Unconformity at Frijoles Canyon in Bandelier National Monument
July 26, 2012
Photographer: Rick Scott; Rick’s Web site
Summary Author: Rick Scott
The geologic unconformity shown in this photo, taken in Frijoles Canyon at Bandelier National Monument, New Mexico, is the result of volcanic processes. The numerous thin layers had been formed by deposition from a maar volcano. They were on the order of 2 in to 6 in (5 cm to 15 cm) wide and looked like a layer cake. Initially, rising lava from the volcano encountered water causing a steam explosion. Lava and existing rock were then thrown into the air and deposited as these thin layers. The edge of the unconformity that slopes downward to the left is the surface of the volcano's crater. Rock above the crater's surface was at one time a lava pool that solidified. Above this is a layer of basalt from an overlying lava flow. Photo taken on June 21, 2012.
Photo details: Camera Maker: Canon; Camera Model: Canon PowerShot G1 X; Lens: 15.1-60.4 mm; Focal Length: 41.337mm; Focus Distance: 64.4m; Aperture: f/5.6; Exposure Time: 0.017 s (1/60); ISO equiv: 100; Exposure Bias: +0.67 EV; Metering Mode: Matrix; Exposure Mode: Manual; White Balance: Manual; Flash Fired: No (enforced); Orientation: Normal; Color Space: sRGB; Software: Adobe Photoshop CS5 Windows.