The dry and sandy gravel roads have less intense colors than the asphalt of I-25. In this image these gravel roads appear white. Road 104 runs in front of Orlando Reservoir Number 2 in the right corner of the photo. The northwest edge of Orlando Reservoir is white, which reflects the high levels of built-up sand. With the increase of sediment deposits, the reservoir turns to lighter blue tones.
Pristine water is black.
Shallow water reflects the material in its bottom. North is at the top of the photo. North is at the top of the photo. Acknowledgments I thank Dr. Brian Penn, Department of Geological Sciences, University of Texas at El Paso, with dating and general interpretation and Shelly Veatch for field assistance. Prentice Hall, New Jersey, p 140.