![]() "Fault zone structure from topography: Signatures of en echelon fault slip at Mustang Ridge on the San Andreas Fault, Monterey County, California." 2010. "Ancient sag ponds add to diversity at HREC." Web. "An upper cretaceous sag pond deposit: Implications for recognition of local seismicity and surface rupture along the Kaibab monocline, Utah." Geology. ![]() ^ Nevada-Government Dictionary on Water Words, retrieved April, 3rd 2012.^ THE SAG POND STORY - INTERPRETIVE TRAIL GUIDE, retrieved May, 9th 2017. ![]() Various lagoons on the plateau of Pico Island in the Azores are the result of a graben. Some have been converted into reservoirs like the San Andreas Reservoir near San Bruno, California. Sag ponds of various sizes can be found along the San Andreas Fault, most notably within the Carrizo Plain and Sierra Pelona Mountains. Normal faults: faults in which the hanging wall is moved. 3.The relation of the fault altitude with the altitude of the displaced bed. Larger sag ponds are converted into reservoirs for public water sources, such as San Andreas Lake Examples Classification of faults Following are the factors commonly considered important : 1.The apparent movement of the rock blocks along the fault plane. Sag ponds have been converted into stock reservoirs. Aerial photography or high-resolution topography can easily determine their locations. Sag pond formation is common in California, and many of them can be found on the San Andreas Fault, which runs through the western part of the state. When water enters the depression from rivers, streams, rainfall or snowfall, it fills the low-lying area, and a pond is the result. A strike-slip fault is one that is associated with horizontal displacement parallel to the strike of a vertical or steeply inclined fault plane. Formation Ī sag pond is formed along a strike-slip fault, which may create a depression in the earth. ( April 2020) ( Learn how and when to remove this template message)Įlizabeth Lake is one of numerous sag ponds along the San Andreas Fault.Ī sag pond is a body of fresh water collected in the lowest parts of a depression formed between two sides of an active strike-slip, transtensional or normal fault zone. You may improve this article, discuss the issue on the talk page, or create a new article, as appropriate. The examples and perspective in this article deal primarily with the United States and do not represent a worldwide view of the subject.
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