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Thin Section&#13;
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/1"&gt;General Rocks Suite&lt;/a&gt;</text>
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                <text>Portland Point Quarry, near Ithica N.Y.</text>
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                <text>Dark colored phaneritic peridotite containes micas, garnets, olivine pyroxene and plagioclase all visible from hand sample. Sample is speckled with light colored material and larger crystals of pyroxcene, olivine and michas visible in hand sample, elongate light colored crystals, mostly small in size (&lt;1mm) but infrequently larger (0.5mm-1cm), darker well formed crystals of olivine. rock unevenly weathers to a light grey to light reddish brown&#13;
&#13;
Thin Section&#13;
Rounded crystals of olivine pyroxcene and numerous small opaques </text>
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                <text>RBH</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/1"&gt;General Rocks Suite&lt;/a&gt;</text>
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            <name>Identifier</name>
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            <description>Spatial characteristics of the resource.</description>
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                <text>Near Lexington, KE</text>
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            <element elementId="50">
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                  <text>(HA) Volcanic Phenomena Suite -- The Hawaiian Islands of Hawaii and Oahu</text>
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              <name>Description</name>
              <description>An account of the resource</description>
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                  <text>These 31 samples comprise a collection of volcanic rocks associated with the hot-spot volcanism of the Hawaiian Islands. Samples were collected from various locations across the islands of Hawaii and Oahu. The collection contains samples of primarily tholeiitic &amp; alkalic basalts, pumice, scoria, oceanite, and hawaiite. </text>
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            </element>
            <element elementId="37">
              <name>Contributor</name>
              <description>An entity responsible for making contributions to the resource</description>
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                <elementText elementTextId="17794">
                  <text>Western Minerals, Inc.</text>
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                  <text>1969</text>
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                  <text>HA-1 - HA-31</text>
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              <description>Spatial characteristics of the resource.</description>
              <elementTextContainer>
                <elementText elementTextId="17821">
                  <text>Samples were collected from various locations on the islands of Hawaii and Oahu. </text>
                </elementText>
              </elementTextContainer>
            </element>
            <element elementId="116">
              <name>Temporal Coverage</name>
              <description>Temporal characteristics of the resource.</description>
              <elementTextContainer>
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                  <text>Samples formed from Holocene eruptions of the past 300 years. Dated samples formed between 1750 and 1960. </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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                  <text>Purchased from Western Minerals, Inc. </text>
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            </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="17997">
                  <text>&lt;p&gt;&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Macdonald, G.A., 1949, Petrography of the Island of Hawaii, U.S.G.S. Prof. Paper 214 D&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article is a part of the general investigation of the island of Hawaii by the United States Geologic Survey. The paper describes the dominant volcanoes of the island of Hawaii (from which most of the suite's samples were collected) and describes the petrographic phenomena observed and geochemical analyses of volcanic rocks.Â &lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;strong&gt;Additional Resources:&lt;/strong&gt;&lt;br /&gt;Ho, R.A., Garcia, M.O., 1988, Origin of differentiated lavas at Kilauea Volcano, Hawaii; implications from the 1955 eruption: Bulletin of Volcanology, v. 50, p. 35-46.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article describes a study of lava flows from the 1955 eruption of the Kilauea Volcano on the island of Hawaii to evaluate models of crystal fractionation or magma mixing as the processes forming differentiated magmas. Through geochemical analyses, the study concluded that crystal fractionation resulted in the observed differentiation of lavas.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;br /&gt;Hofman, A.W., Farnetani, C.G., 2013, Two Views of Hawaiian Plume Structure: Geochemistry, Geophysics, Geosystems, v.14, p. 5308-5322, doi:10.1002/2013GC004942&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article presents two opposing views of the source of magmas for the Hawaiian volcanoes. Both views favor a deep mantle source, but try to explain differences in isotopic compositions.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;br /&gt;Macdonald, G.A., 1968, Composition and origin of Hawaiian LavasÂ &lt;em&gt;in&lt;/em&gt; GSA Memoirs 1968, p. 477-522&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article provides geochemical analysis of major elements as well as determinations of minor elements of volcanic rocks from the island of Hawaii. The article describes the three major rock types - tholeitic, alkalic, and nephelinic - and concludes these rock suites are chemically intergradational and are likely derived from crystal differentiation of a single parent magma.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;br /&gt;Moore, J.G., Clague, D.A., 1992, Volcano growth and evolution of the Island of Hawaii: Geologic Society of America Bulletin, v. 104, p. 1471-1484&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article proposes a chronologic evolution of the island of Hawaii, from where many of the suite's samples were collected.&lt;/li&gt;
