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the Dome wildfire in BNM burned 16,516 acres in and near Capulin Canyon and the surrounding Dome Wilderness area. Both Frijoles and Capulin Canyon watersheds are characterized by archeological artifacts that could be affected by increased runoff and accelerated rates of erosion, which typically occur after a fire. In response to this concern, the U.S. Geological Survey (USGS), in cooperation with the National Park Service, conducted a study to monitor and document the wildfire effects on streamflow after the 1996 Dome fire. Post-fire hydrologic changes have been observed, but not often documented, for wildfires in Arizona, California, Idaho, Montana, New Mexico, and Wyoming. In 1996, the Hondo fire near Taos, New Mexico; the Buffalo Creek fire near Denver, Colorado; a fire in the Jicarilla Apache Reservation, New Mexico; and a fire in Mesa Verde National Monument all caused large increases in the magnitude of storm flows. In general, after each fire, peak flows increased, erosion and corresponding sediment transport increased, and channel geometry changed. This Fact Sheet summarizes the effects of the 1977 La Mesa wildfire on the

Effects of wildfire on the hydrology of Frijoles and Capulin canyons in and near Bandelier National Monument, New Mexico