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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>Hand Sample: Porphyritic medium-grained phenocrysts of potassium feldspar in a dark purple-red groundmass. Weathers to white and orange-brown.</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/15"&gt;St. Francois Mountains suite&lt;/a&gt;</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/4ee10b43b24c8c4757ea46f6ecefea71.pdf"&gt;SE Rock Suite&lt;/a&gt;</text>
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                  <text>(FM) Flysch Stratigraphic Suite -- Molasse Basin, Switzerland </text>
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                  <text>Flysch is dominantly a turbidite succession, alternating sandstone and shale 100mm to rarely 100m in syntectonic accumulations. With a rising landmass shedding clastic debris into "deep" troughs, oversteepening of sediments along the shelf or actual tilting of the shell initiated turbidity currents flows deeper into the marine basin. There may be hundreds of these units in a given section. Nappes then over rode the soft sediments, locally producing strong deformational structures in the flysch sediments.Â &lt;br /&gt;&lt;br /&gt;The nappes shed their debris into fresh marine environments in great fans with large accumulations of coarse conglomerates. A molasse section may be a thousand meters thick. Molasse comprises a clastic sedimentary succession in a post-tectonic environment. &lt;br /&gt;&lt;br /&gt;Flysch and molasse both have sedimentatlogical as well as tectonic implications associated with their appearance in an outcrop. Â &lt;br /&gt;&lt;br /&gt;Dr. Trumpy at the Geological Institute in Zurich suggested specific localities for collecting and arranged for Dr. Hanspeter and Mr. Freeman to take me into the field on successive days. Later, Mr. Freeman spent several days in order to procure this suite. &lt;br /&gt;&lt;br /&gt;A set of kodachrome slides is available and should be used with the specimens to put the rocks into relationships seen in the field. There are 11 slide specimens. All slide specimens were photographed in PPL and XPL.</text>
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                  <text>&lt;strong&gt;Start Here:&lt;/strong&gt; &lt;br /&gt;Eynatten, H.V., 2003, Petrology and chemistry of sandstones from the Swiss Molasse Basin: an archive of the Oligocene to Miocene of the Central Alps: Sedimentology, v.50, p.703-724. &lt;a href="http://dx.doi.org/10.1046/j.1365-1309.2003.00571.x"&gt;http://dx.doi.org/10.1046/j.1365-1309.2003.00571.x&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Fluvial sandstones from the Swiss Molasse Basin were analyzed for sandstone framework composition, heavy minerals, whole-rock geochemistry and detrital chrome spinel chemistry to understand its provenance.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;&lt;strong&gt;Additional resources:&lt;/strong&gt; &lt;br /&gt;Schlunegger, F., Matter, A., Burbank, D.W., and Â Klaper, E.M., 1997, Magnetostratigraphic constraints on relationships between evolution of the central Swiss Molasse Basin and Alpine orogenic events: Geological Society of America Bulletin, v.109, p.225-241. &lt;a href="http://dx.doi.org/10.1130/0016-7606(1997)1092.3.CO;2%20"&gt;http://dx.doi.org/10.1130/0016-7606(1997)1092.3.CO;2 &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Magnetostratigraphic chronologies, together with lithostratigraphic, sedimentological, and petrological data enable detailed reconstruction of the Oligocene to Miocene history of the North Alpine foreland basin in relation to specific orogenic events and exhumation of the Alps.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Sinclair, H.D., 1997, Flysch to molasses transition in peripheral foreland basins; the role of the passive margin versus slab breakoff: Geology, v.25, p.1123-1126. &lt;a href="http://dx.doi.org/10.1130/0091-7613(1997)0252.3.CO;2%20"&gt;http://dx.doi.org/10.1130/0091-7613(1997)0252.3.CO;2 &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;It is proposed that slab breakoff may have been responsible for the increased sediment supply that resulted in the flysch to molasse transition in the North Alpine foreland basin, and that this provides an alternative to the passive margin model.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Spiegel, C., Siebel, W., Frisch, W., and Berner, Z., 2002, Nd and Sr isotopic ratios and trace element geochemistry of epidote from the Swiss Molasse Basin as provenance indicators; implications for the reconstruction of the echumation history of the Central Alps: Chemical Geology, v.189, p.231-250.&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Uses a combination of events to explain the geodynamic scenario of large-scale lateral extension processes affecting the Central Alps in post-collisional times.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Willet, S.D. and Schlunegger, F., 2010, The last phase of deposition in the Swiss Molasse Basin; from foredeep to negative-alpha basin: Basin Research, v.22, p.623-639. &lt;a href="http://dx.doi.org/10.1111/j.1365-2117.2009.00435.x%20"&gt;http://dx.doi.org/10.1111/j.1365-2117.2009.00435.x &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Simple analytical theory for the necessary conditions for such a negative-alpha basin to develop and be maintained.&lt;/li&gt;
