<?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-2173</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>Овражная эрозия Нижегородского Предволжья и ее динамика</article-title><trans-title-group xml:lang="en"><trans-title>Gully erosion in the Fore-Volga region of Nizhny Novgorod district</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>Пияшова</surname><given-names>С. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Piyashova</surname><given-names>S. N.</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>Нижегородский государственный педагогический университет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2003</year></pub-date><pub-date pub-type="epub"><day>16</day><month>07</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>92</fpage><lpage>97</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Пияшова С.Н., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Пияшова С.Н.</copyright-holder><copyright-holder xml:lang="en">Piyashova S.N.</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/2173">https://geomorphology.igras.ru/jour/article/view/2173</self-uri><abstract><p>The article deals with spatial and temporal variability of gully erosion within the region. On the basis of large-scale aerial data the density of gully network was determined and zoning of territory by this characteristic was fulfilled. Conjunctions of spatial differentiation of gully network with tilling degree, amount of woodland, relief, surface rocks were determined. The area dynamics of arable land and woodland during last four centuries was analyzed and these data were juxtaposed with gully network dynamics. Aerial data with 40 years lag show the distinct degressive trend of gully erosion in the second half of the XX century; the cause of this phenomenon is described.</p><p> </p></abstract><trans-abstract xml:lang="en"><p>The article deals with spatial and temporal variability of gully erosion within the region. On the basis of large-scale aerial data the density of gully network was determined and zoning of territory by this characteristic was fulfilled. Conjunctions of spatial differentiation of gully network with tilling degree, amount of woodland, relief, surface rocks were determined. The area dynamics of arable land and woodland during last four centuries was analyzed and these data were juxtaposed with gully network dynamics. Aerial data with 40 years lag show the distinct degressive trend of gully erosion in the second half of the XX century; the cause of this phenomenon is described.</p><p> </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>
