Proceedings of the 3rd International Conference on Social Sciences (ICSS 2020)

Study Area Geomorphology Manado

Authors
Rosita Treny Selvana Tewal, Helena Sri Sulastriningsih, Jelly Robot
Corresponding Author
Rosita Treny Selvana Tewal
Available Online 15 October 2020.
DOI
10.2991/assehr.k.201014.038How to use a DOI?
Keywords
Geomorphology, geomorphological processes, geomorphological map
Abstract

The problem in this research is the variety of topography, rock and rainfall conditions Manado City, all of which affect the condition of geomorphology and geomorphological processes in Manado Interest implemented this research is to assess the condition of geomorphology and geomorphological mapping the city of Manado. The method to be used include the analysis of maps, aerial photo interpretation, field observations to produce a map of geomorphology or landform geomorphology Manado based map will be obtained information about the land form the city of Manado, subsequently combined with the results of the field observations in order to obtain information about the process geomorphology happens in each landform in Manado City Research results show the city of Manado based Map Geomorphology in morphogenesis landform Manado City consists of three classifications namely landform origin process Fluvial, landform origin denudational process and landform Volcanic origin. Conditions morphometry and morphography Manado, as follows, morphometry indicated by the slope of 0% to> 15%, and morphography include flood plains, alluvial plains, hills denudasional eroded medium, denudational hills eroded strong, slope amid volcano, the lower slopes of volcanoes and slopes foot volcano. Morfoassociation aspects occur because of the collaboration of various factors of the topography, constituent material, and precipitation. Tangible erosion, landslides and sedimentation collectible the three landforms in Manado City ie landforms Fluvial, denudational and landforms Volcanic, while morphochronology drawn from the condition of the material making up the rate of development varies from erosion / stadium young to old are seen from the rock material eroded further even the outcrop, as well as chunks of rock to the ground.

Copyright
© 2020, the Authors. Published by Atlantis Press.
Open Access
This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

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Volume Title
Proceedings of the 3rd International Conference on Social Sciences (ICSS 2020)
Series
Advances in Social Science, Education and Humanities Research
Publication Date
15 October 2020
ISBN
10.2991/assehr.k.201014.038
ISSN
2352-5398
DOI
10.2991/assehr.k.201014.038How to use a DOI?
Copyright
© 2020, the Authors. Published by Atlantis Press.
Open Access
This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

Cite this article

TY  - CONF
AU  - Rosita Treny Selvana Tewal
AU  - Helena Sri Sulastriningsih
AU  - Jelly Robot
PY  - 2020
DA  - 2020/10/15
TI  - Study Area Geomorphology Manado
BT  - Proceedings of the 3rd International Conference on Social Sciences (ICSS 2020)
PB  - Atlantis Press
SP  - 171
EP  - 174
SN  - 2352-5398
UR  - https://doi.org/10.2991/assehr.k.201014.038
DO  - 10.2991/assehr.k.201014.038
ID  - Tewal2020
ER  -