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                    <text>DUCO-12 hand sample of muscovite schist</text>
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                  <text>(DUCO) Barrovian Metamorphic Sequence -- Dutchess County, New York</text>
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                  <text>A classic example of Barrovian-type metamorphism in Dutchess County, NY associated with the Taconic orogeny. A Barrovian metamorphic sequence displays gradual pressure and temperature increase along the metamorphic gradient, and occurs during regional metamorphism. These zones of pressure and temperature increase are recognizable by the characteristic minerals that accompany them. Dutchess County, NY contains an unusually complete sequence.&#13;
&#13;
This collection contains metamorphic rocks from chlorite grade to sillimanite grade in a tight spatial window which records the regional metamorphic gradient increasing  from WNW to ESE. This collection also contains some rocks that mirror the protoliths of the schists and quartzites of the sequence (shales and graywacke). </text>
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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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                <text>Muscovite schist</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/18"&gt;Barrovian Metamorphic Sequence--Dutchess County, New York&lt;/a&gt;</text>
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                <text>Extremely coarse-grained muscovite schist. Large garnets visible in hand sample. Sillimanite is not recognizable in hand sample, however.&#13;
&#13;
The thin section shows muscovite (with minor sillimanite) in a large band, biotite, staurolite, and quartz.&#13;
&#13;
This rock is from the sillimanite zone of the Barrovian metamorphic sequence (highest metamorphism). </text>
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                <text>Purchased from Western Minerals Inc.</text>
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                  <text>A classic example of Barrovian-type metamorphism in Dutchess County, NY associated with the Taconic orogeny. A Barrovian metamorphic sequence displays gradual pressure and temperature increase along the metamorphic gradient, and occurs during regional metamorphism. These zones of pressure and temperature increase are recognizable by the characteristic minerals that accompany them. Dutchess County, NY contains an unusually complete sequence.&#13;
&#13;
This collection contains metamorphic rocks from chlorite grade to sillimanite grade in a tight spatial window which records the regional metamorphic gradient increasing  from WNW to ESE. This collection also contains some rocks that mirror the protoliths of the schists and quartzites of the sequence (shales and graywacke). </text>
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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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              <text>Barrovian Metamorphic Sequence</text>
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                <text>Marble</text>
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                <text>Dutchess Co., NY</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/18"&gt;Barrovian Metamorphic Sequence--Dutchess County, New York&lt;/a&gt;</text>
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            <description>An account of the resource</description>
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                <text>Metamorphised Briarcliff dolostone.&#13;
&#13;
The thin section shows well-twinned dolomite grains with diopside at the bottom.&#13;
&#13;
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                  <text>A classic example of Barrovian-type metamorphism in Dutchess County, NY associated with the Taconic orogeny. A Barrovian metamorphic sequence displays gradual pressure and temperature increase along the metamorphic gradient, and occurs during regional metamorphism. These zones of pressure and temperature increase are recognizable by the characteristic minerals that accompany them. Dutchess County, NY contains an unusually complete sequence.&#13;
&#13;
This collection contains metamorphic rocks from chlorite grade to sillimanite grade in a tight spatial window which records the regional metamorphic gradient increasing  from WNW to ESE. This collection also contains some rocks that mirror the protoliths of the schists and quartzites of the sequence (shales and graywacke). </text>
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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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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/18"&gt;Barrovian Metamorphic Sequence--Dutchess County, New York&lt;/a&gt;</text>
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                <text>Metamorphised Briarcliff dolostone with visible micas. Contains diopside, tremollite, and phlogopite. At the metamorphic grade of the first sillimanite isograd. &#13;
&#13;
Thin section shows irregular dolomite grains in the center, with pleochroic phlogopite at top and tremolite at bottom.</text>
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                  <text>A classic example of Barrovian-type metamorphism in Dutchess County, NY associated with the Taconic orogeny. A Barrovian metamorphic sequence displays gradual pressure and temperature increase along the metamorphic gradient, and occurs during regional metamorphism. These zones of pressure and temperature increase are recognizable by the characteristic minerals that accompany them. Dutchess County, NY contains an unusually complete sequence.&#13;
&#13;
