Richard F Madole (Former Employee)
Science and Products
Filter Total Items: 27
Rocky Mountains Rocky Mountains
The Rocky Mountain region is one of the most topographically distinct and impressive parts of North America. The Rocky Mountains rise abruptly above the bordering regions, particularly on the east and northeast where they are flanked by plains, less so on the west and southwest where they are bounded by high plateaus. The Rocky Mountains comprise more than 100 individually named ranges...
Authors
Richard F. Madole, W.C. Bradley, D.S. Loewenherz, D.F. Ritter, N.W. Rutter, C.E. Thorn
Lake Devlin and Pinedale glacial history, front range, Colorado Lake Devlin and Pinedale glacial history, front range, Colorado
Glacial Lake Devlin was an ice-margin lake that formed during Pinedale time when the North Boulder Creek valley glacier blocked the mouth of a tributary near the downvalley limit of glaciation. The lake was about 2 km long and as much as 60 m deep, and was fed by meltwater from small valley glaciers. It accumulated sediment, apparently without interruption, for about 10,000 yr. The...
Authors
R.F. Madole
Geology of the Pontiac Pit archeological site, Rocky Mountain National Park, Colorado Geology of the Pontiac Pit archeological site, Rocky Mountain National Park, Colorado
No abstract available.
Authors
R.F. Madole
Science and Products
Filter Total Items: 27
Rocky Mountains Rocky Mountains
The Rocky Mountain region is one of the most topographically distinct and impressive parts of North America. The Rocky Mountains rise abruptly above the bordering regions, particularly on the east and northeast where they are flanked by plains, less so on the west and southwest where they are bounded by high plateaus. The Rocky Mountains comprise more than 100 individually named ranges...
Authors
Richard F. Madole, W.C. Bradley, D.S. Loewenherz, D.F. Ritter, N.W. Rutter, C.E. Thorn
Lake Devlin and Pinedale glacial history, front range, Colorado Lake Devlin and Pinedale glacial history, front range, Colorado
Glacial Lake Devlin was an ice-margin lake that formed during Pinedale time when the North Boulder Creek valley glacier blocked the mouth of a tributary near the downvalley limit of glaciation. The lake was about 2 km long and as much as 60 m deep, and was fed by meltwater from small valley glaciers. It accumulated sediment, apparently without interruption, for about 10,000 yr. The...
Authors
R.F. Madole
Geology of the Pontiac Pit archeological site, Rocky Mountain National Park, Colorado Geology of the Pontiac Pit archeological site, Rocky Mountain National Park, Colorado
No abstract available.
Authors
R.F. Madole