Re: Stonehenge Coal Trend

Now that Timothy Darvill, archaeologist and Geoffrey Wainwright,
archaeologist have confirmed Bluestone rock located at Stonehenge is a
glacial erratic from inside South Wales Coalfield as discovered by
German historian, antiquarian, and dentist, Doctor Garry Whilhelm
Denke (1622-1699). Summer of '56, here are more geological,
paleontological, and geophysical papers from their reading list.

1) Denke, G.W. 1973. Stonehenge Phase I: An Openpit Coalfield Model;
The First Geologic Mining School. (Indiana University of Pennsylvania)
GDG, 73: 1-56.
2) Denke, G.W. 1975. Invertibrate Paleontology of the High Tor
Limestone (Lower Carboniferous) and the Upper Senonian Chalk (Late
Cretaceous) of Stonehenge. (Arizona State University) GDG, 75: 1-7.
3) Denke, G.W. 1977. Possible Source Areas of the High Tor Limestone
(Early Mississippian) Fill of the Aubrey Holes and Heel Stone Ditch in
Europe. (Arizona State University) GDG, 77: 1-24.
4) Beus, S.S. 1984. Fossil Associations in the High Tor Limestone
(Lower Carboniferous) of South Wales. (Northern Arizona University)
Journal of Paleontology, 58: 3; 651-667.
5) Denke, G.W. 1984. Mid-Dinantian (Waulsortian Facies) High Tor
Limestone: The First Stones Transported to Stonehenge from the South
Wales Coast. (Arizona State University) GDG, 84: 1-4.
6) Denke, G. 1984. Magnetic and Electromagnetic Surveys at Heelstone,
Stonehenge, United Kingdom. (Indiana University of Pennsylvania) GDG,
84: 5-42.
7) Lees, A. and Miller, J. 1985. Facies variatian in Waulsortian
buildups, Part 2; Mid-Dinantian buildups from Europe and North
America. (Revised) Geological Journal, 20: 159-180.

http://www.archaeology.co.uk/index.php?option=com_content&task=view&id=402&Itemid=26

Archaeology is a fascinating subject. Enjoy.

GDenke
.

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