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Relevant bibliographies by topics / Limestone landform

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Academic literature on the topic 'Limestone landform'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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Journal articles on the topic "Limestone landform"

1

Thamodi, A. A. R., and B. A. S. C. Kumara. "A geological study on the importance of a limestone cave (with special reference to waulpane cave in Ratnapura District)." South Florida Journal of Development 6, no. 3 (2025): e5041. https://doi.org/10.46932/sfjdv6n3-009.

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Karsts are truly ‘living landscapes’ as they are the outcome of complex interplay between geology, climate, hydrology, and biological factors over a long period of time. Karst landscape is a collection of surface and subterranean landforms, formed through the dissolution of soluble bedrocks mainly limestone. Limestone caves or solutional caves are the most important and the main landform of karst landscape. Sri Lanka consists of several limestone caves mainly in Sabaragamuwa, Uva and Central provinces. Waulpane limestone cave in Pallebedda, Ratnapura district is important due to its geological

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2

Indra Agus Riyanto, Ahmad Cahyadi, Dwi Sismoyo, Azura Ulfa, Wilda Aulia Fathoni, and Ghalih Nur Wicaksono. "Geomorfologi Tanah Pada Transisi Geologi Formasi Wonosari dan Nglanggran di Kecamatan Purwosari Gunungkidul Yogyakarta." Jurnal Geografi, Edukasi dan Lingkungan (JGEL) 6, no. 2 (2022): 74–86. http://dx.doi.org/10.22236/jgel.v6i2.9072.

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The transition zone of the Wonosari and Nglanggran Formation in Purwosari District has the characteristics of thick soil, steep slopes, and no outcrops. The different characteristics found in the Wonosari Formation Zone are characterized by polygonal karst formations with thin soil and limestone rocks, and the Nglanggran Formation in the form of thick soil, andesite rock outcrops, and steep slopes. Geomorphological mapping of the Nglanggran and Wonosari Formation can be done easily through morphological approaches and outcrops. Geomorphological mapping is quite difficult to do in the transitio

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3

Paterson, Keith. "Limestone landform studies and their curriculum applications." Earth Surface Processes and Landforms 12, no. 5 (1987): 575–81. http://dx.doi.org/10.1002/esp.3290120516.

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4

Arif Pambudi, Ridwan, Ahmad Bahtiazhar Rodhial Falah, Ari Naldi, et al. "Satellite imagery detection of land destruction in Klapanunggal Karst Landscape induced by limestone surface mining." E3S Web of Conferences 211 (2020): 04002. http://dx.doi.org/10.1051/e3sconf/202021104002.

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Limestone mining activities in the Klapanunggal Karst Landscape were carried out at surface level. This method induced several adverse impacts on the environment. This study aimed to detect land destruction in the Klapanunggal Karst Landscape triggered by open limestone mining on the surface in the 2014-2020 period. The supervised classification method of Maximum Likelihood Estimation (MLE) was used to detect the change in land cover from Landsat 8 imagery, and Differential Interferometric Synthetic Aperture Radar (DInSAR) was applied to detect the change in landform from Sentinel 1A imagery.

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Bailey, D., and J. Gunn. "Landform Replication Research in Two English Limestone Quarries." Journal American Society of Mining and Reclamation 1992, no. 1 (1992): 487–96. http://dx.doi.org/10.21000/jasmr92010487.

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6

Ding, Cong, Ang Liu, Xun-Lin Yu, and Chun-Ping Zhang. "Primulina cataractarum sp. nov. (Gesneriaceae) from limestone landform in Southern Hunan, China." Phytotaxa 511, no. 1 (2021): 51–64. https://doi.org/10.11646/phytotaxa.511.1.4.