This collection contains metamorphic rocks from chlorite grade to sillimanite grade in a tight spatial window which records the regional metamorphic gradient increasing  from WNW to ESE. This collection also contains some rocks that mirror the protoliths of the schists and quartzites of the sequence (shales and graywacke). </text>
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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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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/18"&gt;Barrovian Metamorphic Sequence--Dutchess County, New York&lt;/a&gt;</text>
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                <text>Metamorphised Balmville limestone with visible phlogopite crystals. Also contains actinolite.&#13;
&#13;
Thin section shows calcite with interspersed pleochroic phlogopite.</text>
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                <name>Title</name>
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                    <text>DUCO-16 hand sample of marble</text>
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                  <text>(DUCO) Barrovian Metamorphic Sequence -- Dutchess County, New York</text>
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              <name>Contributor</name>
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                <elementText elementTextId="17801">
                  <text>Western Minerals, Inc.</text>
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                  <text>Purchased from Western Minerals, Inc.</text>
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              <name>Description</name>
              <description>An account of the resource</description>
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                <elementText elementTextId="17809">
                  <text>A classic example of Barrovian-type metamorphism in Dutchess County, NY associated with the Taconic orogeny. A Barrovian metamorphic sequence displays gradual pressure and temperature increase along the metamorphic gradient, and occurs during regional metamorphism. These zones of pressure and temperature increase are recognizable by the characteristic minerals that accompany them. Dutchess County, NY contains an unusually complete sequence.&#13;
&#13;
This collection contains metamorphic rocks from chlorite grade to sillimanite grade in a tight spatial window which records the regional metamorphic gradient increasing  from WNW to ESE. This collection also contains some rocks that mirror the protoliths of the schists and quartzites of the sequence (shales and graywacke). </text>
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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>
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                <elementText elementTextId="17810">
                  <text>1970</text>
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            <element elementId="115">
              <name>Spatial Coverage</name>
              <description>Spatial characteristics of the resource.</description>
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                <elementText elementTextId="17811">
                  <text>Dutchess County, New York</text>
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            </element>
            <element elementId="116">
              <name>Temporal Coverage</name>
              <description>Temporal characteristics of the resource.</description>
              <elementTextContainer>
                <elementText elementTextId="17812">
                  <text>450-430 Ma</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="17970">
                  <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;
&lt;/ul&gt;</text>
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      <description>A physical material with a mineral composition.</description>
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              <text>Barrovian Metamorphic Sequence</text>
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          <name>Number of Thin Sections</name>
          <description>Number of thin sections associated with this sample</description>
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              <text>1</text>
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            <name>Identifier</name>
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                <text>DUCO-16</text>
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            <name>Title</name>
            <description>A name given to the resource</description>
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              <elementText elementTextId="17961">
                <text>Marble</text>
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          <element elementId="115">
            <name>Spatial Coverage</name>
            <description>Spatial characteristics of the resource.</description>
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              <elementText elementTextId="17962">
                <text>Dutchess Co., NY</text>
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          <element elementId="37">
            <name>Contributor</name>
            <description>An entity responsible for making contributions to the resource</description>
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              <elementText elementTextId="17964">
                <text>Western Minerals</text>
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          <element elementId="104">
            <name>Is Part Of</name>
            <description>A related resource in which the described resource is physically or logically included.</description>
            <elementTextContainer>
              <elementText elementTextId="17965">
                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/18"&gt;Barrovian Metamorphic Sequence--Dutchess County, New York&lt;/a&gt;</text>
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          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="17966">
