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Upper Colville River, Alaska

        Upper Colville Fossil Images Unassigned Fossil Images 85JTP02

 

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 Hotspot linking to Smiley's Colville and Chandler River localities.

Locality 85JTP02

As with 85JTP01 this locality is mapped as belonging to KcKt (lower part of the Killik Tongue of the Chandler Formation and Tuktu Formation undifferentiated, Chapman et al., 1964). Mull et al. (2003) reassigned this unit to the middle part of the Nanushuk Formation.

This section was given the name 'Western Horseshoe Bend' (LePain et al., 2008). The fine sands forming the 'split' in the coal seam was interpreted to represent a crevasse splay deposit. The main coal seam, which in places is as much as 3 m thick, is overlain by downlapping deltaic foresets interpreted to be a bayhead delta. Upsection, an upward-coarsening, upward-thickening sandstone unit displays well developed hummocky cross-stratification (Section 06DL005). LePain et al. (2008) interpret this as representing a transgressive deepening or lateral facies shift to fully marine lower or middle shoreface settings.

Sketch of the 85JTP02 section (slightly shortened horizontally). The red rectangle indicates the part of the section shown in the photograph below. The red line shows the approximate position of the representative sedimentary log below.   sketch of the 85JTO02 section

 

Field photograph of section at 85JTP02
 
Field photograph of the section at 85JTP02. The approximate height of the section is 20 m.
represntative sedimentary log of the 85JTP02 section   detail of the split in the coal seam at section 85JTP02

Above: detail of the split in the coal seam in the 85JTP02 section looking west.

Left: representative sedimentary log of the 85JTP02 section as measured in 1985. The coals in the section are those shown in 06DL006 below.

Section of Western Horseshow Bend  

 

 

 

 

Left: Measured sections and environmental interpretations of LePain et al. (2008).