Canyon Lake Gorge is a limestone gorge in Texas, which is around 1 mile long, hundreds of yards wide, and up to 50 feet or more deep, which was exposed in 2002 when extensive flooding of the Guadalupe
Part of Canyon Lake Gorge
Waterfalls and boulders in Canyon Lake Gorge
In geomorphology, a knickpoint or nickpoint is part of a river or channel where there is a sharp change in channel bed slope, such as a waterfall or lake. Knickpoints reflect different conditions and
Canyon Lake Gorge
…the gorge are known to be associated with rapidly flowing flood water (such as the streamlined islands), other formations (such as the inner channels, knickpoints and terraces) have traditionally been interpreted through the “long ago and very slow” paradigm of geologic time in response to shifting climate or…
The Horseshoe Falls, one of the three Niagara Falls. The falls are a knickpoint, formed by slower erosion above the falls than below.
Bridalveil Fall, in Yosemite, flows over the edge of a glacially-carved hanging valley.
Dry Falls, Washington: a prehistoric knickpoint