scholarly journals Trainees and Instructors at the WV Division of Forestry's 1963 Forest Fire Training School Held at the Cabwaylingo State Forest, Wayne County, West Virginia

2014 ◽  
Vol 112 (2) ◽  
pp. 241-241
Author(s):  
Robert L. Beanblossum
Keyword(s):  
West Virginia ◽  
Forest Fire ◽  
Training School ◽  
Wayne County

A Synoptic Climatology for Forest-Fires in the NE US and Future Implications From GCM Simulations

1994 ◽  
Vol 4 (4) ◽  
pp. 217 ◽  
Author(s):  
ES Takle ◽  
DJ Bramer ◽  
WE Heilman ◽  
MR Thompson
Keyword(s):  
West Virginia ◽  
Forest Fire ◽  
Surface Pressure ◽  
Forest Fires ◽  
Circulation Model ◽  
Synoptic Climatology ◽  
Global Circulation Model ◽  
Weather Patterns ◽  
Forest Fire Danger ◽  
Drying Conditions

We studied surface-pressure patterns corresponding to reduced precipitation, high evaporation potential, and enhanced forest-fire danger for West Virginia, which experienced extensive forest-fire damage in November 1987. From five years of daily weather maps we identified eight weather patterns that describe distinctive flow situations throughout the year. Map patterns labeled extended-high, back-of-high, and pre-high were the most frequently occurring patterns that accompany forest fires in West Virginia and the nearby four-stare region. Of these, back-of-high accounted for a disproportionately large amount of fire-related damage. Examination of evaporation acid precipitation data showed that these three patterns and high-to-the-south patterns ail led to drying conditions and all other patterns led to moistening conditions. Surface-pressure fields generated by the Canadian Climate Centre global circulation model for simulations of the present (1xCO2) climate and 2xCO2 climate were studied to determine whether forest-fire potential would change under increased atmospheric CO2. The analysis showed a tendency for increased frequency of drying in the NE US, but the results were not statistically significant.

Limnopus trackways from the Conemaugh Group (Late Pennsylvanian), southern West Virginia

1991 ◽  
Vol 65 (6) ◽  
pp. 957-972 ◽  
Author(s):  
Ronald L. Martino
Keyword(s):  
West Virginia ◽  
Subtropical Climate ◽  
Plant Debris ◽  
Mean Values ◽  
Wayne County ◽  
Delta Plain ◽  
Total Length ◽  
Glenshaw Formation ◽  
Channel Systems ◽  
Stratigraphic Interval

Abundant and well-preserved tetrapod footprints have been discovered in the Glenshaw Formation (Lower Conemaugh Group) in Wayne County, West Virginia. The tracks occur along at least three horizons within a 30-cm-thick stratigraphic interval about 15 m (50 ft) above the Brush Creek Limestone; they are of Missourian age. The tracks are preserved mainly as casts on the underside of thin-bedded, ripple cross-laminated sandstones and less commonly as molds in intervening dark-gray shales. Associated body fossils include Spirorbis worm tubes and washed-in plant debris. Facies characteristics indicate the tracks were formed along the margins of an ephemeral lake in a flood basin setting adjacent to delta plain fluviodeltaic channel systems. Short-lived lacustrine conditions were likely to have resulted from a seasonal tropical to subtropical climate.Most of the tracks can be assigned to the ichnogenus Limnopus, making them one of the earliest known occurrences. At least five trackways are discernible with an external width ranging from 320 to 400 mm. Limnopus glenshawensis, a new ichnospecies, is herein proposed and various morphologic and locomotion parameters are quantified. Mean values include stride/manus, 407 mm; stride/pes, 411 mm; oblique pace/manus, 313 mm; oblique pace/pes, 317 mm; pace angle/manus, 82.4 degrees; pace angle/pes, 80.5 degrees; glenoacetabular distance, 329 mm; manus length, 87.2 mm; manus width, 104.2 mm; pes length, 121.4 mm; pes width, 112.7 mm. The tracemaker was most likely an eryopoid amphibian with a total length of slightly over 1 m.

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