“…By walking the perimeter of the vernal pool, we also confirmed there were no visible inflow or outflow channels that potentially could connect to a wetland, river, or stream. Basin area, perimeter shape, maximum water depth (< 0.3 m, 0.3 -1.0 m, and >1.0 m), surrounding upland slope, and aspect were collected for each pool Previant and Nagel 2014;. Following Coburn (2004), each vernal pool was assigned an initial hydrological class based on when the basin was filled (spring or fall) and length of flooding duration (semi-permanent, short-or long-cycle).…”