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The watershed contains a dendritic drainage pattern which indicates homogenous subsurface strata of the study area.
The output slope grid of Makhawan watershed contains values representing degree of slope from 0° to 11°, with a mean slope of 1.10° and slope standard deviation is 0.16°.
But the watershed contains just one-tenth of the state's known gas deposits.
The one million acres northwest of New York City that comprise the watershed contain less than one-tenth of the rich deposits of natural gas lodged in the state's portion of the Marcellus Shale, a thick subterranean layer of rock that runs from West Virginia to New York.
The Dehgolan watershed contains both mountains and plains.
However, the Cranberry Creek watershed contains 6.5 percent barren land, the Black Creek watershed contains 14 percent, and the Stony Creek watershed contains 30 percent.
The Little Nescopeck Creek watershed contains 30 percent farmland and the Nescopeck Creek watershed contains 24 percent.
Nescopeck Creek's watershed contains several major rock formations.
Approximately 24 percent of the creek's watershed contains the Wellsboro-Oquaga-Morris series.
The lower stretches of the watershed contain soils such as decomposed lavas, clay, and gravel.
The watershed contains the largest groundwater source in the entire Rogue River basin; one major outlet is at Big Butte Springs.
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