<?xml version="1.0"?>
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" article-type="research-article" dtd-version="1.2" xml:lang="ru" xlink="http://www.w3.org/1999/xlink"><front><journal-meta><journal-id journal-id-type="publisher-id">&#x413;&#x435;&#x43E;&#x43B;&#x43E;&#x433;&#x438;&#x44F; &#x438; &#x413;&#x435;&#x43E;&#x444;&#x438;&#x437;&#x438;&#x43A;&#x430; &#x42E;&#x433;&#x430; &#x420;&#x43E;&#x441;&#x441;&#x438;&#x438;</journal-id><journal-title-group><journal-title>&#x413;&#x435;&#x43E;&#x43B;&#x43E;&#x433;&#x438;&#x44F; &#x438; &#x413;&#x435;&#x43E;&#x444;&#x438;&#x437;&#x438;&#x43A;&#x430; &#x42E;&#x433;&#x430; &#x420;&#x43E;&#x441;&#x441;&#x438;&#x438;</journal-title></journal-title-group><issn publication-format="print">2221-3198</issn><publisher><publisher-name>&#x424;&#x435;&#x434;&#x435;&#x440;&#x430;&#x43B;&#x44C;&#x43D;&#x43E;&#x435; &#x433;&#x43E;&#x441;&#x443;&#x434;&#x430;&#x440;&#x441;&#x442;&#x432;&#x435;&#x43D;&#x43D;&#x43E;&#x435; &#x431;&#x44E;&#x434;&#x436;&#x435;&#x442;&#x43D;&#x43E;&#x435; &#x443;&#x447;&#x440;&#x435;&#x436;&#x434;&#x435;&#x43D;&#x438;&#x435; &#x43D;&#x430;&#x443;&#x43A;&#x438; &#x424;&#x435;&#x434;&#x435;&#x440;&#x430;&#x43B;&#x44C;&#x43D;&#x44B;&#x439; &#x43D;&#x430;&#x443;&#x447;&#x43D;&#x44B;&#x439; &#x446;&#x435;&#x43D;&#x442;&#x440;  "&#x412;&#x43B;&#x430;&#x434;&#x438;&#x43A;&#x430;&#x432;&#x43A;&#x430;&#x437;&#x441;&#x43A;&#x438;&#x439; &#x43D;&#x430;&#x443;&#x447;&#x43D;&#x44B;&#x439; &#x446;&#x435;&#x43D;&#x442;&#x440; &#x420;&#x43E;&#x441;&#x441;&#x438;&#x439;&#x441;&#x43A;&#x43E;&#x439; &#x430;&#x43A;&#x430;&#x434;&#x435;&#x43C;&#x438;&#x438; &#x43D;&#x430;&#x443;&#x43A;"</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">510</article-id><article-id pub-id-type="doi"/><article-categories><subj-group subj-group-type="heading"><subject>&#x421;&#x442;&#x430;&#x442;&#x44C;&#x438;</subject></subj-group></article-categories><title-group><article-title>GLACIAL AND PERIGLACIAL PROCESSES OF GEORGIA</article-title></title-group><contrib-group><contrib contrib-type="author"><name name-style="eastern" xml:lang="ru"><surname>&#x411;&#x43E;&#x43D;&#x434;&#x44B;&#x440;&#x435;&#x432;</surname><given-names>&#x418;. &#x412;.</given-names></name><xref ref-type="aff" rid="aff-aff-1"/></contrib></contrib-group><aff id="aff-aff-1">&#x422;&#x431;&#x438;&#x43B;&#x438;&#x441;&#x441;&#x43A;&#x438;&#x439; &#x433;&#x43E;&#x441;&#x443;&#x434;&#x430;&#x440;&#x441;&#x442;&#x432;&#x435;&#x43D;&#x43D;&#x44B;&#x439; &#x443;&#x43D;&#x438;&#x432;&#x435;&#x440;&#x441;&#x438;&#x442;&#x435;&#x442; &#x438;&#x43C;. &#x418;. &#x414;&#x436;&#x430;&#x432;&#x430;&#x445;&#x438;&#x448;&#x432;&#x438;&#x43B;&#x438;, &#x413;&#x440;&#x443;&#x437;&#x438;&#x44F;, 0179, &#x433;. &#x422;&#x431;&#x438;&#x43B;&#x438;&#x441;&#x438;, &#x43F;&#x440;. &#x427;&#x430;&#x432;&#x447;&#x430;&#x432;&#x430;&#x434;&#x437;&#x435;, 1</aff><pub-date date-type="pub" iso-8601-date="2014-06-03" publication-format="electronic"><day>03</day><month>06</month><year>2014</year></pub-date><issue>4</issue><fpage>51</fpage><lpage>62</lpage><permissions><copyright-statement>Copyright (c) 2013 &#x413;&#x435;&#x43E;&#x43B;&#x43E;&#x433;&#x438;&#x44F; &#x438; &#x433;&#x435;&#x43E;&#x444;&#x438;&#x437;&#x438;&#x43A;&#x430; &#x42E;&#x433;&#x430; &#x420;&#x43E;&#x441;&#x441;&#x438;&#x438;</copyright-statement><copyright-year>2013</copyright-year><copyright-holder>&#x413;&#x435;&#x43E;&#x43B;&#x43E;&#x433;&#x438;&#x44F; &#x438; &#x433;&#x435;&#x43E;&#x444;&#x438;&#x437;&#x438;&#x43A;&#x430; &#x42E;&#x433;&#x430; &#x420;&#x43E;&#x441;&#x441;&#x438;&#x438;</copyright-holder></permissions><self-uri href="https://geosouth.ru/article/view/510"/><abstract>There are about 786 glaciers registered in the mountains of Georgia. The possible consequences of human activity on the whole geodynamic system of the Caucasus are discussed. Geography of glaciers, glacial melting, avalanches, cryogenic processes, classification of periglacial formations and impact of cryogenic processes are studied.</abstract><kwd-group xml:lang="ru"><kwd>Glaciers</kwd><kwd>avalanches</kwd><kwd>cryogenic processes</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>Glaciers</kwd><kwd>avalanches</kwd><kwd>cryogenic processes</kwd></kwd-group></article-meta></front><body/><back><ref-list/></back></article>