                <text>Metamorphised Balmville limestone with visible phlogopite crystals. Also contains tremolite visible at the outcrop level. Within nose of anticline of Walloomsac schist.&#13;
&#13;
The PPL thin section shows a large irregular calcite grain with tremolite at the bottom.</text>
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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="17968">
                <text>Purchased from Western Minerals Inc.</text>
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              <element elementId="50">
                <name>Title</name>
                <description>A name given to the resource</description>
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                    <text>Wollastonite-garnet-diopside</text>
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              <description>A name given to the resource</description>
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                  <text>(ADK) Anorthosite-Charnockite and Metamorphic Suite --&#13;
 Adirondack Mountains, New York</text>
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              <name>Description</name>
              <description>An account of the resource</description>
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                <elementText elementTextId="17772">
                  <text>The Adirondack Mountains of northern New York State are underlain by approximately 20,000 square miles of complexly deformed, high grade metamorphic rocks which are believed to represent a southern outlier of the much larger Grenville Province.The Adirondacks can be divided into the "Lowlands" and the "Highlands" . The Lowlands comprise the northwestern quarter of the belt and are characterized by amphibolite facies metamorphism. The Highlands appear to consist entirely of granulite facies rocks.  All rocks in this suite have been collected from the Highlands and predominantly from the southern quarter of the Adirondacks.  &#13;
&#13;
This suite of rocks is designed to be representative of the Highlands in general. Therefore it includes both metasedimentary and metaigneous rocks.  The latter are very common throughout the Adirondacks and contain the often-discussed anorthosite-charnockite suite of rocks. Almost all rocks in the Adirondack Highlands are strongly foliated. This is the result of intense polyphase deformation that has affected this area.&#13;
</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="17773">
                  <text>Western Minerals Inc.</text>
                </elementText>
              </elementTextContainer>
            </element>
            <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="17808">
                  <text>&lt;strong&gt;Start here:Â &lt;br /&gt;&lt;/strong&gt;McLelland, J., and Selleck, B.W.,2011,Â Megacrystic Gore Mountain-type garnets in the Adirondack Highlands; age, origin, and tectonic implications:Geosphere, v.7, no. 5, p.1194-1208, doi:Â &lt;a href="http://dx.doi.org/10.1130/GES00683.1" target="_blank"&gt;10.1130/GES00683.1&lt;/a&gt;.&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article describes the formation of the megacrystic garnet amphibolites in the Gore Mountain section of the Adirondack Mountains. The authors conclude that three main factors influenced the garnet development: collapse of the Ottawan orogeny, intrusion of Lyon Mountain Granite, and fluid-related alteration at high temperature.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;McLelland, J.M., Bickford, M.E., Hill, B.M., Clechenko, C.C., Valley, J.W., and Hamilton, M.A., 2004,Â Direct dating of Adirondack Massif anorthosite by U-Pb SHRIMP analysis of igneous zircon; implications for AMCG complexes:Â Geological Society of America Bulletin, v.116, no. 11-12, p.1299-1317, doi:Â &lt;a href="http://dx.doi.org/10.1130/B25482.1" target="_blank"&gt;10.1130/B25482.1&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article describes techniques used to more accurately date the Adirondack Massif anorthosite.The authors concluded that the massifsÂ &lt;span&gt;constitute a single, composite anorthosite-mangerite-charnockite-granite (AMCG) suite intruded at ca. 1155 Ma. Although the rock suite is considered to be coeval, the authors conclude the rocks are not comagmatic.&lt;/span&gt;&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;McLelland, J., Bickford, M.E., Spear, F., and Storm, L., 2002, Geology and geochronolgy of the eastern Adirondacks inÂ &lt;span&gt;New England Intercollegiate Geological Conference, 94th, New York State Geological Association 74th: guidebook for field trips in New York and Vermont : Lake George, New York&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This field trip guide provides for nine stops in the eastern Adirondacks. It also include some thin sections images and zircon images from sample rocks of the field trip stops.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;McLelland, J., Daly, J.S., and McLelland, J.M., 1996,Â The Grenville orogenic cycle (ca. 1350-1000 Ma); an Adirondack perspective: Tectonophysics, v.265, issue 1-2, p.1-28, doi: &lt;a href="http://dx.doi.org/10.1016/S0040-1951(96)00144-8" target="_blank"&gt;10.1016/S0040-1951(96)00144-8&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article provides a detailed geochronological account of the Grenville orogeny (ca. 1350-1000 Ma) with emphasis on the impact it had on the formation of the Adirondack Mountains.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;McLelland, J., Lewis, A., and Moore, L., 1994,Â Composition and petrogenesis of oxide-, apatite-rich gabbronorites associated with Proterozoic anorthosite massifs: examples from the Adirondack Mountains, New York: Contributions to Mineralogy and Petrology, v.116, p.225-238, doi:Â &lt;a href="http://dx.doi.org/10.1007/BF00310702" target="_blank"&gt;10.1007/BF00310702&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article investigates the occurence of oxide-, apatite-rich gabbronorites with anorthosite massifs of the Adirondacks. The authors describe a multilple-step process of plagioclase crystal fractionation that ultimately leads to high concentrations of P, Fe, and Ti.