, 1971). The area around Lily Pond was not spared human modification as the pond was created by re-sculpting
an abandoned river meander and its surrounding terrain (Galaida, 1941). The pond is flanked immediately to the north by steep, wooded slopes (up to 38° in gradient) that transition to an almost level paleovalley interfluve (at ∼280 m in elevation; Fig. 1); a small hill flanks the pond to the south (Fig. 1 and Fig. 2A). Most of the hillsides are underlain by glacial till deposits that filled a re-glacial paleovalley; a nearby creek excavated the area around Lily Pond during the Holocene before avulsing to its current position (Galaida, 1941). A walking trail around the pond’s 0.5 km-perimeter has made this locality the most frequented site within the Youngstown Metro Park system. The walking trail is Smad inhibitor partitioned from the steep forested slopes around the pond by a ∼0.5 m-tall VX-809 mouse stone retaining wall and runs along the water’s edge for most of the pond’s circumference (Fig. 2B). No perennial streams flow into the pond; water levels remain fairly constant as average annual precipitation for Youngstown (∼97 cm/yr) is distributed very evenly across the year. Since its construction the pond’s spillway
has determined pond-full level, which is just beneath the elevation of the pathway around Lily Pond’s perimeter (Fig. 2F). As there is little storage capacity at the base of the steep hillslopes surrounding the pond, materials transported during surface-runoff events are washed directly into the pond (Fig. 3). This high trap efficiency, as defined by Verstraeten and Poesen (2000), caused Lily Pond to almost completely fill up with detrital sediment by 1974, prompting the Park Service to undertake a sediment-excavation project that would re-grade the entire pond basin to a uniform 1.5-m depth with a 2:1 aspect along the perimeter. No structural changes have been made to the pond since 1974 and it has continuously filled in with materials derived from the surrounding hillslopes. As
most of the pond floor was excavated to bedrock or till in 1974, subsequent sedimentation is easy to recognize texturally and compositionally. Survey maps of the newly engineered pond floor from 1974 detail its morphology in great detail, providing a blue print for analyzing subsequent volume change SB-3CT due to sedimentation. The bedrock or till bottom at −1.5 m provides a datum for integrating the 1974 dataset with modern bathymetry measurements and measures of sediment thickness obtained from cores. The Lily Pond watershed encompasses ∼0.063 km2 of surrounding hillslopes that are vegetated predominantly with deciduous trees and little undergrowth (grasses and brush, etc.). Forest occupies ∼85% of the drainage basin and 100% of slopes in excess of 15° (Fig. 4). The average tree density across the steeply inclined terrain to the north of the pond (between 270 and 284 m in elevation) is ∼0.36/m; the tree density decreases to ∼0.