<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD JATS (Z39.96) Journal Publishing DTD v1.3 20210610//EN" "JATS-journalpublishing1-3.dtd">
<article article-type="research-article" dtd-version="1.3" 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" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">geomorf</journal-id><journal-title-group><journal-title xml:lang="ru">Геоморфология и палеогеография</journal-title><trans-title-group xml:lang="en"><trans-title>Geomorfologiya i Paleogeografiya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2949-1789</issn><issn pub-type="epub">2949-1797</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">geomorf-3505</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>Научные сообщения</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Short communications</subject></subj-group></article-categories><title-group><article-title>Особенности развития овражной эрозии в Восточном Закамье Татарстана</article-title><trans-title-group xml:lang="en"><trans-title>Peculiar features of gully erosion in the eastern territories of Tatarstan over Kama river</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Серебренникова</surname><given-names>И. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Serebrennikova</surname><given-names>I. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Казанский государственный университет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1998</year></pub-date><pub-date pub-type="epub"><day>21</day><month>12</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>101</fpage><lpage>104</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Серебренникова И.А., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Серебренникова И.А.</copyright-holder><copyright-holder xml:lang="en">Serebrennikova I.A.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://geomorphology.igras.ru/jour/article/view/3505">https://geomorphology.igras.ru/jour/article/view/3505</self-uri><abstract><p>Gully erosion development in the easter over Kama region is compared with that of the other regions of Tatarstan. Drainage density and depth of erosion cutting in the region are of maximum values in Tatarstan, the slopes are very large, but the gully density is of minimum value. The main causes of this peculiarity are shown.</p></abstract><trans-abstract xml:lang="en"><p>Gully erosion development in the easter over Kama region is compared with that of the other regions of Tatarstan. Drainage density and depth of erosion cutting in the region are of maximum values in Tatarstan, the slopes are very large, but the gully density is of minimum value. The main causes of this peculiarity are shown.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
