alluvial terraces and a burned landscape near Grassy Flat I
Looking downstream onto a recent channel altering landslide at Bernard Creek.
A series of alluvial terraces stacked on the inside of the Camas Creek bend.
Gin clear water and cliffs of Idaho Batholith Granite in Impassable Canyon.
An aerial view of the Impassable Canyon.
Looking onto Wall Creek Rapid with large outcrops of Idaho Batholith Granite walls behind.
Vertical walls of metamorphic Gneiss flank the river in Lower Impassable Canyon.
Large Idaho Batholith granite boulders clog the river at Weber Rapid.
Large ramps may be the result of regional faulting throughout central Idaho.
A close-up shot of the Tappan Canyon Metamorphic Gneiss.
Looking down onto the debris flow slides at Haystack Rapid.
Drifting through dike riddled walls of Idaho Batholith Granite.
Rafting past a wall of water polished metamorphic gneiss.
Looking upstream onto fire induced the Lake Creek debris fan.
An aerial view of the initial Lake Creek debris fan in August of 2001.
Haystack and Bernard rapid prior to the Bernard Creek debris flow.
The view into the granite hear of the Impassable Canyon.
Lower Impassable Canyon is flanked by broken metamorphic rock.
An aerial view of the Orelano creek debris flow.
A view of the river near Pool camp that shows several distince alluvial terraces.
Idaho Batholith slabs in the heart of the Impassable Canyon.
The tappan canyon contace (river left downstream) between the Casto Pluton granites and metamorphic gneiss.
The alcove and watervall at Vail Cave.
Below Rattlesnake Cave, the river enters the Yellowjacke formation meta-sedimentary rocks.
