Garry Denke
G-D
2nd February 2003
Doctor Garry Denke (1656) first proposed the two (2) horseshoes in the central part of Stonehenge were not two (2) horseshoes, because the ancients had neither horses, nor horseshoes. The German dentist first proposed the ancient builders were modeling their male open mouth (larger) and female open mouth (smaller), human teeth:
for the purpose of passing on knowledge of the ancient white fossils by "word of mouth", theirs. Doctor Anthony Perks' (2002) genitilia proposal makes more sense than the two (2) horseshoes theory of British archaeologists, considering the ancients had neither horses, nor horseshoes; but Doctor Garry Denke's (1656) "word of mouth" rules:
Chronology of Stonehenge Construction Materials
First (1st) Discovered by Dr. Garry Denke (1656):
The oldest limestone sedimentary rocks at Stonehenge are the Early Carboniferous Period, Arundian Age, calcium carbonates. The Early Carboniferous Period limestone sedimentary rocks comprise the first (1st) foreign construction material used by the Stonehenge builder. This material is approximately 340 million years old. These rocks are locally called the Birnbeck Limestone Formation (Stonehenge Whitestones).
The outcrop sedimentary rocks at Stonehenge are the Late Cretaceous Period, Santonian Age, calcium carbonates. The Late Cretaceous Period outcrop sedimentary rocks comprise the first (1st) local [in situ] construction material used by the Stonehenge builders. This material is approximately 85 million years old. These rocks are locally called the Seaford Chalk Formation (Stonehenge White Chalk).
The volcanic rocks (oldest geologically) at Stonehenge are the Ordovician Period intrusive igneous diabases (dolerites), and extrusive igneous felsites (rhyolites) and tuffs (basic). The Ordovician Period igneous rocks comprise the second (2nd) foreign construction material used by the Stonehenge builders. This material is approximately 470 million years old. These rocks are locally called the Ordovician Volcanics (Stonehenge Bluestones).
The oldest sandstone sedimentary rocks at Stonehenge are the Silurian - Devonian Period micaceous sandstones. The Silurian - Devonian Period sedimentary sandstone rocks comprise the third (3rd) foreign construction material used by the Stonehenge builders. This material is approximately 417 million years old. These rocks are locally called the Old Red Sandstone Formation (Stonehenge Coshestons).
The youngest sandstone sedimentary rocks at Stonehenge are the Oligocene - Miocene Period silicates. The Oligocene - Miocene Period sandstone sedimentary rocks comprise the fourth (4th) foreign construction material used by the Stonehenge builders. This material is approximately 24 million years old. These rocks are locally called the Reading Formation (Stonehenge Sarsens).
http://www.bgs.ac.uk/education/britstrat/timecharts/phaner.html
"The ancients had dental (lintel) bridges too."
Kind regards,
Garry W. Denke
Geologist/Geophysicist
Doctor Garry Denke (1656) first proposed the two (2) horseshoes in the central part of Stonehenge were not two (2) horseshoes, because the ancients had neither horses, nor horseshoes. The German dentist first proposed the ancient builders were modeling their male open mouth (larger) and female open mouth (smaller), human teeth:

for the purpose of passing on knowledge of the ancient white fossils by "word of mouth", theirs. Doctor Anthony Perks' (2002) genitilia proposal makes more sense than the two (2) horseshoes theory of British archaeologists, considering the ancients had neither horses, nor horseshoes; but Doctor Garry Denke's (1656) "word of mouth" rules:

Chronology of Stonehenge Construction Materials
First (1st) Discovered by Dr. Garry Denke (1656):
The oldest limestone sedimentary rocks at Stonehenge are the Early Carboniferous Period, Arundian Age, calcium carbonates. The Early Carboniferous Period limestone sedimentary rocks comprise the first (1st) foreign construction material used by the Stonehenge builder. This material is approximately 340 million years old. These rocks are locally called the Birnbeck Limestone Formation (Stonehenge Whitestones).
The outcrop sedimentary rocks at Stonehenge are the Late Cretaceous Period, Santonian Age, calcium carbonates. The Late Cretaceous Period outcrop sedimentary rocks comprise the first (1st) local [in situ] construction material used by the Stonehenge builders. This material is approximately 85 million years old. These rocks are locally called the Seaford Chalk Formation (Stonehenge White Chalk).
The volcanic rocks (oldest geologically) at Stonehenge are the Ordovician Period intrusive igneous diabases (dolerites), and extrusive igneous felsites (rhyolites) and tuffs (basic). The Ordovician Period igneous rocks comprise the second (2nd) foreign construction material used by the Stonehenge builders. This material is approximately 470 million years old. These rocks are locally called the Ordovician Volcanics (Stonehenge Bluestones).
The oldest sandstone sedimentary rocks at Stonehenge are the Silurian - Devonian Period micaceous sandstones. The Silurian - Devonian Period sedimentary sandstone rocks comprise the third (3rd) foreign construction material used by the Stonehenge builders. This material is approximately 417 million years old. These rocks are locally called the Old Red Sandstone Formation (Stonehenge Coshestons).
The youngest sandstone sedimentary rocks at Stonehenge are the Oligocene - Miocene Period silicates. The Oligocene - Miocene Period sandstone sedimentary rocks comprise the fourth (4th) foreign construction material used by the Stonehenge builders. This material is approximately 24 million years old. These rocks are locally called the Reading Formation (Stonehenge Sarsens).
http://www.bgs.ac.uk/education/britstrat/timecharts/phaner.html
"The ancients had dental (lintel) bridges too."
Kind regards,
Garry W. Denke
Geologist/Geophysicist