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                  <text>(GC) Grand Canyon Stratigraphic Suite -- Grand Canyon, Arizona</text>
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                  <text>This collection contains 21 samples. They are a representation of samples of lithology from the early precambrian to the late permian. The stratigraphic sequence contains a variety of rocks including, but not limited to schist, limestone, and sandstone. These specimens are representative of the geologic section in the Grand Canyon, but no specimens were collected within the boundaries of the National Park. </text>
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                  <text>Western Minerals Inc.</text>
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                  <text>&lt;strong&gt;Start Here&lt;/strong&gt;:&lt;br /&gt;Blakey, R.C., and Middleton, L.T., 2012, Geologic history and paleogeography of paleozoic and early mesozoic sedimentary rocks, eastern Grand Canyon, Arizona: Geologic Society of America Bulletin, v. 489, pp. 81-92, doi: &lt;a href="%20http%3A//dx.doi.org/10.1130/2012.2489(05)"&gt;10.1130/2012.2489(05)&lt;/a&gt;&lt;br /&gt;&lt;a href="http://dx.doi.org/10.1130/2012.2489(05)%20" target="_blank"&gt;&lt;br /&gt;&lt;/a&gt;
&lt;ul&gt;&lt;li&gt;This reference outlines the stratigraphy found in this suite. It specifically highlights the paleozoic era in which the samples represent.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;&lt;strong&gt;Additional Resources:Â &lt;br /&gt;&lt;/strong&gt;Brown, E.H., Babcock, R.S., Clark, M.D., and Livingston, D.E., 1979,Â Geology of the older Precambrian rocks of the Grand Canyon Part I. Petrology and structure of the Vishnu Complex: Precambrian Research, v. 8, p. 219-241, doi:Â &lt;a href="http://dx.doi.org/10.1016/0301-9268(79)90030-5%20"&gt;10.1016/0301-9268(79)90030-5Â &lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Brown et al. begins this series of 3 articles outlining the geologic timescale and discusses the Vishnu complex and how it fits into the geologic timescale. It provides an explaination for several of the samples in this collection.Â &lt;/li&gt;
&lt;/ul&gt;
Brown, E.H., Babcock, R.S., Clark, M.D., and Livingston, D.E., 1979,Â Geology of the older Precambrian rocks of the Grand Canyon Part II. The Zoroaster Plutonic Complex and related rocks: Precambrian Research, v. 8, p. 243-275, doi&lt;span&gt;&lt;span&gt;:Â &lt;a href="http://dx.doi.org/10.1016/0301-9268(79)90031-7" target="_blank"&gt;10.1016/0301-9268(79)90031-7&lt;/a&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;In the second part of the article, the authors discuss the importance of the pluton and how it affected the formation of the stratigraphic profile of the grand canyon.Â &lt;/li&gt;
&lt;/ul&gt;
Clark, M.D., 1979,Â Geology of the older Precambrian rocks of the Grand Canyon. Part III. Petrology of mafic schists and amphibolites: Precambrian Research, v. 8, p. 277-302, doi&lt;span&gt;&lt;span&gt;:Â &lt;a href="http://dx.doi.org/10.1016/0301-9268(79)90032-9" target="_blank"&gt;10.1016/0301-9268(79)90032-9&lt;/a&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;The final section of this discussion set provides insight into the mafic layers of the stratigraphic column.Â &lt;/li&gt;
&lt;/ul&gt;
Ilg, B.R., Karlstrom, K.E., Hawkins, D.P., and Williams, M.L., 1996,Â Tectonic evolution of Paleoproterozoic rocks in the Grand Canyon: Insights into middle-crustal processes:Â Bulletin of the Geological Society of America, v. 108, p. 1149-1166, doi&lt;span&gt;&lt;span&gt;:Â &lt;a href="http://dx.doi.org/10.1130/0016-7606(1996)108" target="_blank"&gt;10.1130/0016-7606(1996)108&lt;/a&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;This is a general look into the formation of the stratigraphic layers. This article does a good job combining the above articles into one condensed summary.Â &lt;/li&gt;
&lt;/ul&gt;</text>
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                  <text>Peach Springs, Mohave Co., Arizona&#13;
Peach Springs, Coconino Co., Arizona&#13;
Seligman, Ysvupai Co., Arizona &#13;
Williams, Coconino Co., Arizona</text>
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                  <text>Purchased from Western Minerals Inc. </text>
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              <text>Vishnu Schist </text>
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                <text>no date</text>
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                <text>Western Minerals Inc.</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/items/show/1"&gt;Grand Canyon Western Minerals Supplementary Information&lt;/a&gt;</text>
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                <text>GC-1A</text>
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                <text>East wall of Peach Springs Canyon about 14.2 mi. N. of Peach Springs</text>
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                <text>Older Precambrian</text>
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                <text>Purchased from Western Minerals Inc.</text>
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            <name>Description</name>
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                <text>Both cross polarized and plain polarized images were taken at a 400x magnification. </text>
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                <text>Biotite Schist </text>
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                    <text>100x Magnification</text>
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                  <text>(HA) Volcanic Phenomena Suite -- The Hawaiian Islands of Hawaii and Oahu</text>
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              <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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              <name>Contributor</name>
              <description>An entity responsible for making contributions to the resource</description>
