Main Stem
The main stem of White Clay Creek is formed by the junction of the West and Middle branches. From here, it enters a narrow valley and then the White Clay Creek Preserve, meeting the East Branch at Yeatman. It flows south through the White Clay Creek Preserve and enters New Castle County, Delaware and White Clay Creek State Park approximately 12 miles (19 km) west of Wilmington. Trails parallel the creek, some of them using parts of the Pomeroy & Newark roadbed, which follows the creek to the outskirts of Newark. The creek then turns away to the east, receiving Middle Run and Pike Creek. As it approaches the Christina estuary, the valley opens up, and it passes Delaware Park. Mill Creek flows into it, shortly followed by its largest tributary, Red Clay Creek. The conjoined streams turn southwest and then back to the east as they loop around Bread and Cheese Island, formed between the Red Clay, White Clay, and Hershey Run by a back channel now filled. Just after passing the island, White Clay Creek enters the Christina approximately 5 miles (8 km) southwest of Wilmington at Churchman's Marsh.
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