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;New York State Geological Survey&lt;br /&gt;&lt;a href="http://www.nysm.nysed.gov/nysgs/nygeology/mineralogy/adirondacks/index.html"&gt;http://www.nysm.nysed.gov/nysgs/nygeology/mineralogy/adirondacks/index.html&lt;br /&gt;&lt;/a&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;The NYS Geological Survey is a division of the New York State Museum system. This web page provides some details about the Adirondack Highlands and pictures of various minerals found in this region.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Regan, S.P., Chiarenzelli, J.R., McLelland,Â J.M., and Cousens, B. L., 2011,Â Evidence for an enriched asthenospheric source for coronitic metagabbros in the Adirondack Highlands: Geosphere, v.7, issue 3, p.&lt;span&gt;Â 694-709, doi:Â &lt;a href="http://dx.doi.org/10.1130/GES00629.1" target="_blank"&gt;10.1130/GES00629.1&lt;/a&gt;.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article describes the formation of coronitc metagabbros through tectonic processes involving the asthenosphere. Through geochemical and isotopic analyses, the authors provide a timeline of tectonic and petrologic events that supports an asthenospheric source for coronitic metagabbros.&lt;/li&gt;
&lt;/ul&gt;</text>
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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>
                <elementText elementTextId="17814">
                  <text>1980</text>
                </elementText>
              </elementTextContainer>
            </element>
            <element elementId="116">
              <name>Temporal Coverage</name>
              <description>Temporal characteristics of the resource.</description>
              <elementTextContainer>
                <elementText elementTextId="17815">
                  <text>The Adirondack Mountains were formed approximately 1.1- 1.3 billion years ago during the Grenville Orogeny (Precambrian eon, Proterozic era).</text>
                </elementText>
              </elementTextContainer>
            </element>
            <element elementId="117">
              <name>Accrual Method</name>
              <description>The method by which items are added to a collection.</description>
              <elementTextContainer>
                <elementText elementTextId="17816">
                  <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="17824">
                  <text>This rock suite was collected from the Adirondack Mountains located in the northeastern part of New York State.</text>
                </elementText>
              </elementTextContainer>
            </element>
          </elementContainer>
        </elementSet>
      </elementSetContainer>
    </collection>
    <itemType itemTypeId="15">
      <name>Rock</name>
      <description>A physical material with a mineral composition.</description>
      <elementContainer>
        <element elementId="129">
          <name>Number of Thin Sections</name>
          <description>Number of thin sections associated with this sample</description>
          <elementTextContainer>
            <elementText elementTextId="18300">
              <text>Thin section not  available.</text>
            </elementText>
          </elementTextContainer>
        </element>
      </elementContainer>
    </itemType>
    <elementSetContainer>
      <elementSet elementSetId="1">
        <name>Dublin Core</name>
        <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
        <elementContainer>
          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="18066">
                <text>Wollastonite-garnet-diopside</text>
              </elementText>
            </elementTextContainer>
          </element>
          <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="18067">
                <text>1980</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="37">
            <name>Contributor</name>
            <description>An entity responsible for making contributions to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="18068">
                <text>Western Minerals Inc.</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="43">
            <name>Identifier</name>
            <description>An unambiguous reference to the resource within a given context</description>
            <elementTextContainer>
              <elementText elementTextId="18069">
                <text>AD-24</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="115">
            <name>Spatial Coverage</name>
            <description>Spatial characteristics of the resource.</description>
            <elementTextContainer>
              <elementText elementTextId="18070">
                <text>Adirondack Highlands-this specimen was obtained from the NYCO MIne in Willsboro, NY.</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="18071">
                <text>This unique rock contains white crystalline wollastonite, brown grains of andradite garnet, and green diopside. Specimens courtesy of R.R. Bauer, plant manager of NYCO MInes (1980). McLelland reports some grossularite in addition to andradite.&#13;
&#13;
The following information is from the original OCR document: This interesting rock is discussed by Buddington, 1939, p. 41-43. See also Buddington and Whitcomb, 1941, Geology of the Willsboro Quandrant, New York State Museum Bulletin 325 and Buddington, 1950, "Composition and Genesis of Pyroxene and Garnet Related to the Adirondack Anorthosite and Anorthosite-Marble Contacts," American Mineralogist, v.35, p.659-670.</text>
              </elementText>
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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="18072">
