.

ruins carved into the rock with cliff towering above
The Tshirege Member of the Bandelier Tuff, shown here at Long House in Frijoles Canyon, contains natural cavities that ancient people further excavated, making cavates for habitation and storage. (Photograph © George H. H. Huey)

Related Links

Related Articles

Bandelier National Monument

National Park Service Geodiversity Atlas

The servicewide Geodiversity Atlas provides information on geoheritge and geodiversity resources and values within the National Park System. This information supports science-based geoconservation and interpretation in the NPS, as well as STEM education in schools, museums, and field camps. The NPS Geologic Resources Division and many parks work with National and International geoconservation communities to ensure that NPS abiotic resources are managed using the highest standards and best practices available.

For more information on the NPS Geodiversity Atlas, contact us.