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CSI/CUNY News Release |
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For Immediate Release |
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New mineral discovered in NYS
to be displayed by NY State Museum and Smithsonian Institute
Staten
Island, NY – March 15, 2004 -- The Commission on New Minerals
and Mineral Names (CNMMN) and the International Mineralogical
Association (IMA) approved the classification of a new
manganese-rich silicic edenite mineral named parvo-mangano-edenite.
The discovery of this new mineral from a talc
mine in St. Lawrence County adds more evidence supporting the theory
that this area in upstate New York just northeast of Lake Ontario
was covered by sub-tropical shallow seas approximately one billion
years ago.
Dr. Alan Benimoff, of The City University of
New York’s College of Staten Island, is part of an international
six-member team of geoscientists that discovered the new mineral in
the Grenville Marble section of Fowler, New York, after nearly a
decade of research.
“Being a geologist is like being a detective,”
said Benimoff. “A rock is not just a rock. It’s a collection of
clues that tell us about the formation and history of the earth.”
MAJOR BREAKTHROUGH
So how does one go about discovering a new
mineral? "It's very simple," states Benimoff. "We have a database of
all known minerals, and if you can't fit your mineral in it, then
you have probably discovered a new one." Benimoff's new silicate
mineral is an amphibole, meaning it consists of double chains of
silicon and oxygen molecules joined to manganese and iron, as well
as other ions.
The difficult part of Benimoff’s “very simple”
process is distinguishing the sample mineral compound from countless
others with similar compositions.
X-RAY SPECS
The research involves using powerful and
precise electronic microscopes, X-Ray Diffraction (XRD) and single
crystal X-Ray techniques. The technological advances over the past
decade have made it possible for geologists to critically analyze
these materials and their composition.
According to Benimoff, XRD equipment
effectively creates a “fingerprint” of inorganic matter, allowing
scientists and researchers to distinguish minute differences in the
material’s structure and composition.
This new amphibole mineral is also metamorphic,
as it was altered through intense heat and pressure along a tectonic
fault-line when continental plates collided. This particular event
in New York State’s history is referred to as the Grenville Mountain
Building Episode.
WATER WORLD
The mineral makeup suggests it was formed in
shallow water, but the mountainous region found there today hints of
dramatic change to the landscape during the last billion years. An
odd component of the mineral is its 10 percent manganese content and
only 0.3 percent iron content. So much manganese compared to so
little iron is “peculiar” for an amphibole of this variety,
according to Benimoff.
Further study of this mineral will give
geologists more clues of the Precambrian Era, an era long before
dinosaurs walked the Earth, when life forms were merely simple,
single-celled organisms.
WORLD AS LABORATORY
As an undergraduate student, Benimoff majored
in engineering science. A field trip changed the course of his life
by igniting his passion for geology and its enduring sense of
discovery. He was so taken by the Earth, and the stories it hid
within its rocks, that he changed his major to geology.
Today, Benimoff leads the field trips.
Recently, he and 14 students studied the fossils found in the floor
of the Staten Island Mall, in New York City. Although the age of the
floor is still being investigated by Benimoff, it clearly contains
ancient sea creatures that lived during the Phanerozoic era.
"What we have here is a living museum," he said
of the 1.2 square-foot shopping center. "There are so many
invertebrate remains in this limestone, it's a budding geologist's
dream come true.”
ROCK SOLID FOUNDATION
Benimoff credits his engineering science
background with giving him the knowledge base to really study
geology, and he is quick to remind his students that “geologic
research [also] involves using calculus, material science, physics
and chemistry.”
Other upcoming field trips and research
expeditions for Benimoff and his students include the Smithsonian
Institute in Washington DC, and the Pioneer Coal Mine in Ashland,
PA, both of which are designed to help give the students a sense of
the real-world application and relevance of geology, according to
Benimoff.
“Being a geologist is hands-on, dirty work, and
very rewarding” said Benimoff, who is also the executive secretary
of the New York State Geological Association. “I enjoy my work here
at the College of Staten Island. I have a passion for geology and I
try to relay that passion to my students.”
MUSEUM MATTERS
Samples of the newly identified mineral will become part of the
collections of the New York State Museum and the Smithsonian
Institute in Washington, DC.
EDITOR’S NOTE: Photography available. For more
information visit www.csinews.net or contact Ken Bach at
718-982-2328. Members of the international team credited with the
classification of the new mineral include Dr. Alan Benimoff, adjunct
associate professor and chief college laboratory technician with the
engineering science and physics department at the College of Staten
Island of The City University of New York; Roberta Oberti and
Fernando Camara, CNR-Instituto di Geoscienze e Georisorse, Pavia,
Italy; George R. Rossman, California Institute of Technology,
Pasadena CA; Giancarlo Della Ventura, Dipartimento di Scienze
Geologiche, Università di Roma Tre, Rome, Italy; and Gianluca Iezzi,
Bayerisches Geoinstitut, Universität Bayreuth, Bayreuth, Germany.
The College of Staten Island (CSI) is a senior college of The City
University of New York (CUNY), the nation’s leading urban
university. CSI offers 35 academic programs, 15 graduate degree
programs, and challenging doctoral programs to 12,000 students.
The 204-acre landscaped campus of CSI, the largest in NYC, is fully
accessible and contains an advanced, networked infrastructure to
support technology-based teaching, learning, and research. For more
information, visit www.csi.cuny.edu
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