At Coleman's Hill, the upper beds consist of yellowish, soft, gritty sandstone, containing some small calcareous fragments, a few pebbles of quartz, blotches of red shale, and fragments of sandstone with impressions of stems of plants.

This enhancement in the low momentum region compensating dehancement in the high momentum region means that positrons are trapped at vacancies and nanovoids […]

The article offered a snapshot of life in that region.

Oh, he looked pretty functioning to me.