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Ding, Cong, Liu, Ang, Yu, Xun-Lin, Zhang, Chun-Ping (2021): Primulina cataractarum sp. nov. (Gesneriaceae) from limestone landform in Southern Hunan, China. Phytotaxa 511 (1): 51-64, DOI: 10.11646/phytotaxa.511.1.4, URL: http://dx.doi.org/10.11646/phytotaxa.511.1.4

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Maulana, Karina Meiyanti, Langgeng Wahyu Santosa, and Tjahyo Nugroho Adji. "Groundwater Potential in Unconfined Aquifers Using a Landform Approach in Gorontalo City." Jambura Geoscience Review 5, no. 1 (2023): 22–32. http://dx.doi.org/10.34312/jgeosrev.v5i1.15185.

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This research aimed to determine the potential of the unconfined aquifer in Gorontalo City based on the landform approach. The landforms in Gorontalo City consist of alluvial plains of lake deposits, floodplains of river deposits, alluvial fans of lake deposits, hills of structural fractures of reef limestones, hills of structural fractures of pinogu volcanic rocks, and hills of intrusive bone diorite. The method used consisted of a meteorological approach in the southern hills of Gorontalo City and a dynamic approach on the plains of Gorontalo City. The calculation of groundwater availability

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Liu, Ang, Xiong Li, Guo-xing Deng, et al. "Cardamine mangshanensis, a new species of Brassicaceae from limestone landform in Southern Hunan, China." PhytoKeys 256 (May 21, 2025): 131–39. https://doi.org/10.3897/phytokeys.256.153110.

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<i>Cardamine mangshanensis</i>, a new species, is described and illustrated from the limestone landform in southern Hunan, China. The new species is similar to <i>C. macrophylla</i>, but differs from the latter in having more prominent tubers, shorter plant height (10–25 cm vs. 30–95 cm), fewer cauline leaves (3–4 vs. 3–18), crenate leaf margin (vs. serrate), fewer flowers (4–10 vs. 10–30), an earlier flowering period (late February to mid-March vs. April to June) and a shorter growth cycle (ca. 4 months vs. ca. 8 months). Following the IUCN Red List Criteria, <i>C. mangshanensis</i> is assess

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Liu, Ang, Jian-jun Zhou, Lei Wu, and Xun-lin Yu. "Carex yankouensis, a new species of Cyperaceae from limestone landform in northern Guangdong, China." PhytoKeys 254 (March 24, 2025): 77–85. https://doi.org/10.3897/phytokeys.254.140929.

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<i>Carex yankouensis</i>, a new species of Cyperaceae (Carex section Rhomboidales) from the limestone landform in northern Guangdong, China is described and illustrated. The new species is similar to <i>C. brevicuspis</i> C. B. Clarke, but differs in having shorter culms (10–15 cm vs 20–55 cm) and spikes (1–1.5 cm vs 3.7–7 cm), leaves wider (15–20–35 mm vs 5–10 mm) and lighter colored (pale green or yellow-green vs dark green), nutlet beak oblique (vs erect or slightly curved), and slightly thickened (vs thickened) style base. Following the IUCN Red List Criteria (IUCN 2024), <i>Carex yankouen

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Roselini, Sabrina, Dian Adhetya Arif, and Sri Kandi Putri. "Mapping of Limestone Potential Using Landsat 8 Satellite Imageryin Some Areasof Timpeh." International Remote Sensing Applied Journal 3, no. 2 (2023): 55–62. http://dx.doi.org/10.24036/irsaj.v3i2.36.

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Limestone potential is important information that can be obtained from remote sensing data which has advantages and speed in processing results. Remote sensing is a technology that can overcome the problemof measuring data for fast and accurate information. This research was carried out in some areas of the Timpeh sub-district,andDharmasraya districtusing Landsat 8-OLI imagery with the aimof1) identifying the potential of limestone using the Band Ratio method. 2) How to apply remote sensing in mapping the potential of limestoneusing Landsat 8 Oli imagery. This research was carried out in

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Books on the topic "Limestone landform"

1

Dept.of Environment. Landform Replication as a Technique for Reclamation of Limestone Quarries. Stationery Office Books, 1992.

