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&#13;
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                  <text>&lt;strong&gt;Start Here:&lt;/strong&gt; &lt;br /&gt;Vollmer, F. W., and Walker, J., 2009, The classic Barrovian metamorphic sequence of Dutchess County and its structural and stratigraphic context in the Taconic Orogeny. In Guidebookâ€”New York State Geological Association Meeting, v. 81, p. 11-1.Â &lt;br /&gt;&lt;a href="http://www2.newpaltz.edu/~vollmerf/papers/Vollmer_and_Walker_2009_NYSGA.pdf"&gt;http://www2.newpaltz.edu/~vollmerf/papers/Vollmer_and_Walker_2009_NYSGA.pdf&lt;/a&gt;Â (accessed March 15th, 2015)&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;A useful field trip guide across the Barrovian metamorphic sequence of Dutchess county. Good general introduction to the geology of the area.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional Resources:&lt;/strong&gt;&lt;br /&gt;Whitney, D.L., Mechum, T.A., Keuhner, S.M., and Dilek, Y.R., 1996, Progressive metamorphism of pelitic rocks from protolith to granulite facies, Dutchess County, New York, USA: constraints on the timing of fluid infiltration during regional metamorphism, Journal of Metamorphic Geology, v. 14, p. 163-181. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.1046/j.1525-1314.1996.05836.x&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;A fairly general look at the progressive metamorphism in Dutchess County by one of the foremost workers in the area.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Knopf, E.B., 1927, Some recent work in the Taconic area: American Journal of Science, v. 41, p. 42-458. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.2475/ajs.s5-14.84.429&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;One of the first articles to describle the Dutchess County rocks as a "classic" Barrovian sequence.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Ghent, E.D., Stout, M.Z., 1981, Geobarometry and geothermometry of plagioclase-biotite-garnet-muscovite assemblages, Contributions to Mineralogy and Petrology, v. 76, p. 92-97. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.1007/BF00373688&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Work constraining the pressure and temperature paths of metamorphism in the sequence through equilibrium assemblages. This work was found to be in agreement with other equilibrium assemblage PT paths.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Whitney, D.L., Mechum, T.A., Dilek, Y.R., and Keuhner, S.M., 1996, Modification of garnet during regional metamorphism in garnet through sillimanite-zone rocks, Dutchess County, New York, American Mineralogist, v. 81, p. 696-705. &lt;a href="http://www.minsocam.org/MSA/AmMin/TOC/Articles_Free/1996/Whitney_p696-705_96.pdf"&gt; http://www.minsocam.org/MSA/AmMin/TOC/Articles_Free/1996/Whitney_p696-705_96.pdf&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Work by Whitney on changes in PTX conditions leading to modification of garnet in the metamorphic sequence. Garnet is widely distributed through the sequence, which makes it a useful marker for tracking these changes.&lt;/li&gt;
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          <name>Dublin Core</name>
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              <name>Title</name>
              <description>A name given to the resource</description>
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                  <text>(SFM) Igneous Suite -- St. Francois Mountains, Southeastern Missouri</text>
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              <name>Description</name>
              <description>An account of the resource</description>
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                <elementText elementTextId="17790">
                  <text>This collection is composed of igneous volcanic and intrusive rocks from the St. Francois Mountains of Missouri. The variation within the collection can be used to explain the geologic history of the area. The St. Francois Mountains batholith was formed by granitic intrusions into Precambrian rhyolites, tuffs, and breccias. Then basalt, diabase, and porphyritic intrusions cut the granitoids.</text>
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            <element elementId="37">
              <name>Contributor</name>
              <description>An entity responsible for making contributions to the resource</description>
              <elementTextContainer>
                <elementText elementTextId="17791">
                  <text>Western Minerals, Inc.</text>
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            <element elementId="109">
              <name>References</name>
              <description>A related resource that is referenced, cited, or otherwise pointed to by the described resource.</description>
              <elementTextContainer>
                <elementText elementTextId="17991">
                  <text>Start here:Â &lt;br /&gt;&lt;br /&gt;Bickford, M.E. and Mose, D.G., 1974, Geochronology of Precambrian rocks, St. Francois Mountains, South eastern Missouri: GSA Special Papers 1975, v. 165, p. 1-48 doi: &lt;a href="http://dx.doi.org/10.1130/SPE165-p1" target="_blank"&gt;http://dx.doi.org/10.1130/SPE165-p1&lt;br /&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Early study of the geochronology of the Precambrian rocks within the St. Francois mountains. Provides further insight upon the sequence discussed in the dscription.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Meert, J.G. and Stuckey, W., 2002, Revisiting the paleomagnetism of the 1.476 Ga St. Francois Mountains igneous province, Missouri: Tectonics v. 21, Issue 2, p. 1-19 doi: &lt;a href="http://dx.doi.org/10.1029/2000TC001265%20" target="_blank"&gt;http://dx.doi.org/10.1029/2000TC001265 &lt;br /&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Information acquired from paleomagnestism studies of the St. Francois igneous provence has proven fruitful for determining an acient paleomagnetic pole for Laurentia.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Menuge, J.F, Brewer, T.S., and Seeger, C.M., 2002, Petrogenesis of metaluminous A-type rhyolites from the St. Francois Mountains, Missouri and the Mesoproterozoic evolution of the southern Laurentian Margin: Precambrian Research, volume 113, issues 3-4, p. 269-291 doi: &lt;a href="http//dx.doi.org/10.1016/S0301-9268(01)00211-X%20" target="_blank"&gt;http//dx.doi.org/10.1016/S0301-9268(01)00211-X &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Trace elemental analysis of Precambrian rocks from the SFM provide insight into the condition of crystallization and the elemental constituents which played a role into the interesting history of this rhyolitic provence.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Rohs, R. C, and Van Schmus, W.R., 2006, Isotopic connection between basement rocks exposed in the St. Francois Mountains and the arbucks Mountains southern mid-continent, North America: International Journal of Earth Sciences, volume 96, Issue 4, p. 599-611 &lt;br /&gt;doi: &lt;a href="http://dx.doi.org/10.1007/s00531-006-0123-5" target="_blank"&gt;http://dx.doi.org/10.1007/s00531-006-0123-5&lt;br /&gt;&lt;/a&gt;