&lt;/ul&gt;</text>
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            <description>A name given to the resource</description>
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            <description>An account of the resource</description>
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                <text>Hand Sample: Natural surface of sample is dark in color with smooth texture. Cut face reveals blocks of peridotite and dunite held together with a thin layer of lava cement. Sample has high specific gravity. </text>
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                <text>Thin Section: Large euhedral to subhedral olivine grains compose the majority of the sample, with thin bands of glass material between them. </text>
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                <text>Hualalai - 9 miles north of Hohokahau - Island of Hawaii &#13;
Sample collected just north of Relay Tower and approx. one mile southeast of the highway. </text>
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            <name>Temporal Coverage</name>
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              <elementText elementTextId="16477">
                <text>1801</text>
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                <text>Sample collected in January, 1969.</text>
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                  <text>Northern Apennines, Liguria Region, Italy&lt;br /&gt;Samples 1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, and 15 are taken from the region around Bargone, Italy&lt;br /&gt;Samples 14, 16, 17, 18, 19, 20, and 21 are taken from the region around Sassello, Italy&lt;br /&gt;Sample 22 is taken from outside Genoa, Italy</text>
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                  <text>&lt;a href="http://geosciencecollections.milne-library.org/" target="_blank"&gt;The Geneseo Geoscience Collection&lt;/a&gt;</text>
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                  <text>Purchased by Western Minerals, Inc.</text>
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;/strong&gt;&lt;span class="cit-auth cit-auth-type-author"&gt;Lagabrielle, Y.,&lt;/span&gt;&lt;span class="cit-sep cit-sep-two-item-separator"&gt;Â and Cannat, M., 1990, &lt;/span&gt;&lt;span class="cit-title"&gt;Alpine Jurassic ophiolites resemble the modern central Atlantic basement: Geology, v. 18, p. 319-322&lt;br /&gt;&lt;/span&gt;Link:Â &lt;a href="http://geology.geoscienceworld.org/content/18/4/319.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This fairly short article gives some insight into the development of the North Apennine Ophiolites with a fairly recent view on the matter.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;&lt;br /&gt;Additional Resources&lt;/strong&gt;&lt;strong&gt;:&lt;/strong&gt;&lt;br /&gt;Garuti, G., and Zaccarini, F., 2005, Minerals of Au, Ag and U in Volcanic-Rock-Associated Massive Sulfide Deposits of the Northern Apennine Ophiolite, Italy: The Canadian Mineralogist, v. 43, p. 935-950&lt;br /&gt;DOI: &lt;a href="http://dx.doi.org/10.2113/gscanmin.43.3.935" target="_blank"&gt;10.2113/gscanmin.43.3.935&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the elemental composition of the North Apennine Ophiolite sequence and uses that to determine previous geologic events.&lt;/li&gt;
&lt;/ul&gt;
Garuti, G., Zaccarini, F., Scacchetti, M., and Bartoli, O., 2011, The Pb-rich sulfide veins in the Boccassuolo ophiolite: Implications for the geochemical evolution of the hydrothermal activity across the ocean-continent transition in the Ligurian Tethys (Northern-Apennine, Italy): Lithos, v. 124, p. 243-254&lt;br /&gt;DOI:Â &lt;a title="10.1016/j.lithos.2010.11.006" href="http://dx.doi.org/10.1016/j.lithos.2010.11.006" target="_blank"&gt;10.1016/j.lithos.2010.11.006&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the chemical composition of the ophiolite sequence under a different name and ties it into the formation history.&lt;/li&gt;
&lt;/ul&gt;
Garzanti, E., Canclini, S., Foggia, F.M., and Petrella, N., 2002, Unraveling Magmatic and Orogenic Provenance in Modern Sand: The Back-Arc Side of the Apennine Thrust Belt, Italy: Journal of Sedimentary Research, v. 72, p. 2-17&lt;br /&gt;DOI:Â &lt;a title="10.1306/051801720002" href="http://dx.doi.org/10.1306/051801720002" target="_blank"&gt;&lt;span&gt;10.1306/051801720002&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into great detail on the provenance characteristics for a number of sands. including sands originating from the North Apennine Ophiolite sequence.&lt;/li&gt;
&lt;/ul&gt;
Cibin, U., Spadafora, E., Zuffa, G.G., and Castellarin, A., 2001, Continental collision history from arenites of episutural basins in the Northern Apennines, Italy: Geological Society of America Bulletin, v. 113, p. 4-19&lt;br /&gt;Link: &lt;a title="GeoScienceWorld" href="http://bulletin.geoscienceworld.org/content/113/1/4.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into detail about the deformations experienced by the North Apennine Ophiolites after the Eocene.&lt;/li&gt;
&lt;/ul&gt;</text>
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                <text>Quartz-Diorite</text>
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