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Phát triển bền vững các vùng đá vôi ở Việt Nam. Viện nghiên cứu địa chất và khoáng sản, 2005.

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Book chapters on the topic "Limestone landform"

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Mylroie, John E., and Joan R. Mylroie. "Telogenetic Limestones and Island Karst." In Coastal Karst Landforms. Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-5016-6_17.

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Plašienka, Dušan, and Ján Novotný. "Limestone Klippen Belt—Atypical Landforms in Flysch Uplands." In World Geomorphological Landscapes. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-89293-7_10.

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Pánek, Tomáš, Jan Miklín, and Karel Kirchner. "Limestone Klippen of the Pavlov Hills." In Landscapes and Landforms of the Czech Republic. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-27537-6_29.

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Sammut, Sephora, Ritienne Gauci, Robert Inkpen, Jessica Jade Lewis, and Andy Gibson. "Selmun: A Coastal Limestone Landscape Enriched by Scenic Landforms, Conservation Status and Religious Significance." In World Geomorphological Landscapes. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-15456-1_26.

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5

Hughes, Philip, and Jamie Woodward. "Glacial and Periglacial Environments." In The Physical Geography of the Mediterranean. Oxford University Press, 2009. http://dx.doi.org/10.1093/oso/9780199268030.003.0024.

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Traditionally, glacial and periglacial geomorphology has not featured prominently in discussions about the physical geography of the Mediterranean basin. It is now clear, however, that on numerous occasions during the Pleistocene, and to a lesser extent during the Little Ice Age (LIA), glacial and periglacial activity was widespread in many of the region’s mountain ranges (Hughes et al. 2006a; Hughes and Woodward 2008). Even today, small glaciers and active periglacial features can be found on the highest peaks. Many mountain landscapes in the Mediterranean basin are therefore the product of g

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Migon, Piotr. "Granite Weathering." In Granite Landscapes of the World. Oxford University Press, 2006. http://dx.doi.org/10.1093/oso/9780199273683.003.0010.

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Weathering is a necessary precursor for landform development. However, in the context of granite it acquires a particular importance for various reasons. First, many granite terrains show an extensive development of deep weathering profiles, which can be extremely varied in terms of their depth, vertical zonation, degree of rock decomposition, and mineralogical and chemical change. Moreover, the transitional zone between the weathering mantle and the solid rock, for which the term ‘weathering front’ is used (Mabbutt, 1961b), may be very thin. There is now sufficient evidence that many geomorph

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Gillieson, David. "Karst in Southeast Asia." In The Physical Geography of Southeast Asia. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780199248025.003.0021.

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Flying over the patchwork quilt of land uses that comprise Southeast Asia, one often sees extensive tracts of rugged topography with plateaux pitted with depressions, deep gorges, rivers arising at the bases of mountains, and towers arising from alluviated plains. These are the karst lands, formed on limestone bedrock and subject to the solutional erosion of that bedrock above and below ground. With a total area of about 400 000 km2, Southeast Asia contains some of the more extensive karst regions in the world. Many of these karst areas are of high relief with spectacular arrays of tower and c

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Migon, Piotr. "Slope Development in Granite Terrains." In Granite Landscapes of the World. Oxford University Press, 2006. http://dx.doi.org/10.1093/oso/9780199273683.003.0013.

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Rock slopes developed in granite may take different forms, as reflected in their longitudinal profiles. Field observations and a literature survey (e.g. Dumanowski, 1964; Young, 1972) allow us to distinguish at least five major categories of slopes: straight, convex-upward, concave, stepped, and vertical rock walls. In addition, overhang slopes may occur, but their height is seldom more than 10 m high and their occurrence is very localized. These basic categories may combine to form compound slopes, for example convex-upward in the upper part and vertical towards the footslope. Somewhat differ

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Conference papers on the topic "Limestone landform"

1

Waravita, C. S., A. U. Madhuranga, M. A. J. Rodrigo, S. P. Chaminda, C. L. Jayawardena, and K. G. A. U. Samarakoon. "Geomatics for Monitoring Rehabilitation Status in Aruwakkalu Limestone Quarry, Sri Lanka." In International Symposium on Earth Resources Management & Environment - ISERME 2023. Department of Earth Resources Engineering, 2023. http://dx.doi.org/10.31705/iserme.2023.5.

