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• W2108068350 abstract "Research Article| May 01, 1990 Stonelines and landscape development on the laterized craton of Madagascar NEIL A. WELLS; NEIL A. WELLS 1Geology Department, Kent State University, Kent, Ohio 44242 Search for other works by this author on: GSW Google Scholar BENJAMIN ANDRIAMIHAJA; BENJAMIN ANDRIAMIHAJA 2Ministère de l'Etablissement d'Enseignement Supérieur des Sciences, B.P. 4163, Tsimbazaza, Antananarivo, Madagascar Search for other works by this author on: GSW Google Scholar H.F.S. RAKOTOVOLOLONA H.F.S. RAKOTOVOLOLONA 3Musée d Art et d'Archéologie, 17, Rue Dr. Villette, Isoraka, Antananarivo, Madagascar Search for other works by this author on: GSW Google Scholar Author and Article Information NEIL A. WELLS 1Geology Department, Kent State University, Kent, Ohio 44242 BENJAMIN ANDRIAMIHAJA 2Ministère de l'Etablissement d'Enseignement Supérieur des Sciences, B.P. 4163, Tsimbazaza, Antananarivo, Madagascar H.F.S. RAKOTOVOLOLONA 3Musée d Art et d'Archéologie, 17, Rue Dr. Villette, Isoraka, Antananarivo, Madagascar Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (1990) 102 (5): 615–627. https://doi.org/10.1130/0016-7606(1990)102<0615:SALDOT>2.3.CO;2 Article history First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation NEIL A. WELLS, BENJAMIN ANDRIAMIHAJA, H.F.S. RAKOTOVOLOLONA; Stonelines and landscape development on the laterized craton of Madagascar. GSA Bulletin 1990;; 102 (5): 615–627. doi: https://doi.org/10.1130/0016-7606(1990)102<0615:SALDOT>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract In Madagascar, stonelines (horizons of quartz pebbles in laterites) are buried colluvial and alluvial lag gravels that outline former hill and valley surfaces. Their fabrics, especially rare multiple stone layers, identify the stonelines as old surface lags, and the immature geochemical compositions of their over-burdens relative to their substrates demonstrate burial by colluvium. Hill-mantling stonelines are convex upward and less well developed, whereas those lining valleys are concave to irregular, thicker, deeper, better packed and sorted, and have more rounded stones. Local differences in position between former and modern landforms demonstrate that, in a complexly and tightly folded metamorphic terrain, hills and valleys are likely to shift as the landscape is lowered by weathering, thus implying that the landscape is held at a relatively submature stage of development. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2108068350 title "Stonelines and landscape development on the laterized craton of Madagascar" @default.
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