| | Tectonic History of Paleocene Coal Basins (Site not responding. Last check: 2007-10-21) |
 | | In early Paleocene time, about 65 million years ago, the north side of the future basin began to accumulate sediments at a faster rate than the south side, because of uplifting of the Granite Mountains to the south. |
 | | By middle Paleocene time, the Wind River basin began accumulating a thick succession of lake sediments on its north side as the basin was rapidly depressed due to crustal loading from thrust faulting along its northern margin. |
 | | Later, during the late Paleocene, the Wind River basin accumulated an even thicker wedge of lake sediments, but during this phase of development, the lake bordered the thrust-faulted margin of the growing Owl Creek Mountains. |
| energy.cr.usgs.gov /coal_poster/tertiary/tect.hist.html (401 words) |