This terraced section of the valley ends at a fault scarp, marking the edge of the subsiding Ghab Basin (a segment of the Dead Sea Fault Zone), which has been filled to a depth of ~ 1 km by dominantly lacustrine sediments of Pliocene–Quaternary age.
This mechanism indicates that a pull-apart basin, marking a segment boundary of the NAF, is developing there.
A diagnostic state-and-transition framework offers a parsimonious strategy to quantitatively or qualitatively anticipate the influence of water, sediment, and ecological fluxes on channel evolution at the basin, reach, or segment scale.
Another already-known structural element is the Ganos Fault (Şengör, 1979) located to the southern part of the basin, constituting a segment of the active and dextral North Anatolian Fault Zone (Ketin, 1969; Jackson and McKenzie, 1988; Barka, 1992).
The studied basin was then segmented by means of a fuzzy k-means classification algorithm into different spatial subdomains characterized by specific local geomorphic signatures.
For quantitative analysis of the watershed involving various components such as stream segments, basin perimeter, basin area, elevation difference, slope and profile of land has been responsible for the natural development of basin (Horton 1945).
To the east of the basin, the Yalova–Hersek segment of NAF goes through the Gulf of Izmit extending between Çınarcık basin and Hersek delta (Okyar et al. 2008).
In addition to the Loihi clone, other related SSU rRNA gene signatures have been observed from deep-sea hydrothermal systems, including the Guaymas Basin [36], the Cleft Segment hydrothermal system off the coast of Oregon [37], and the Mariana Trench in the western Pacific.
These basins form the northern segment of the Ural African transcontinental oil and gas belt, a belt characterized by a high concentration of hydrocarbon deposits.
Drainage density (Dd) is described as an expression of the closeness of spacing of channels and quantitatively obtained by the ratio of total channel segment lengths within a basin over the basin area (Horton 1945; Strahler 1964).