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Aruwakkalu limestone quarry in Sri Lanka, owned and operated by Siam City Cement (Lanka) Limited, is one of the largest limestone deposits in Sri Lanka. Since the limestone deposit is seated in a shallow depth, it is being excavated by utilising opencast mining methods. The target main product from the extracted limestone is to produce cement. As the first step of ehabilitation, the land restoration is carried out by backfilling the mined-out areas with the previously stripped overburden material. To achieve the final landform, replantation of vegetation cover is formed by planting native tree

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2

BOBOC, Nicolae. "The karst and pseudokarst landforms in the eastern region of the Moldavian Plateau." In "Mediul şi dezvoltarea durabilă", conferinţă ştiinţifică naţională cu participare internaţională. Ion Creangă Pedagogical State University, 2024. https://doi.org/10.46727/cg.17-18-05-2024.p43-53.

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In the geological composition of the upper part of the terrestrial crust of the Moldavian Plateau, limestones, marls, and Meotian gypsums, a category of the soluble rocks, are widely present in the NW. More considerable thickness of 150 -180 m of limestone is visible today in the eastern and NE regions of the plateau. In relation to the geological structure, we distinguish carbonate karst and sulfate karst. The deep carbonate karst formations are represented by caves (Rudi Cave, Surprizelor Cave) and multiple grottoes and smaller caves, sinkholes, gorge, quays in the river valleys of the Toltr

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3

Ponta, Gheorghe, Bashir Memon, James LaMoreaux, Jade Julawong, and Somchai Wongsawat. "Karst Landforms in the Saraburi Group Limestones, Thailand." In National Cave and Karst Research Institute Symposium 2. National Cave and Karst Research Institute, 2013. http://dx.doi.org/10.5038/9780979542275.1140.

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4

Milošević, Marko, Jelena Ćalić, Milovan Milivojević, and Dragan Nešić. "Dolines on Suva planina Mt." In Zbornik radova – VI Kongres geografa Srbije sa medunarodnim ucešcem. University of Belgrade - Faculty of Geography, Belgrade, 2024. http://dx.doi.org/10.5937/kongef24014m.

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Suva Planina Mt. is a part of the Carpatho-Balkanides of Eastern Serbia. It encompasses the area of 427 km2, striking in NW-SE direction at the length of 43 km. Out of the total area of the mountain, limestones cover about 60%, mostly in the central part. The landform types include paleofluvial, fluvial, slope, as well as surface and underground Karst forms. The largest number of landforms are Karst dolines (1227 mapped), based on the official topographical map at the scale 1:25,000). Morphometric characteristics of doline-covered areas have been determined using the SRTM DEM (90 m resolution)

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Reports on the topic "Limestone landform"

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Paulen, R. C., and I. R. Smith. Surficial geology, Sulphur Bay, western Great Slave Lake, Northwest Territories, NTS 85-G. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330073.

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The Sulphur Bay map sheet is a low-relief terrain underlain by lower- to middle-Devonian dolostone and limestone. A thin (&amp;lt;4 m thick) Laurentide Ice Sheet-derived glacial sediment cover drapes most of the landscape, except for bedrock outcrops exposed near Great Slave Lake. Relict glacial landforms record an older northwest ice flow across the region. These are strongly overprinted by subsequent west-southwest-oriented flutings and mega-scale glacial lineations formed during deglaciation. As ice retreated, the entire map area became inundated by glacial Lake McConnell and then subse

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