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<front>
<journal-meta>
<journal-id journal-id-type="publisher">CPD</journal-id>
<journal-title-group>
<journal-title>Climate of the Past Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">CPD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Clim. Past Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1814-9359</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/cp-2016-101</article-id>
<title-group>
<article-title>Glacio-archaeological evidence of warmer climate during the Little Ice Age
in the Miyar basin, Lahul Himalaya, India</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Saini</surname>
<given-names>Rakesh</given-names>
<ext-link>https://orcid.org/0000-0003-4165-7423</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sharma</surname>
<given-names>Milap Chand</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Deswal</surname>
<given-names>Sanjay</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Barr</surname>
<given-names>Iestyn David</given-names>
<ext-link>https://orcid.org/0000-0002-9066-8738</ext-link>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kumar</surname>
<given-names>Parvendra</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of General &amp; Applied Geograp hy, Dr. Harisingh Gour Central University, Sagar, 470003, India</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Centre for the Study of Regional Development, Jawaharlal Nehru University,  New Delhi, 110067, India</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Geography, Government College Dujana, Dujana , 124102, India</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>School of Natural and Built Environment, Queen’s University, Belfast,  BT7 1NN,  United Kingdom</addr-line>
</aff>
<pub-date pub-type="epub">
<day>07</day>
<month>11</month>
<year>2016</year>
</pub-date>
<volume>2016</volume>
<fpage>1</fpage>
<lpage>24</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2016 Rakesh Saini et al.</copyright-statement>
<copyright-year>2016</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://cp.copernicus.org/preprints/cp-2016-101/">This article is available from https://cp.copernicus.org/preprints/cp-2016-101/</self-uri>
<self-uri xlink:href="https://cp.copernicus.org/preprints/cp-2016-101/cp-2016-101.pdf">The full text article is available as a PDF file from https://cp.copernicus.org/preprints/cp-2016-101/cp-2016-101.pdf</self-uri>
<abstract>
<p>Impressive glacio-archaeological evidence is described from the Miyar basin, Lahul Himalaya, India. Three ruins, namely Tharang, Phundang and Patam are identified along with evidence for past settlement and rich irrigation practices in the basin. These ruins are located in the end moraine complex of Tharang glacier, just ~&amp;thinsp;2&amp;ndash;3&amp;thinsp;km from the present glacier snout. Reconstruction of these ruins was undertaken based on mapping and radiocarbon (&lt;sup&gt;14&lt;/sup&gt;C) dating. The radiocarbon dates (9 samples were dated) indicate that the settlement was occupied between cal AD ~&amp;thinsp;1170 and cal AD ~&amp;thinsp;1730, thereby encompassing the majority of Little Ice Age period. The settlement’s occupation at ~&amp;thinsp;3700&amp;thinsp;m&amp;thinsp;a.s.l. (whereas present habitation is restricted to areas below ~&amp;thinsp;3500&amp;thinsp;m&amp;thinsp; a.s.l.) for almost ~&amp;thinsp;550 years during the 12&lt;sup&gt;th&lt;/sup&gt; to 17&lt;sup&gt;th&lt;/sup&gt; centuries suggest warmer conditions than today. Moreover, the study finds no evidence to suggest any noticeable glacier advance during this period.</p>
</abstract>
<counts><page-count count="24"/></counts>
</article-meta>
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