Panhole

Panholes are erosional or destructional features that are developed in a variety of climatic environments and in a wide range of rock types. These shallow basins, or closed depressions, are quite commonly well developed in surfaces of granitic rocks and sandstone. They are generally characterized by flat bottoms and sometimes by overhanging sides. The initial form may be a closed hollow created by a patch of humus. Diameters are rarely greater than 6 ft (1.8 m).[6] Some panholes were at one time thought to be man-made because their roundness was so perfect they were argued not be natural and must have been shaped by humans.[1][4]

Panholes are most commonly found in desert environments such as the Colorado Plateau. A few well-known panholes are found developed in sandstone surfaces in Canyonlands National Park, Capitol Reef National Park, and Moab. Panholes are capable of collecting water when it rains, freezing over when the weather gets cold, dry out in hotter weather, and can even contain some species of bacteria, lichens, mosses, and blue-green algae.[6] Panholes range in size from a few centimeters to many meters in diameter. The cavities can be shallow or more than 15 meters (49 ft) deep, containing hundreds of liters of water. The Australian Aboriginal term gnamma, in particular, implies a depression capable of holding water in arid areas, forming an important water resource for Aboriginal people that needed to be carefully maintained.[2][7]

Within the panholes is a varied eco-system that contains bacteria such as cyanobacteria, fungi, and algae which can be referred to as biofilm.[4] Panholes do not contain predators like fish or aquatic insects.[8] The biofilm breaks down some of the siliceous minerals in the panhole for nutrients resulting in furthering the weathering the panhole.[8] The organisms that live in the panholes have to tolerate rapid change in water temperature, pH, oxygen, carbon dioxide concentration, and ion concentration.[4]

Panholes in granodiorite at Glacier Point, Yosemite National Park, California

In the Sierra Nevada, California these features were termed weathering pits[9] by François E. Matthes, where they are thought to indicate rock surfaces that are unglaciated or escaped more recent glaciations. In Sierra Nevada granitic rocks, these features have a characteristic shape such that they expand more rapidly in width than they grow in depth.[10] One explanation for their conformation is because the most active environment for weathering is the zone of alternate wetting and drying along the margins of the pools that collect in the pits, the margins tend to deepen and enlarge until all points of the bottom are equally wet or dry at the same time, thus producing their characteristic shape.[11] Panholes can expand from weathering and erosion but the main activity of how panholes expand is from biological weathering. At one time the belief was that the only agents involved with the expansion of panholes were physical weathering.[4]