&lt;/ul&gt;</text>
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                  <text>Typical turbidite sequence rocks (predominantly clastics with some evidence of carbonate input) </text>
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                  <text>In the Late Eocene, the area subsided again and developed into the Molasse Basin. </text>
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                  <text>Turbidite sequences and carbonate pulses of deposition in a basin.</text>
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                  <text>The collection consists of a variety of shale, sandstones and conglomerates that illustrate sediment trapped in a molasse basin. </text>
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                <text>Gray, medium to coarse grained quartz-rich lithic sandstone with rip up clasts and mud rich areas present. &lt;br /&gt;&lt;br /&gt;Thin Section Fine, (.7-.1 mm) sub angular crystal fragments floating in mud matrix, with feldspar, quartz, and pyroxene present.</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/13"&gt;Flysch Molasse Suite&lt;/a&gt;</text>
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                  <text>(FM) Flysch Stratigraphic Suite -- Molasse Basin, Switzerland </text>
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                  <text>Flysch is dominantly a turbidite succession, alternating sandstone and shale 100mm to rarely 100m in syntectonic accumulations. With a rising landmass shedding clastic debris into "deep" troughs, oversteepening of sediments along the shelf or actual tilting of the shell initiated turbidity currents flows deeper into the marine basin. There may be hundreds of these units in a given section. Nappes then over rode the soft sediments, locally producing strong deformational structures in the flysch sediments.Â &lt;br /&gt;&lt;br /&gt;The nappes shed their debris into fresh marine environments in great fans with large accumulations of coarse conglomerates. A molasse section may be a thousand meters thick. Molasse comprises a clastic sedimentary succession in a post-tectonic environment. &lt;br /&gt;&lt;br /&gt;Flysch and molasse both have sedimentatlogical as well as tectonic implications associated with their appearance in an outcrop. Â &lt;br /&gt;&lt;br /&gt;Dr. Trumpy at the Geological Institute in Zurich suggested specific localities for collecting and arranged for Dr. Hanspeter and Mr. Freeman to take me into the field on successive days. Later, Mr. Freeman spent several days in order to procure this suite. &lt;br /&gt;&lt;br /&gt;A set of kodachrome slides is available and should be used with the specimens to put the rocks into relationships seen in the field. There are 11 slide specimens. All slide specimens were photographed in PPL and XPL.</text>
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                  <text>Western Minerals, inc.</text>
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                <elementText elementTextId="17995">
                  <text>&lt;strong&gt;Start Here:&lt;/strong&gt; &lt;br /&gt;Eynatten, H.V., 2003, Petrology and chemistry of sandstones from the Swiss Molasse Basin: an archive of the Oligocene to Miocene of the Central Alps: Sedimentology, v.50, p.703-724. &lt;a href="http://dx.doi.org/10.1046/j.1365-1309.2003.00571.x"&gt;http://dx.doi.org/10.1046/j.1365-1309.2003.00571.x&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Fluvial sandstones from the Swiss Molasse Basin were analyzed for sandstone framework composition, heavy minerals, whole-rock geochemistry and detrital chrome spinel chemistry to understand its provenance.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;&lt;strong&gt;Additional resources:&lt;/strong&gt; &lt;br /&gt;Schlunegger, F., Matter, A., Burbank, D.W., and Â Klaper, E.M., 1997, Magnetostratigraphic constraints on relationships between evolution of the central Swiss Molasse Basin and Alpine orogenic events: Geological Society of America Bulletin, v.109, p.225-241. &lt;a href="http://dx.doi.org/10.1130/0016-7606(1997)1092.3.CO;2%20"&gt;http://dx.doi.org/10.1130/0016-7606(1997)1092.3.CO;2 &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Magnetostratigraphic chronologies, together with lithostratigraphic, sedimentological, and petrological data enable detailed reconstruction of the Oligocene to Miocene history of the North Alpine foreland basin in relation to specific orogenic events and exhumation of the Alps.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Sinclair, H.D., 1997, Flysch to molasses transition in peripheral foreland basins; the role of the passive margin versus slab breakoff: Geology, v.25, p.1123-1126. &lt;a href="http://dx.doi.org/10.1130/0091-7613(1997)0252.3.CO;2%20"&gt;http://dx.doi.org/10.1130/0091-7613(1997)0252.3.CO;2 &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;It is proposed that slab breakoff may have been responsible for the increased sediment supply that resulted in the flysch to molasse transition in the North Alpine foreland basin, and that this provides an alternative to the passive margin model.