[at-l] Appalachian Mountains' Geologic History

David Addleton dfaddleton at gmail.com
Thu Nov 16 15:02:57 CST 2006


Looks like if you want to finish hiking ALL the appalachians, you'll have to
go down to Mexico!!

New theories and evidence:
http://us.lrd.yahoo.com/SIG=124i3jufc;_ylc=X3oDMTNrajk1NDh2BFJfYWlkAwRSX2QDaHR0cDovL3d3dy5ldXJla2FsZXJ0Lm9yZwRSX2Rpc3QDTmV3cwRSX2RtbgNldXJla2FsZXJ0Lm9yZwRSX2ZpZAM0MzMxNTA3MzRiNDJjYzY5YmZhNzdjZWMzYzc2MTc5MwRSX2x0cAMx/**http%3A//www.eurekalert.org/pub_releases/2006-11/ou-gfn111606.php

 Geologists find new origins of Appalachian Mountains Study redraws ancient
map of continents

Athens, Ohio (November 16, 2006) -- Geologists have developed a new theory
to explain how and when the Appalachian Mountain range was created. Their
research redraws the map of the planet from 420 million years ago.

The scientists recently discovered a piece of the Appalachian Mountains in
southern Mexico, a location geologists long had assumed was part of the
North American Cordillera. The Cordillera is a continuous sequence of
mountain ranges that includes the Rocky Mountains. It stretches from Alaska
to Mexico and continues into South America.

For the past decade, geologists have collected information from Mexico's
Acatlán Complex, a rock outcropping the size of Massachusetts. As they
uncovered each new piece of data from the complex, evidence contradicting
earlier assumptions about the origins of that part of Mexico emerged.

"It was a story that had the Appalachians written all over it," said Damian
Nance, Ohio University professor of geological sciences and lead author of
an article detailing the findings, which was published in the October issue
of Geology. "This will change the way geologists look at Mexico."

It also changes existing theory regarding the creation of the Appalachians,
which has radically altered scientists' understanding of the planet's
geography, said Nance. Age data, newly unearthed fossils and chemical
analysis of the rocks show that the complex is much younger than previously
thought. It records a pivotal part of the Appalachian story not preserved
elsewhere.

According to the conventional map of 420 million years ago, two main land
masses were separated by the Rheic Ocean. In the south sat Gondwana, a
supercontinent consisting of South America, Africa, India, Australia and
Antarctica. To the north was Laurussia, made up of North America, Greenland,
Europe and part of Asia. The old map showed the Acátlan Complex attached to
Laurussia. The complex broke off Gondwana about 80 million years earlier,
drifted toward North America along with the other land masses, closing an
older ocean, known as the Iapetus Ocean, as it did so. The collision created
the Appalachian Mountains.

The new map looks rather different.

Evidence collected by Nance and his colleagues from rocks in the Acatlán
Complex shows that its collision with Laurussia actually occurred about 120
million years later. The rocks once existed on an ancient ocean floor, but
this ocean has proven to be the Rheic, not Iapetus as previously thought.

The explanation, Nance and his fellow authors say, is that the Acatlán
Complex was originally attached to Gondwana. Gondwana and the complex
eventually slammed into North America, closing the Rheic Ocean in the
process. This cataclysmic crunch of continental plates formed the goliath
land mass known as Pangea, Nance said, and created the Appalachian
Mountains.

"We believe we have found the missing piece of the Rheic suture where
Gondwana and North America converged," said Nance. "All the evidence point
to that and, as far as we know, it is the best preserved piece of this
puzzle in North America."

Now geologists from around the world, funded by the United Nations
Educational, Scientific and Cultural Organization (UNESCO), are expanding
the search for evidence of the Rheic Ocean in order to unravel its history
from initial opening to final closure.

"We want to see if the ocean opened and closed everywhere at the same time
or at different times like a jaw opening and closing. We want to understand
the mechanics of these processes," said Nance.

###

The Acatlán Complex study was funded by the National Science Foundation, the
Natural Sciences and Engineering Council of Canada, the Spanish Ministry of
Education and Science and a Mexican Papiit Grant.

Brent V. Miller of Texas A&M University, J. Duncan Keppie of Universidad
Nacional Autonoma de Mexico, J. Brendan Murphy of St. Francis Xavier
University in Nova Scotia and Jaroslav Dostal of St. Mary's University in
Nova Scotia co-authored the paper appearing in Geology.


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