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Little Wood River Dam was constructed during 1936-1939 and is located 11 miles NW of Carey, Idaho.
Built in 1918 by Shell, the Wood River Refinery is now owned by ConocoPhillips and Cenovus Energy.Their joint venture company WRB Refining operates the refinery.
The rehabilitation work that was done on the dam included raising the dam crest 39 feet, extending the outlet tunnel downstream 150 feet, and relocating the spillway from right to left abutment. The completed structure has a structural height of 129 feet high, with a zoned earthfill embankment containing about 959,000 cubic yards of material.
Outlet works reconstruction included enlargement of the entrance channel to the existing intake structure, construction of a gate chamber with a connecting 6-foot-diameter access shaft and shaft house in the existing tunnel approximately 250 feet downstream from the intake structure, extension of the existing tunnel with a 150-foot-long, 6- by 8-foot conduit and a 60-foot-long, 6- by 10-foot chute, and excavation of a stilling basin in the outlet channel. At higher elevations trees appear singly or in scattered groups, but not as continuous forest.Sedimentary rocks, which range in age from very old to moderately young, are found at higher elevations.

During geologically recent time, intracanyon basalt flows have covered the valley floor and they are the youngest formations. In the vicinity of the reservoir, the river flows along the contact of the intracanyon basalts and the older volcanic rocks.
The intracanyon basalt flows terminate several miles below the present The soil throughout the basin is a silty clay loam and appeared to be thin in depth and rocky in nature. The estimated depth of the soil mantel is 6 to 12 inches.The basin of the Little Wood River is a part of a region of very complex geology. A synopsis of this information follows:Sedimentary deposits of sandstone with interbedded conglomerate and limestone (designated the Wood River formation), shale with interbedded blue limestone and quartzite (designated the Milligen formation) and extensive flows of andesite underlie most of the drainage. Metamorphosed limestone, quartzite and schist occupy a small area on the extreme northwest divide and an olivine basalt flow in the vicinity of the Little Wood Reservoir covers a considerable area.

The entire region has been subjected to extensive uplift, folding and faulting with considerable igneous intrusion. The headwaters area of the main stem and its minor tributaries have been subjected to some glacial action.

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