                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/7"&gt;Anorthosite-Charnockite and Metamorphic Suite-Adirondack Mountains, New York&lt;/a&gt;</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="116">
            <name>Temporal Coverage</name>
            <description>Temporal characteristics of the resource.</description>
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                <text>Purchased from Western Minerals Inc.</text>
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                  <text>(DUCO) Barrovian Metamorphic Sequence -- Dutchess County, New York</text>
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                  <text>A classic example of Barrovian-type metamorphism in Dutchess County, NY associated with the Taconic orogeny. A Barrovian metamorphic sequence displays gradual pressure and temperature increase along the metamorphic gradient, and occurs during regional metamorphism. These zones of pressure and temperature increase are recognizable by the characteristic minerals that accompany them. Dutchess County, NY contains an unusually complete sequence.&#13;
&#13;
This collection contains metamorphic rocks from chlorite grade to sillimanite grade in a tight spatial window which records the regional metamorphic gradient increasing  from WNW to ESE. This collection also contains some rocks that mirror the protoliths of the schists and quartzites of the sequence (shales and graywacke). </text>
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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;
&lt;/ul&gt;</text>
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                <text>Barrovian Metamorphic Sequence--Dutchess County, NY Western Minerals Supplementary Information</text>
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                <text>&lt;em&gt;Clinoa&lt;/em&gt; (boring sponge)</text>
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            <description>The topic of the resource</description>
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                <text>possibly Clinoa celata</text>
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                <text>Modern Sponge (sponge)</text>
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Phylum: Porifera &lt;br /&gt;
Class: Demospongea &lt;br /&gt;
Order: &lt;br /&gt;
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          <name>Unit</name>
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            <name>Title</name>
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              <elementText elementTextId="18793">
                <text>&lt;em&gt;Actinostroma expansum&lt;/em&gt; (sponge)</text>
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                <text>Kingdom: Animalia&lt;br /&gt; Phylum: Porifera &lt;br /&gt; Class: Stromatoporoidea &lt;br /&gt; Order: Actinostromatida &lt;br /&gt; Family: Actinostromatidae &lt;br /&gt; Genus: &lt;em&gt;Actinostroma&lt;/em&gt; &lt;br /&gt; Species: &lt;em&gt;expansum&lt;/em&gt; &lt;br /&gt;&lt;br /&gt;</text>
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              <elementText elementTextId="18797">
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                <text>Kingdom: Animalia&lt;br /&gt; 
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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              <elementText elementTextId="18816">
                <text>&lt;em&gt;Stylaster sp.&lt;/em&gt; (hydroid)</text>
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          <element elementId="43">
            <name>Identifier</name>
            <description>An unambiguous reference to the resource within a given context</description>
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                <text>DC7-3S-1</text>
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          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
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              <elementText elementTextId="18818">
                <text>Kingdom: Animalia&lt;br /&gt; Phylum: Cnidaria &lt;br /&gt; Class: Hydrozoa &lt;br /&gt; Order: Stylasterina &lt;br /&gt; Family: Stylasteridae &lt;br /&gt; Genus: &lt;em&gt;Stylaster&lt;/em&gt; &lt;br /&gt; Species: &lt;em&gt;sp.&lt;/em&gt; &lt;br /&gt;&lt;br /&gt;</text>
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          <element elementId="48">
            <name>Source</name>
            <description>A related resource from which the described resource is derived</description>
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                <text>2nd floor hallway, display case 7</text>
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          <element elementId="116">
            <name>Temporal Coverage</name>
            <description>Temporal characteristics of the resource.</description>
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              <elementText elementTextId="18820">
                <text>Recent</text>
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          <element elementId="115">
            <name>Spatial Coverage</name>
            <description>Spatial characteristics of the resource.</description>
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              <elementText elementTextId="18821">
                <text>Samoa</text>
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          <element elementId="49">
            <name>Subject</name>
            <description>The topic of the resource</description>
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              <elementText elementTextId="18822">
                <text>possibly "Stylaster spatula"</text>
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          </element>
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            <element elementId="50">
              <name>Title</name>
              <description>A name given to the resource</description>
