Geology Pueblo Loop Trail Stop 2
in New Mexico · centroid 53 mi from Albuquerque
Frijoles Canyon is carved into a thick layer of volcanic ash that over time compacted into a soft rock known as tuff. This ash was deposited over 1 million years ago in two separate eruptions of the Jemez Volcano, each spewing over 600 times more ash than Mt St Helens in 1980. Tuff is a malleable rock overall and one component within the tuff, pumice, is especially susceptible to erosion by wind and water.
Using this quality of the tuff, Ancestral Pueblo people used harder rock, such as basalt found further down this canyon and under the tuff, to enlarge natural erosional cavities into human excavated openings called cavates (CAVE-eights). You will be able to climb ladders into several of these further down the trail.If you are interested in learning more about this fantastic volcanic geology, visit the Valles Caldera National Preserve located about 40 minutes away on Highway 4. The Preserve protects the collapsed top (caldera) of the Jemez Volcano.
- States
- New Mexico
- Trail type
- National Monument trail
- Centroid nearest city
- Albuquerque, NM · 53 mi · ~1.5 hr drive
- Centroid coords
- 35.7797°, -106.2716°
About Bandelier National Monument
This trail is inside Bandelier National Monument, a national monument managed by the U.S. National Park Service. Conditions, road status, trail closures, and reservation requirements are published on the park's NPS page — check it before driving in, especially in winter or during major weather events.
Entrance fee: $25 per vehicle (verify current rate on the park page). An America the Beautiful annual pass ($80) covers entrance to all NPS units.
Official NPS trail page: https://www.nps.gov/places/pueblo-loop-trail-stop-2.htm
Park homepage: https://www.nps.gov/band/index.htm
Plan your hike
Maps + permits: long-distance trails like this often require permits for through-hiking, backcountry camping, or specific sections (especially in National Parks). Check with the maintaining organisation listed above and the relevant land manager before booking travel.
Water + supplies: water sources vary seasonally on most U.S. trails. Carry a filter and consult current trail-condition reports — through-hiker journals (PCT-L, AT Reddit, etc.) and the maintaining organisation publish regular updates.
When to go: hiking seasons vary widely with elevation, latitude, and snowpack. Through-hikers traditionally start the AT in March-April (Springer northbound) and the PCT in late April (Campo northbound). High-elevation western trails (CDT, JMT, Wonderland) generally aren't passable until July.
If you've hiked Geology Pueblo Loop Trail Stop 2 and have current notes (water sources, trail closures, permit changes), tell us at /contact — we update pages as we learn.
Stay nearby
Other trails within 50 miles
Ancient Life Pueblo Loop Trail Stop 1
0 miles from this trail's centroid
Frijoles Creek Pueblo Loop Trail Stop 3
0 miles from this trail's centroid
Big Kiva Pueblo Loop Trail Stop 4
0 miles from this trail's centroid
Garden Pueblo Loop Trail Stop 5
0 miles from this trail's centroid
Native Plants Pueblo Loop Trail Stop 6
0 miles from this trail's centroid
Entering Tyuonyi Pueblo Loop Trail Stop 7
0 miles from this trail's centroid
Sources
Trail data on this page is compiled from OpenStreetMap contributors (ODbL), the maintaining organisation's public-facing materials, and Wikipedia (CC BY-SA where excerpts are quoted). Distance, terminus, and descriptive text for nationally-designated trails are hand-curated from federal land-manager websites and trail-association sources. We do not modify the underlying data; this page presents what is already publicly recorded. To suggest corrections, see our methodology page.