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Upper Colville River, Alaska

        Upper Colville Fossil Images Unassigned No Images for 85JTP04

 

This interactive map of part of the Colville River, Northern Alaska, shows the locations of plant fossil collections made by J.T. Parrish and R.A. Spicer in 1985 and 1989. Click on a number for more details on that site. The red outlined area links to another map showing positions of florules (plant fossil assemblages) collected by C.J. Smiley along both the Colville and Chandler Rivers.

Interactive map of the Upper Colville River Hotspot linking to 85RAS09 Hotspot linking to Smiley's Colville and Chandler River localities. Hotspot linking to 85RAS02 Hotspot linking to 85RAS01 Hotspot linking to 85RAS03 Hotspot linking to 85RAS04 Hotspot linking to 85RAS05 Hotspot linking to 85RAS06 Hotspot linking to 85RAS07  Hotspot linking to 85RAS08 Hotspot linking to 85RAS10 Hotspot linking to 85RAS11 Hotspot linking to 85RAS12 Hotspot linking to 85RAS13 Hotspot linking to 85RAS14 Hotspot linking to 85RAS13 Hotspot linking to 85RAS16 Hotspot linking to 85RAS17 Hotspot linking to 85RAS18 Hotspot linking to 85RAS19 Hotspot linking to 89RAS1_3 Hotspot linking to 89RAS04 Hotspot linking to 89RAS05 Hotspot linking to 89RAS06 Hotspot linking to 89RAS07 Hotspot linking to 89RAS09 Hotspot linking to 89RAS10 Hotspot linking to 89RAS11 Hotspot linking to 89RAS12 Hotspot linking to 89RAS164_320

Locality 85JTP04

This locality is on the south side of the Colville River just downstream of the mouth of Kucher Creek. Exposures are mapped as representing the marine Tuktu Formation of Chapman et al. (1964). The section, as logged by J.T. Parrish in July 1985, is as follows:

Top of section    
  0.3 m Gray fine to very fine sandstone with coarse sand-pebble grains incorporated. These form a basal lag in places, with mud rip ups and bivalves. No inocermid debris was seen.
  0.05 m Claystone
  0.25 m Indurated white-weathering gray claystone
  0.05 m Gray claystone
  8 m Green fine sandstone, orange-weathering in some horizons. Parallel current laminations, cross-bedded near the top. Rare pebbles in float below the upper part of the section. The sand coarsens to medium-grained where the cross beds become more pronounced and contains abundant plant debris.
Base of section