Arthur Nelson went to the Kings River in and around Lemoore, CA to collect rock samples. The Kings River starts in the Sierra Nevada and splits into multiple forks before flowing through an artificial channel into the Tulare Lake bed, providing irrigation water. Nelson found and described several rock samples, including conglomerate made of cemented smaller rocks, likely jasper which is red from iron oxide, potassium feldspar which has two cleavage planes at 90 degrees, gneiss which is foliated and metamorphosed, and quartz monzonite which is an intrusive igneous rock with quartz, biotite and hornblende.