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The Use of Infra Red Aerial Photo for Identification the Existance and Spread of Cave in Planning sub District, Eromoko District, Wonogiri Regency

Forum Geografi · Vol. 15 No. 1 (2016) · hlm. 46–59

DOI
10.23917/forgeo.v15i1.4662
ISSN
2460-3945, 0852-0682
Terbit
2016-07-20
Penerbit
Universitas Muhammadiyah Surakarta
Bahasa
eng
Lisensi
creativecommons.org/licenses/by-nc-nd/4.0

Abstrak

Science that studied all of the aspect related to cave and their circles (speleology) in Indonesia does not still quite expand. Expantion more advanced need all sorts of research, publication and its interest to an academic party who get in touch with cave and their circles. One of them the basic of data collection about the existence and the spread of cave. The usual manner that is used to know the existence and the spread of cave, is by means of the analysis topography map which is continued by terrestrial research. Weakness for this manner is it need huge time, cost and energy. The making use of aerial photo can be done in supporting the basic of date collection, is the· interpretation to bug or detect appearances the phenomena in earth’s surface. One of them is appearances the edge of cave. The result of the research indicates that interpretation of aerial photo can be use to identify the spread of the edge of cave. It is olksified according to; the edge that obtained of center depression by the accuracy of 100%; the edge of cave that obtained of slope depression (the accuracy of 33.3%); the edge of cave that is obtained of river current (the accuracy of 100%); and the edge of cave that obtained of fragment (the accuracy of 50%).

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  • Muhammadiyah University of Surakarta
  • Universitas Gadjah Mada
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Rekan penulisOrganisasiArtikel bersama
Alif Noor AnnaMuhammadiyah University of Surakarta3
Yuli PriyanaMuhammadiyah University of Surakarta3
Taryono TaryonoUniversitas Gadjah Mada2
Suharto WidjojoAfiliasi tidak diketahui2
Pujo Nur CahyoMuhammadiyah University of Surakarta2
M MulyonoMuhammadiyah University of Surakarta2
Heru Sri WidodoMuhammadiyah University of Surakarta2
Retno Woro KaeksiMuhammadiyah University of Surakarta1
Munawar CholilMuhammadiyah University of Surakarta1
‪Kuswaji Dwi PriyonoMuhammadiyah University of Surakarta1
T TaryonoMuhammadiyah University of Surakarta1
Adi RusmantoAfiliasi tidak diketahui1

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Sumber metadata: OAI-PMH (metadata jurnal) http://journals.ums.ac.id/index.php/fg/oai, pertama di-harvest 8 Nov 2026, terakhir terlihat 8 Nov 2026.
Metadata asli (oai_dc) 
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	<dc:title xml:lang="en-US">The Use of Infra Red Aerial Photo for Identification the Existance and Spread of Cave in Planning sub District, Eromoko District, Wonogiri Regency</dc:title>
	<dc:creator>Suharjo, S</dc:creator>
	<dc:creator>Santoso, Sugiharto Budi</dc:creator>
	<dc:creator>Purnaningsih, Reshinta</dc:creator>
	<dc:creator>Suryanto, S</dc:creator>
	<dc:creator>Prasetyo, Yuliarta Rudi</dc:creator>
	<dc:subject xml:lang="en-US"></dc:subject>
	<dc:subject xml:lang="en-US">Aerial photo interpretation; cave; accuracy of Interpretation</dc:subject>
	<dc:subject xml:lang="en-US"></dc:subject>
	<dc:description xml:lang="en-US">Science that studied all of the aspect related to cave and their circles (speleology) in Indonesia does not still quite expand. Expantion more advanced need all sorts of research, publication and its interest to an academic party who get in touch with cave and their circles. One of them the basic of data collection about the existence and the spread of cave. The usual manner that is used to know the existence and the spread of cave, is by means of the analysis topography map which is continued by terrestrial research. Weakness for this manner is it need huge time, cost and energy. The making use of aerial photo can be done in supporting the basic of date collection, is the· interpretation to bug or detect appearances the phenomena in earth’s surface. One of them is appearances the edge of cave. The result of the research indicates that interpretation of aerial photo can be use to identify the spread of the edge of cave. It is olksified according to; the edge that obtained of center depression by the accuracy of 100%; the edge of cave that obtained of slope depression (the accuracy of 33.3%); the edge of cave that is obtained of river current (the accuracy of 100%); and the edge of cave that obtained of fragment (the accuracy of 50%).</dc:description>
	<dc:publisher xml:lang="en-US">Universitas Muhammadiyah Surakarta</dc:publisher>
	<dc:contributor xml:lang="en-US"></dc:contributor>
	<dc:date>2016-07-20</dc:date>
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	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://journals.ums.ac.id/index.php/fg/article/view/4662</dc:identifier>
	<dc:identifier>10.23917/forgeo.v15i1.4662</dc:identifier>
	<dc:source xml:lang="en-US">Forum Geografi; Vol 15, No 1 (2001): July 2001; 46-59</dc:source>
	<dc:source>2460-3945</dc:source>
	<dc:source>0852-0682</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://journals.ums.ac.id/index.php/fg/article/view/4662/3049</dc:relation>
	<dc:coverage xml:lang="en-US"></dc:coverage>
	<dc:coverage xml:lang="en-US"></dc:coverage>
	<dc:coverage xml:lang="en-US"></dc:coverage>
	<dc:rights xml:lang="en-US">Copyright (c) 2017 S Suharjo, Sugiharto Budi Santoso, Reshinta Purnaningsih, S Suryanto, Yuliarta Rudi Prasetyo</dc:rights>
	<dc:rights xml:lang="en-US">https://creativecommons.org/licenses/by-nc-nd/4.0</dc:rights>
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