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                  <text>(BKM) Belknap Mountains Ring Complex -- White Mountains, New Hampshire</text>
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                <text>BKM-10</text>
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                <text>Granite</text>
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                <text>Glendale, New Hampshire</text>
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                <text>1980</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/df566258e339655610e57ce52cf18970.pdf"&gt;BKM Rock Suite&lt;/a&gt;</text>
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                <text>fine grained</text>
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            <name>Accrual Method</name>
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                <text>Purchased from Western Minerals, Inc.</text>
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                  <text>(BKM) Belknap Mountains Ring Complex -- White Mountains, New Hampshire</text>
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                <text>BKM-12</text>
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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Granite</text>
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                <text>Gilford, New Hampshire</text>
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            <name>Accrual Periodicity</name>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/df566258e339655610e57ce52cf18970.pdf"&gt;BKM Rock Suite&lt;/a&gt;</text>
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                <text>Purchased from Western Minerals, Inc.</text>
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                  <text>(WMB) White Mountains Batholith -- New Hampshire</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>WMB-5</text>
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            <description>A name given to the resource</description>
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                <text>Granite</text>
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                <text>Hwy. 302 (west side); 1/2 mile N. of Notchland, NH and 1 mile S. of Mt. Nancy rest stop.&#13;
Central Crawford Notch quadrangle map, NH</text>
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                <text>Western Minerals, Inc.</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/53c413d54ead7c05b0db1bd214fc9f41.pdf"&gt;WMB Rock Suite&lt;/a&gt;</text>
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          <element elementId="117">
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                <text>Purchased from Western Minerals, Inc.</text>
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            <name>Alternative Title</name>
            <description>An alternative name for the resource. The distinction between titles and alternative titles is application-specific.</description>
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              <elementText elementTextId="36711">
                <text>Mt. Osceola granite</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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                <text>The granites at this locality are intruded by aplite dikes (WMB-6)</text>
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            <name>Temporal Coverage</name>
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              <elementText elementTextId="36713">
                <text>Early - Middle Jurassic</text>
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              <name>Title</name>
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                  <text>(WMB) White Mountains Batholith -- New Hampshire</text>
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          <name>Unit</name>
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              <text>Littleton Formation</text>
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            <name>Identifier</name>
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                <text>WMB-7</text>
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            <name>Title</name>
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                <text>Granite</text>
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                <text>Hwy. 302 (east side of rd), Crawford Notch, NH;  20-30 ft. from contact with the Littleton formation.; ~1.2 miles S. of Crawford house.&#13;
N. central Crawford Notch quadrangle map, NH</text>
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                <text>Western Minerals, Inc.</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/53c413d54ead7c05b0db1bd214fc9f41.pdf"&gt;WMB Rock Suite&lt;/a&gt;</text>
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            <name>Accrual Method</name>
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                <text>Purchased from Western Minerals, Inc.</text>
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            <description>An alternative name for the resource. The distinction between titles and alternative titles is application-specific.</description>
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                <text>Conway granite</text>
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            <description>An account of the resource</description>
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              <elementText elementTextId="36709">
                <text>fine-coarse grained pink granite</text>
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                  <text>(WMB) White Mountains Batholith -- New Hampshire</text>
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          <name>Number of Thin Sections</name>
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                <text>WMB-12</text>
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                <text>Granite</text>
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                <text>Sample from S. flank of Redstone Ledge at Redstone quarry, Bartlett, NH&#13;
S. Central region of North Conway quadrangle map, NH </text>
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            <name>Contributor</name>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/53c413d54ead7c05b0db1bd214fc9f41.pdf"&gt;WMB Rock Suite&lt;/a&gt;</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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                <text>Massive red granite.  Grain size ranges from coarse to fine.</text>
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          <element elementId="117">
            <name>Accrual Method</name>
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                <text>Purchased from Western Minerals, Inc.</text>
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            <name>Alternative Title</name>
            <description>An alternative name for the resource. The distinction between titles and alternative titles is application-specific.</description>
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                <text>Conway granite</text>
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                  <text>(WMB) White Mountains Batholith -- New Hampshire</text>
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      <description>A physical material with a mineral composition.</description>
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          <name>Number of Thin Sections</name>
          <description>Number of thin sections associated with this sample</description>
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            <description>An unambiguous reference to the resource within a given context</description>
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                <text>WMB-13</text>
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            <description>A name given to the resource</description>
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                <text>Granite</text>
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            <description>Spatial characteristics of the resource.</description>
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                <text>Sample collected from a quarry just W. of Redstone quarry; Bartlett, NH</text>
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            <name>Contributor</name>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/53c413d54ead7c05b0db1bd214fc9f41.pdf"&gt;WMB Rock Suite&lt;/a&gt;</text>
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            <description>An account of the resource</description>
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                  <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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                  <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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                  <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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                  <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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                <text>Graniteville Granite</text>
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                <text>medium grained, medium gray w/ pinkish tint</text>
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