|The earth movements that affected the Appalachian Mountains after the Taconic Orogeny USGS|
Tuesday, June 12, 2012
Tales of the Devil: Origin of the Rowe Schist
During the late Cambrian and early Ordovician a series of turbidite flows came down the continental slope of the North American craton. This was the origin of the Roweschist formation. Turbidites are also good sources of gold ore. There are several examples of this kind of formation worldwide with the Witwatersrand of South Africa being the most notable. Much of the gold ore from
is another example as are many of the deposits of the world. To date the Timmins, ON Witwatersrand
has produced around 40% of the entire world’s gold supply in the past 40
years. The gold mines found here are
some of the deepest in the world that now are approaching 13,000 feet deep.
Earth movements associated with the Taconic Orogeny during the late Ordovician caused this layer of turbidite to be shoved to its present location close to the Iapetus Suture zone that locally in
and New York is called Cameron’s
Line under differing names it reaches to the mountains of western Norway. It is truly one of the largest suture zones
on earth. By definition a suture zone is
also a subduction zone where rocks of oceanic origin are forced under the
continental margin. Cameron’s Line is
about two miles west of the Rowe schist the formation that underlies the
property belonging to the finder of the Whodunit Mine.
According to the USGS the following illustration graphically explains the Taconic Orogeny an Alpino type orogeny, a long narrow belt of mountains that formed the Taconic mountain range. This is the orogeny that initiated the first of several mountain building events that occurred in the
Appalachians. This is the
orogeny that had the greatest effect on the Litchfield site.
The site itself is composed of a series of turbidite flows that flowed down the continental slope into a back arc basin behind the island arc. This was composed of the sand and mud component illustrated in the first of the illustrations shown of the below diagram. The Hoosac Schist on the landward side of Cameron’s line is represented by the portion marked sand. The continental crust is represented by the Precambrian rock north and west of the site on the landward side of Cameron’s Line.
Cameron’s Line is where the Hoosac schist and the portion marked sediment meet in a long suture line that extends from
that was broken in
half after the Staten
Island, NY Atlantic Ocean opened during the Mesozoic
and after passing through Ireland,
eventually ends in the mountains of northern Norway.
When the Taconic Orogeny ended the mountains that rivaled the
Himalayas in height were completely eroded away to a
flat plain we know as a peneplain. There
were small mountain building events that occurred during the Silurian that
although they affected the local area were so small as to be hardly noticed. The next big event that affected the eastern
seaboard occurred during the Devonian called the Acadian Orogeny.
The Acadian Orogeny produced a different type of mountain range that was much broader then the Taconic Orogeny that to geologists is a Hercyanian type orogeny that was caused when
sideswiped the North American Continent.
It was during this event that the Rowe schist was intruded with molten
magma causing it to become a type of rock called granofels. This action caused many secondary minerals to
be deposited in the schist ilmenite being the most prominent. The event also caused further deformation to
the Rowe schist.
At the end of this orogeny the Rowe schist has stayed above sea level unlike at the end of the Taconic orogeny as the rocks were eroded smooth the ocean came back to cover the land with ocean water.
For the most part the only Orogenies that affected the local area were the Taconic, the Silurian (?) and the Devonian. The later Orogenies affected the lands to the south and east.