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                  <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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              <elementTextContainer>
                <elementText elementTextId="17821">
                  <text>Samples were collected from various locations on the islands of Hawaii and Oahu. </text>
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              <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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                  <text>Purchased from Western Minerals, Inc. </text>
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                <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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                <text>Volcanic Bomb</text>
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                <text>Hand Sample: Imperfect volcanic bomb. Aphanitic with reddish brown color. Observed mudcrack texture of surface likely formed due to weathering. Sample contains abundant vesicles (&lt; 0.05cm in size).</text>
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                <text>Thin Section: Opaque groundmass with numerous vesicles. Phenocrysts of amphiboles are present. </text>
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                <text>Kapoho, Kiluea - Island of Hawaii</text>
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                <text>Volcanic Phenomena Suite - The Hawaiian Islands of Hawaii and Oahu</text>
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                <text>Sample collected January, 1969</text>
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                  <text>(KBR) Karroo Igneous Complex -- Birds River, South Africa</text>
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                  <text>The Birds River Complex is a "Bell-Jar" intrusion first described by du Toit in 1905 and then by Ealey and Robey in 1976. One of the best exposed sections across the margin of the complex is on the farm Denwood, in the southwestern corner of the complex. The samples were  collected from a mafic intrusion near Denwood farm. These samples from the Karroo Complex were collected  from the previously studied section of the complex and neighboring areas.</text>
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                  <text>Dr. Brian Lock,  Rhodes University</text>
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                <elementText elementTextId="17798">
                  <text>Western Minerals, Inc.</text>
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              <description>A related resource that is referenced, cited, or otherwise pointed to by the described resource.</description>
              <elementTextContainer>
                <elementText elementTextId="18613">
                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;/strong&gt;Cox, K.G., 1972, The Karroo Volcanic Cycle: Journal of the Geological Society, v. 128, p. 311-336.&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;Â doi: 10.1144/gsjgs. 128.4.0311.&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;The petrogenesis of the Mesozoic igneous rocks of south-Eastern Africa is related to the tectonic event believed to be the initiation of the break up of Gondwanaland. The cycle began with the rise of potassium-rich picritic magma, the source material for rocks of the northern province, Rhodesia. On top of and peripheral to the main magma body, a zone of sodic magma was generated and formed some of the rocks of the north and most southern rocks.&lt;/li&gt;
&lt;/ul&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;br /&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;White, R.S., 1992, Magmatism During and After Continental Break-Up, Geological Society, London, Special Publications, v. 68, p. 1-16. doi:Â &lt;span&gt;10.1144/GSL.SP.1992.068.01.0.&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;Magmatism that goes along with continental break-up is caused primarily by decompression melting of the underlying mantle as it rises up beneath the rift. The amount of melt produced is determined by the asthenospheric mantle temperature and on the rate of rifting.Â &lt;/li&gt;
&lt;/ul&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span class="cit-sep cit-sep-after-article-pages"&gt;&lt;span&gt;Eales, H.V., and van Robey, J.A., 1976, Differentiation of Tholeiitic Karroo Magma at Birds River, South Africa, Contributions to Mineralogy and Petrology 10. v. 56, p. 101-117. doi:Â &lt;span&gt;10.1007/BF00375423&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;Strongly fractionated residue from the partial crystallization of tholeiitic gabbroic magma was emplaced at depth within sediment of the upper part of the Karroo succession. The residue was most likely tapped from a deeper intrusion during cauldron subsidence, but was engulfed by a later intrusion of olivine gabbro on a large scale.&lt;/li&gt;
&lt;/ul&gt;
Walker, F., and Poldervaart, A., 1949, Karroo Dolerites of the Union of South Africa, Geological Society of America Bulletin, v. 60, p. 591-706. doi: 10.1130/0016-7606(1949)60&lt;span&gt;[591:KDOTUO]2.0.CO;2&lt;/span&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;The Karroo dolerites are the result of the intrusive phase of the early Jurassic basalts that built up the Basutoland lava plateau. Most of the dolerites show little differentiation but olivine rich types and acidic veins have been recorded. The magma had an effect on the sedimentary rocks; many of the rocks described as granophyre were found to be transformed siltstone. The dolerites occur as sills and dikes but "bell-jar inclusions" occur (the Bird's River complex is a bell jar shaped inclusion).Â &lt;/li&gt;
&lt;/ul&gt;
Eales, H.V., and Booth P.W.K., 1974, The Birds River Gabbro Complex, Dordrecht District, Transactions of the Geological Society of South Africa, v. 77, p. 1-15.&lt;br /&gt;&lt;ul&gt;&lt;li&gt;On the gabbros of the Birds River Complex.&lt;/li&gt;
&lt;/ul&gt;</text>
