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<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 pub-id-type="doi">10.15356/0435-4281-1970-2-19-27</article-id><article-id custom-type="elpub" pub-id-type="custom">geomorf-842</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>Общетеоретические статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Articles</subject></subj-group></article-categories><title-group><article-title>ВОПРОСЫ ГЕОМОРФОЛОГИИ ИНДОСТАНА</article-title><trans-title-group xml:lang="en"><trans-title>PROBLEMS   OF   GEOMORPHOLOGY   OF   HINDUSTAN</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>Николаев</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Nikolaev</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Географический факультет</p></bio><bio xml:lang="en"><p>Faculty of Geography</p></bio><email xlink:type="simple">geomorfologiya@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Московский государственный университет имени М.В. Ломоносова</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Lomonosov Moscow State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1970</year></pub-date><pub-date pub-type="epub"><day>18</day><month>08</month><year>2016</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>19</fpage><lpage>27</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Николаев В.А., 2016</copyright-statement><copyright-year>2016</copyright-year><copyright-holder xml:lang="ru">Николаев В.А.</copyright-holder><copyright-holder xml:lang="en">Nikolaev V.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/842">https://geomorphology.igras.ru/jour/article/view/842</self-uri><abstract><p>Проблемы происхождения и возраста поверхностей выравнивания полуостровной глыбы Индостана расcмотрены параллельно с морфоструктурным анализом территории. Отмечается большая древность речных долин и связь их с региональными разломами. Береговые линии Индостана свидетельствуют о колебаниях уровня океана и тектонических подвижках побережья в плейстоцене. Предложена морфоструктурная классификация рельефа.</p></abstract><trans-abstract xml:lang="en"><p>Problems of the origin and age of planation surfaces in the peninsular block of Hindustan are discussed alongside a morphostructural analysis of the area. It is noted that the river valleys are very ancient and are related to regional fractures. The shore line of Hindustan reveals sea-level fluctuations and tectonic movements of the coast in Pleistocene. A morphostructural classification of the relief is suggested.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Дикси Ф. Великие африканские разломы. 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