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Spiegel, C., Siebel, W., Frisch, W., and Berner, Z., 2002, Nd and Sr isotopic ratios and trace element geochemistry of epidote from the Swiss Molasse Basin as provenance indicators; implications for the reconstruction of the echumation history of the Central Alps: Chemical Geology, v.189, p.231-250.&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Uses a combination of events to explain the geodynamic scenario of large-scale lateral extension processes affecting the Central Alps in post-collisional times.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Willet, S.D. and Schlunegger, F., 2010, The last phase of deposition in the Swiss Molasse Basin; from foredeep to negative-alpha basin: Basin Research, v.22, p.623-639. &lt;a href="http://dx.doi.org/10.1111/j.1365-2117.2009.00435.x%20"&gt;http://dx.doi.org/10.1111/j.1365-2117.2009.00435.x &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Simple analytical theory for the necessary conditions for such a negative-alpha basin to develop and be maintained.&lt;/li&gt;
&lt;/ul&gt;</text>
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                  <text>Typical turbidite sequence rocks (predominantly clastics with some evidence of carbonate input) </text>
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              <name>Spatial Coverage</name>
              <description>Spatial characteristics of the resource.</description>
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                  <text>Molasse Basin, Sternenberg, Germany</text>
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              <name>Temporal Coverage</name>
              <description>Temporal characteristics of the resource.</description>
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                <elementText elementTextId="18201">
                  <text>In the Late Eocene, the area subsided again and developed into the Molasse Basin. </text>
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                  <text>Purchased by Western Minerals Inc.</text>
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              <name>Subject</name>
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                <elementText elementTextId="18203">
                  <text>Turbidite sequences and carbonate pulses of deposition in a basin.</text>
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              <name>Abstract</name>
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                  <text>The collection consists of a variety of shale, sandstones and conglomerates that illustrate sediment trapped in a molasse basin. </text>
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              <name>Date</name>
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                  <text>Oct. 10, 2013</text>
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                  <text>FM 1-11</text>
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                <text>Sandstone</text>
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                <text>Fine Sandstone</text>
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                <text>Sandstone with ripple marks and cross bedding and strong flute casts along surface indicating mid-high energy.Â Poorly sorted coarse sandstone with ripple marks, cross bedding and strong flute casts, as well as small pebbles that vary from angular to rounded.&lt;br /&gt;&lt;br /&gt; Thin Section: Fine (.3-.1 mm) poorly sorted grains of quartz, feldspars, and pyroxenes, varying from angular to sub rounded, closely packed in a mud matrix where applicable. &lt;br /&gt;&lt;br /&gt;</text>
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                <text>Western Minerals, lnc.</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/13"&gt;Flysch Molasse Suite&lt;/a&gt;</text>
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                <text>Renggloch, Germany</text>
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                <text>Purchased from Western Minerals, Inc.</text>
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              <elementText elementTextId="18288">
                <text>Oct., 11, 2013</text>
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            <name>Temporal Coverage</name>
            <description>Temporal characteristics of the resource.</description>
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                <text>Mesozoic</text>
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                  <text>2nd Floor ISC Fossil Display Cases</text>
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                <text>Sandstone with bivalve borings (trace fossil)</text>
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                <text>2nd floor hallway, display case 12</text>
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                <text>R.B. Marshall, C.H. Birdseye, Glenn S. Smith, C.G. Anderson, C.C. Holder, S.T. Penick, R.R. Monbeck, D.S. Birkett, Arthur Stiles</text>