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              <text>Lesotho Formation</text>
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        <element elementId="129">
          <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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                <text>Volcanic Breccia</text>
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                <text>This is a volcanic breccia from the farm Murrelfontein adjacent to the contact with the gabbro unit. It includes partially  melted glass and tridymite, a high temperature polymorph of quartz, and has a brecciated appearance. The breccia has a  allotriomorphic- granular texture and is holocrystalline. Coarse, anhedral, chaotic-looking dark black crystals (3-12mm) are surrounded by slightly lighter colored, smaller anhedral crystals (2 mm -6 mm). There are trace olivine phenocrysts (2 mm).&#13;
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              <elementText elementTextId="13268">
                <text>&lt;a href="http://link.springer.com/article/10.1007/BF00375423"&gt;&lt;span&gt;Differentiation of tholeiitic Karroo magma at Birds River, South Africa&lt;/span&gt;&lt;/a&gt;</text>
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                <text>Western Minerals, Inc.</text>
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              <elementText elementTextId="13271">
                <text>http://www.geosciencecollections.milne-library.org/collections/show/17</text>
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            <name>Identifier</name>
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                <text>KBR-19</text>
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            <name>Spatial Coverage</name>
            <description>Spatial characteristics of the resource.</description>
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              <elementText elementTextId="13273">
                <text>Karoo- Birds River, Eastern Cape, South Africa</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="13274">
                <text>183-179 Ma (Jurassic)</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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                <text>Purchased from Western Minerals, Inc.</text>
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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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                <elementText elementTextId="17793">
                  <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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              <name>Contributor</name>
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                <elementText elementTextId="17794">
                  <text>Western Minerals, Inc.</text>
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              <name>Date</name>
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                  <text>1969</text>
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                  <text>HA-1 - HA-31</text>
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              <name>Spatial Coverage</name>
              <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>
                <elementText elementTextId="17822">
                  <text>Samples formed from Holocene eruptions of the past 300 years. Dated samples formed between 1750 and 1960. </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="17823">
                  <text>Purchased from 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="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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                <text>Volcanic Phenomena Suite - The Hawiian Islands of Hawaii and Oahu, Western Minerals Supplementary Information</text>
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            <description>An account of the resource</description>
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                <text>OCR RPD of supplemental information for the Volcanic Phenomena Suite - The Hawaiian Islands of Hawaii and Oahu</text>
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                <text>January 20, 1969</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/items/browse?search=&amp;amp;advanced%5B0%5D%5Belement_id%5D=&amp;amp;advanced%5B0%5D%5Btype%5D=&amp;amp;advanced%5B0%5D%5Bterms%5D=&amp;amp;range=&amp;amp;public=&amp;amp;featured=&amp;amp;collection=16&amp;amp;type=15&amp;amp;user=&amp;amp;tags=&amp;amp;geolocation-address=&amp;amp;geolocation-latitude=&amp;amp;geolocation-longitude=&amp;amp;geolocation-radius=10&amp;amp;geolocation-radius=10&amp;amp;exhibit=&amp;amp;submit_search=Search+%E2%86%92"&gt;Petrographic and Volcanic Phenomena Suite Rocks&lt;/a&gt;</text>
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                  <text>(BKM) Belknap Mountains Ring Complex -- White Mountains, New Hampshire</text>
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      <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>
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              <text>1</text>
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            <description>A name given to the resource</description>
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                <text>Volcanic rock</text>
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            <name>Spatial Coverage</name>
            <description>Spatial characteristics of the resource.</description>
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              <elementText elementTextId="27722">
                <text>Johnson Mountain, New Hampshire</text>
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            <name>Accrual Periodicity</name>
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                <text>1980</text>
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            <description>The material or physical carrier of the resource.</description>
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