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                <elementText elementTextId="18630">
                  <text>2nd Floor ISC Fossil Display Cases</text>
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    <itemType itemTypeId="17">
      <name>Fossil</name>
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        <element elementId="131">
          <name>Number of Items</name>
          <description/>
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            <elementText elementTextId="18829">
              <text>2</text>
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        </element>
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      <elementSet elementSetId="1">
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        <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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              <elementText elementTextId="18824">
                <text>Modern encrusting hydrozoa</text>
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          <element elementId="43">
            <name>Identifier</name>
            <description>An unambiguous reference to the resource within a given context</description>
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              <elementText elementTextId="18825">
                <text>DC7-3S-2</text>
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          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
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              <elementText elementTextId="18826">
                <text>Kingdom: Animalia&lt;br /&gt; 
Phylum: Cnidaria &lt;br /&gt;
Class: Hydrozoa &lt;br /&gt;
Order: Hydroida &lt;br /&gt;
Family:  &lt;br /&gt;
Genus:  &lt;br /&gt; 
Species: &lt;br /&gt;&lt;br /&gt;</text>
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          </element>
          <element elementId="48">
            <name>Source</name>
            <description>A related resource from which the described resource is derived</description>
            <elementTextContainer>
              <elementText elementTextId="18827">
                <text>2nd floor hallway, display case 7</text>
              </elementText>
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          </element>
          <element elementId="116">
            <name>Temporal Coverage</name>
            <description>Temporal characteristics of the resource.</description>
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              <elementText elementTextId="18828">
                <text>Recent</text>
              </elementText>
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          </element>
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  <item itemId="745" public="1" featured="0">
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        <elementSet elementSetId="1">
          <name>Dublin Core</name>
          <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
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            <element elementId="50">
              <name>Title</name>
              <description>A name given to the resource</description>
              <elementTextContainer>
                <elementText elementTextId="18630">
                  <text>2nd Floor ISC Fossil Display Cases</text>
                </elementText>
              </elementTextContainer>
            </element>
          </elementContainer>
        </elementSet>
      </elementSetContainer>
    </collection>
    <itemType itemTypeId="17">
      <name>Fossil</name>
      <description/>
      <elementContainer>
        <element elementId="131">
          <name>Number of Items</name>
          <description/>
          <elementTextContainer>
            <elementText elementTextId="18835">
              <text>1</text>
            </elementText>
          </elementTextContainer>
        </element>
      </elementContainer>
    </itemType>
    <elementSetContainer>
      <elementSet elementSetId="1">
        <name>Dublin Core</name>
        <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="18830">
                <text>&lt;em&gt;Millepora&lt;/em&gt; (fire coral)</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="43">
            <name>Identifier</name>
            <description>An unambiguous reference to the resource within a given context</description>
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              <elementText elementTextId="18831">
                <text>DC7-3S-3</text>
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          </element>
          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
            <elementTextContainer>
              <elementText elementTextId="18832">
                <text>Kingdom: Animalia &lt;br /&gt; 
Phylum: Cnidaria &lt;br /&gt;
Class: Hydrozoa  &lt;br /&gt;
Order: Anthomedusae &lt;br /&gt;
Suborder: Capitata &lt;br /&gt;
Family: Milleporidae &lt;br /&gt;
Genus: &lt;em&gt;Millepora&lt;/em&gt; &lt;br /&gt; 
Species:  &lt;br /&gt;&lt;br /&gt;</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="48">
            <name>Source</name>
            <description>A related resource from which the described resource is derived</description>
            <elementTextContainer>
              <elementText elementTextId="18833">
                <text>2nd floor hallway, display case 7</text>
              </elementText>
            </elementTextContainer>
          </element>
          <element elementId="116">
            <name>Temporal Coverage</name>
            <description>Temporal characteristics of the resource.</description>
            <elementTextContainer>
              <elementText elementTextId="18834">
                <text>Recent</text>
              </elementText>
            </elementTextContainer>
          </element>
        </elementContainer>
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    </elementSetContainer>
  </item>
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