over clayey gravel lying above thinly-bedded clay which in turn rests on the bed-rock of an interglacial channel. Bar- rington's camp is to the east on a gravel bench 20 to 25 feet above the creek (see Fig. 4). A rock bench, thinly covered with clay, sand and gravel lies farther east, about 40 to 45 feet above the creek. The first gold recovered by Peacock was from a ground-sluice cut in the bottom of the creek beside the low gravel bench. The gold in the clayey gravel, was recovered largely because the ground-sluice cut was bottomed by firmly-cemented gravel or thinly-bedded clay. Bed-rock was reached only at the east side of the booming-dam; there was none in the bottom of the cut. Apparently bed-rock slopes steeply westward beneath the creek. 3800 Wheaton (Boulder) Creek Rock bench N 3775 “. Late Tertiary . channel 3750 Draig-line cult Creek by-paps Se | Interglacial channel ! 3725 LEGEND Clayey gravel 4 Scale ees Feet Thinly bedded clay Sedimentary bed-rock KS Fig. 5. Cross-section along section-line A-A on Fig. 4, showing bed-rock channel beneath Wheaton Creek on the Peacock lease, and probable late Tertiary channel lying to the east of the rock bench. Later, in the autumn of 1938, rich pay-gravel was found at the south end of the lowest gravel bench (see Fig. 4). It is reported that in about 6 weeks gold valued at about $12,000.00 was recovered by hand-shovelling from about 11,000 square feet of ground. The surface sloped upward from the edge of the creek to a narrow bench intermediate in level between the low gravel bench on which Barrington's camp is built and the rock bench to the east. The gold was in clayey gravel within 2 to 3 feet of the sloping surface whereas similar gravel beneath is barren. When the ground was worked only the top gravel was shovelled into the sluice-boxes and bed-rock was encountered only at the extreme southern end of the work- ings. The pay-gravel was followed and worked up to the edge of the intermediate bench. All the work done by Peacock on lease No. 345, prior to Se