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DTSTART:20070311T020000
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UID:94acc74f-5613-4e96-8194-4ae00d95e2aa.234508@calendar.missouristate.edu
CREATED:20240228T194232Z
LAST-MODIFIED:20240228T194232Z
LOCATION:Roy Blunt Hall 345
SUMMARY:SEES Seminar: "How Gravitation and Heat Transfer Regulate Plate Te
 ctonics and Earth's Thermal Evolution"
DESCRIPTION:Near-surface motions of Earth's plate are made possible by the
  cold\, brittle lithosphere being underlain by a weak low-velocity zone (
 LVZ). The thermal states of both layers result from the leakage of Earth'
 s internal radiogenic heat to space. But to move the plates laterally req
 uires lateral forces. We propose that force imbalances arising in the uni
 que 3-body-Earth-Moon-Sun system are the main cause of complexity in thes
 e large-scale\, cooperative tectonic motions. Comparing rocky planets sho
 ws that the presence and longevity of volcanism and tectonism depend on t
 he particular combination of moon size\, moon orbital orientation\, proxi
 mity to the Sun\, and rates of body spin and cooling. Earth is the only r
 ocky planet with all the factors needed for plate tectonics. She will exp
 lain that because the lunar orbit is becoming more elliptical\, rather th
 an growing\, plate tectonics is ancient.\n\n\nDr. Anne M. Hofmeister obta
 ined her BS with highest honors in Physics and Literature - Harvey Mudd C
 ollege\, MS in Physics - University of Illinois\, PhD in Geology - Caltec
 h. She has experience with spectroscipic measurements of minerals\, was a
  postdoctoral associate and fellow at the Geophysical Laboratory performi
 ng high-pressure measurements under the supervision of Ho-Kwang Mao. She 
 was an assistant professor and associate professor at U.C. Davis\, includ
 ing a David and Lucille Packard Fellowship. She also completed a brief sa
 bbatical as a Humbolt Fellow at the Max Planck Institute in Mainz\, Germa
 ny\, where she studied with Reinhard Boehler.\n\n\nCurrently\, she conduc
 ts research in several areas at the Earth and Planetary Science Departmen
 t at Washington University in St. Louis. Her research includes: Optical a
 nd infrared spectroscopy with collaborative application to astronomy to b
 etter understand the mechanism of heat transfer\; Measurement and modelli
 ng of heat transport and thermodynamic properties\, with application to g
 eophysics and planetary sceince\; Newtonian gravitational theory\; and Di
 latometry studies of rocks. She is best known for inferring macroscopic p
 roperties of solids from microscopy measurements of spectra. She publishe
 s in the areas of astronomy\, geoscience\, material science\, medicine\, 
 physics and planetary science. She has served as the editor for American 
 Mineralogist and as a councillor for the Mineralogical Society of America
 . 
X-ALT-DESC;FMTTYPE=text/html:&lt;html&gt;&lt;head&gt;&lt;title&gt;&lt;/title&gt;&lt;/head&gt;&lt;body&gt;&lt;p&gt;Ne
 ar-surface motions of Earth's plate are made possible by the cold\, britt
 le lithosphere being underlain by a weak low-velocity zone (LVZ). The the
 rmal states of both layers result from the leakage of Earth's internal ra
 diogenic heat to space. But to move the plates laterally requires lateral
  forces. We propose that force imbalances arising in the unique 3-body-Ea
 rth-Moon-Sun system are the main cause of complexity in these large-scale
 \, cooperative tectonic motions. Comparing rocky planets shows that the p
 resence and longevity of volcanism and tectonism depend on the particular
  combination of moon size\, moon orbital orientation\, proximity to the S
 un\, and rates of body spin and cooling. Earth is the only rocky planet w
 ith all the factors needed for plate tectonics. She will explain that bec
 ause the lunar orbit is becoming more elliptical\, rather than growing\, 
 plate tectonics is ancient.&lt;/p&gt;\n&lt;p&gt;Dr. Anne M. Hofmeister&amp;nbsp\;obtained
  her BS with highest honors in Physics and Literature - Harvey Mudd Colle
 ge\, MS in Physics - University of Illinois\, PhD in Geology - Caltech. S
 he has experience with spectroscipic measurements of minerals\, was a pos
 tdoctoral associate and fellow at the Geophysical Laboratory performing h
 igh-pressure measurements under the supervision of Ho-Kwang Mao. She was 
 an assistant professor and associate professor at U.C. Davis\, including 
 a David and Lucille Packard Fellowship. She also completed a brief sabbat
 ical as a Humbolt Fellow at the Max Planck Institute in Mainz\, Germany\,
  where she studied with Reinhard Boehler.&lt;/p&gt;\n&lt;p&gt;Currently\, she conduct
 s research in several areas at the Earth and Planetary Science Department
  at Washington University in St. Louis. Her research includes: Optical an
 d infrared spectroscopy with collaborative application to astronomy to be
 tter understand the mechanism of heat transfer\; Measurement and modellin
 g of heat transport and thermodynamic properties\, with application to ge
 ophysics and planetary sceince\; Newtonian gravitational theory\; and Dil
 atometry studies of rocks. She is best known for inferring macroscopic pr
 operties of solids from microscopy measurements of spectra. She publishes
  in the areas of astronomy\, geoscience\, material science\, medicine\, p
 hysics and planetary science. She has served as the editor for American M
 ineralogist and as a councillor for the Mineralogical Society of America.
 &amp;nbsp\;&lt;/p&gt;&lt;/body&gt;&lt;/html&gt;
DTSTART;TZID=America/Chicago:20240412T143000
DTEND;TZID=America/Chicago:20240412T153000
SEQUENCE:0
URL:http://www.geosciences.missouristate.edu
CATEGORIES:Public,Alumni,Current Students,Faculty,Future Students
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