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                <text>US Geological Survey</text>
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                <text>Bone Spring, Nine Point Mesa, Agua Fria, Hood Spring, Marathon, Monument Spring, Buck Hill</text>
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            <name>Is Part Of</name>
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                <text>"One Hundred Topograhpic Maps Illustrating Specific Physiographic Features"</text>
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            <element elementId="50">
              <name>Title</name>
              <description>A name given to the resource</description>
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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 elementId="37">
              <name>Contributor</name>
              <description>An entity responsible for making contributions to the resource</description>
              <elementTextContainer>
                <elementText elementTextId="17794">
                  <text>Western Minerals, Inc.</text>
                </elementText>
              </elementTextContainer>
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            <element elementId="40">
              <name>Date</name>
              <description>A point or period of time associated with an event in the lifecycle of the resource</description>
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                  <text>1969</text>
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            <element elementId="43">
              <name>Identifier</name>
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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>
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            <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>
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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="17823">
                  <text>Purchased from Western Minerals, Inc. </text>
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            <element elementId="109">
              <name>References</name>
              <description>A related resource that is referenced, cited, or otherwise pointed to by the described resource.</description>
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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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      <name>Rock</name>
      <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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              <text>1</text>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Scoria </text>
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          <element elementId="41">
            <name>Description</name>
            <description>An account of the resource</description>
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                <text>Hand Sample: Microcrystalline vesicular, dark-gray to black scoria. Vesicle size varies throughout the sample, ranging from larger circular vesicles with a diameter of approx. 1.5 cm on one surface and small vesicles (less than 0.1cm in diameter) on the opposite face. Sample has low specific gravity due to abundance of vesicles. </text>
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                <text>Thin Section : Groundmass composed of glass and microcrystaline grains of plagioclase. Large elongated vesicles are observed throughout the thin section.  </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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                <text>Western Minerals</text>
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            <name>Is Part Of</name>
            <description>A related resource in which the described resource is physically or logically included.</description>
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                <text>Volcanic Phenomena Suite - The Hawaiian Islands of Hawaii and Oahu</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>HA-26</text>
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            <name>Spatial Coverage</name>
            <description>Spatial characteristics of the resource.</description>
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                <text>Hualalai - 9 miles north of Hohokahua - Island of Hawaii&#13;
Sample collected just above HA-25. Collected just North of Relay Tower and approx. one mile southeast of the highway.</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="16462">
                <text>1801</text>
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          <element elementId="40">
            <name>Date</name>
            <description>A point or period of time associated with an event in the lifecycle of the resource</description>
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              <elementText elementTextId="18563">
                <text>Sample collected in January, 1969.</text>
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