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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Geology theses</text>
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    <name>OU Geology thesis</name>
    <description>Thesis or dissertation completed by University of Otago Geology students</description>
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        <name>Location WKT (WGS84)</name>
        <description>The location stored in WKT (WGS84) format</description>
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            <text>POLYGON ((170.833569714077868 -45.480909668997462,170.826016586578646 -45.481528209131739,170.818423885718715 -45.481764438674958,170.806919294742897 -45.478114543899657,170.798941504684763 -45.474341004045343,170.791016875956558 -45.469234238994197,170.778599025090756 -45.461372193729275,170.766447785460343 -45.446845514993981,170.780347319610314 -45.416822534307272,170.777297820358541 -45.38284893635899,170.798056283203096 -45.384394380078035,170.833004973224917 -45.389635807115276,170.850373565071635 -45.395108455896086,170.841303535762535 -45.398938441629141,170.838149165171131 -45.403641991732428,170.830903378717039 -45.409220438313106,170.824678954061312 -45.416342118247258,170.821412308041403 -45.423900988149732,170.818115397194589 -45.432221292414134,170.816338695872304 -45.436188423805447,170.814729234866832 -45.442826123229018,170.812556303282861 -45.45002458350497,170.815544832483369 -45.456750282547759,170.827828088046488 -45.461176249339665,170.832764143085228 -45.466604827112569,170.835521751087271 -45.472372963533324,170.833569714077868 -45.480909668997462))</text>
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        <name>Author last name</name>
        <description>Last name of the Author</description>
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            <text>Douglas</text>
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        <name>Project type</name>
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            <text>PGDipSci</text>
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        <name>Advisers</name>
        <description>Who supervised/advised this student</description>
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            <text>Carter, R.M.</text>
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      <element elementId="55">
        <name>Abstract</name>
        <description>The Abstract for this thesis</description>
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            <text>Upper Cretaceous terrestrial sediments derived from a fault scarp formed in the Rangitata Orogeny were deposited in a tectonic valley. With rapid erosion, peneplanation conditions prevailed inland. Near the coast deltaic and swamp environments existed prior to a marine transgression in the Haumurian. The succeeding Notocene marine units have been examined inn some detail in order to determine the environment in which they were deposited. In later Tertiary times the sediments were subject to folding and faulting of the Kaikoura orogeny. Marine beach sands and loess were deposited in the area during the fluctuating Pleistocene sea-levels.</text>
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        <name>Department</name>
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            <text>Geology</text>
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        <name>Named locality</name>
        <description>Named locality describing the field area location.</description>
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            <text>Shag Point</text>
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            <text> Pukehiwaitahi</text>
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        <name>Thesis description</name>
        <description>Number of pages, maps, CDs, etc.</description>
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            <text>v, 82, lxvii leaves : ill. (some col.), maps (some col.) ; 30 cm.</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>1970Douglas</text>
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          <name>Creator</name>
          <description>An entity primarily responsible for making the resource</description>
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            <elementText elementTextId="29702">
              <text>Douglas, Barry John.</text>
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          <name>Date</name>
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            <elementText elementTextId="29703">
              <text>1970</text>
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        <element elementId="50">
          <name>Title</name>
          <description>A name given to the resource</description>
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            <elementText elementTextId="29705">
              <text>Post eruption deposition from the 10 June 1886, Mt Tarawera eruption </text>
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          <name>Subject</name>
          <description>The topic of the resource</description>
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              <text>Map</text>
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              <text> Sedimentology</text>
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      <name>Notocene</name>
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