&lt;ul&gt;&lt;li&gt;&lt;span style="color:#000000;"&gt;Radiometric study of the SFM provence and the Arbuckle mountains of southern Oklahoma suggests a common source.Â &lt;/span&gt;&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Wenner, D. and Taylor Jr., H.P., 1976, Oxygen and hydrogen isotope studies of a Precambian granite-rhyolite terrane, ST. Francois Mountains, southeastern Missouri: Geological Society of America bulletin v. 87, no. 11, p.1587-1598 &lt;br /&gt;doi: &lt;a href="http://dx.doi.org/10.1130/0016-7606" target="_blank"&gt;http://dx.doi.org/10.1130/0016-7606&lt;br /&gt;&lt;/a&gt;
&lt;ul&gt;&lt;li&gt;Isotopic analysis of oxygen isotope content within mineral grains within the Precambrian rhyolitic rocks of the SFM yields data that suggests Precambrian oceans were similar to modern day meteoric oceans.&lt;/li&gt;
&lt;/ul&gt;</text>
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              <name>Accrual Method</name>
              <description>The method by which items are added to a collection.</description>
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                <elementText elementTextId="18001">
                  <text>Purchased from Western Minerals Inc. </text>
                </elementText>
              </elementTextContainer>
            </element>
            <element elementId="115">
              <name>Spatial Coverage</name>
              <description>Spatial characteristics of the resource.</description>
              <elementTextContainer>
                <elementText elementTextId="18003">
                  <text>St. Francois Mountains, Ozark region of Southeastern Missouri</text>
                </elementText>
              </elementTextContainer>
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            <element elementId="116">
              <name>Temporal Coverage</name>
              <description>Temporal characteristics of the resource.</description>
              <elementTextContainer>
                <elementText elementTextId="18024">
                  <text>Precambrian (1.476 Ga)</text>
                </elementText>
              </elementTextContainer>
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            <element elementId="40">
              <name>Date</name>
              <description>A point or period of time associated with an event in the lifecycle of the resource</description>
              <elementTextContainer>
                <elementText elementTextId="18159">
                  <text>January 20, 1969</text>
                </elementText>
              </elementTextContainer>
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    <itemType itemTypeId="15">
      <name>Rock</name>
      <description>A physical material with a mineral composition.</description>
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        <element elementId="129">
          <name>Number of Thin Sections</name>
          <description>Number of thin sections associated with this sample</description>
          <elementTextContainer>
            <elementText elementTextId="13805">
              <text>1</text>
            </elementText>
          </elementTextContainer>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Basalt Dike</text>
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            <name>Description</name>
            <description>An account of the resource</description>
            <elementTextContainer>
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                <text>Hand Sample: Aphanitic brown-black basalt with microcrystalline inclusions of quartz and alkali feldspar. Weathers to yellow orange. Part of a dike cross cutting granite at the Cornwall Quarry.</text>
              </elementText>
              <elementText elementTextId="13800">
                <text>Thin Section, XPL: 15% medium-grained plagioclase crystals in 75% matrix of very-fine-grained opaques, plagioclase, and biotite. Very fine veins of a darker material run through the sample.</text>
              </elementText>
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            <name>Date</name>
            <description>A point or period of time associated with an event in the lifecycle of the resource</description>
            <elementTextContainer>
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                <text>1/20/1969</text>
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            <name>Is Part Of</name>
            <description>A related resource in which the described resource is physically or logically included.</description>
            <elementTextContainer>
              <elementText elementTextId="13802">
                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/15"&gt; St. Francois Mountains Suite &lt;/a&gt;</text>
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            <name>Identifier</name>
            <description>An unambiguous reference to the resource within a given context</description>
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                <text>SFM-10</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="115">
            <name>Spatial Coverage</name>
            <description>Spatial characteristics of the resource.</description>
            <elementTextContainer>
              <elementText elementTextId="13804">
                <text>St. Francois Mtns. Batholith, Missouri Cornwell Quarry</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="37">
            <name>Contributor</name>
            <description>An entity responsible for making contributions to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="18188">
                <text>Western Minerals, Inc</text>
              </elementText>
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          <element elementId="117">
            <name>Accrual Method</name>
            <description>The method by which items are added to a collection.</description>
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              <elementText elementTextId="18189">
                <text>Purchased from Western Minerals Inc.</text>
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