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Journal articles on the topic 'Tectonic geomorphology'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

Brocklehurst, Simon H. "Tectonics and geomorphology." Progress in Physical Geography: Earth and Environment 34, no. 3 (2010): 357–83. http://dx.doi.org/10.1177/0309133309360632.

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The field of tectonic geomorphology is in a state of tension. The widespread availability of high-quality, high-resolution digital topographic data encourages the development of simple morphological ‘tools’ which can be used to deduce recent tectonic evolution. Meanwhile, process geomorphologists recognize that current models have a significant empirical basis, and lack insight into the underlying physics of erosion processes. Most tectonic geomorphology research is concerned with rivers, but glaciers, debris flows and hillslope processes also play a key role in hypotheses linking climate to t

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2

Bull, William B., and Robert E. Wallace. "Tectonic geomorphology." Geology 13, no. 3 (1985): 216. http://dx.doi.org/10.1130/0091-7613(1985)13<216:tg>2.0.co;2.

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3

Summerfield, M. A. "Tectonic geomorphology." Progress in Physical Geography: Earth and Environment 15, no. 2 (1991): 193–205. http://dx.doi.org/10.1177/030913339101500206.

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4

Voženílek, Vít. "Conceptual remarks for tectonic geomorphology by terrain modelling within GIS." Geografie 111, no. 1 (2006): 3–14. http://dx.doi.org/10.37040/geografie2006111010003.

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The paper deals with term of digital tectonic geomorphology as an integration of structural geology, geomorphology and digital terrain analysis. The author extends traditional set of methods for tectonic geomorphological research and gives general conceptual remarks for methods of tectonic geomorphology developed for the integration of tectonic geomorphology into GIS based on digital terrain modelling. The emphasis is given on selected problems: morphological features associated with fractures, feature recognition and parameter extraction, digital geomorphometry analysis, digital image process

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5

Liu, Zhiheng, Suiping Zhou, Hang Yu, et al. "Quantitative Analysis of Tectonic Geomorphology Research Based on Web of Science from 1981 to 2021." Remote Sensing 14, no. 20 (2022): 5227. http://dx.doi.org/10.3390/rs14205227.

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Tectonic geomorphology is an important research area that uses multisource data to quantify the landscape response induced by the interaction between the tectonic uplift and climate changes. In this study, a comprehensive and quantitative analysis using bibliometric and scientometrics based on the research areas, countries, institutions, journals, authors, keywords, and citations is carried out, which provides an exhaustive history of tectonic geomorphology, and points out the hopspots and trends in the research area. A total of 2796 papers and 110,111 references from 1981 to 2021 are collecte

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6

Rodbell, Donald T. "Book Review: Tectonic geomorphology." Holocene 12, no. 3 (2002): 378–79. http://dx.doi.org/10.1177/095968360201200314.

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7

Burbank, D. W., and R. S. Anderson. "Tectonic Geomorphology, Second Edition." Environmental & Engineering Geoscience 19, no. 2 (2013): 198–200. http://dx.doi.org/10.2113/gseegeosci.19.2.198.

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8

Summerfield, M. A. "Tectonic geomorphology: macroscale perspectives." Progress in Physical Geography: Earth and Environment 10, no. 2 (1986): 227–38. http://dx.doi.org/10.1177/030913338601000205.

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9

Quigley, Mark C., Dan Clark, and Mike Sandiford. "Tectonic geomorphology of Australia." Geological Society, London, Special Publications 346, no. 1 (2010): 243–65. http://dx.doi.org/10.1144/sp346.13.

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10

Faturrakhman, Muhammad Luthfi, Indra Sanjaya, Jamal Jamal, Dian Hari Saputro, and Rully Setiawan. "Tectonic Geomorphology Analysis in Natural Hydrogen Exploration: A Case Study from Tanjung Api, Sulawesi." Riset Geologi dan Pertambangan 35, no. 1 (2025): 37. https://doi.org/10.55981/2025.1357.

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Natural hydrogen exploration has been proven to be a challenging endeavor due to many factors. In this paper we present a new insight to hydrogen exploration by using tectonic geomorphology to identify key target area based on its tectonic activity in relation to the occurrence of active fault. Tectonic geomorphology analysis is performed using 3 morphometric indices such as mountain front sinuosity, basin shape index and drainage density to determine the index of relative tectonic activity in this region. Field observation shows that hydrogen seeps occurred in the area with high to very high

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Faturrakhman, Muhammad Luthfi, Indra Sanjaya, Jamal Jamal, Dian Hari Saputro, and Rully Setiawan. "Tectonic Geomorphology Analysis in Natural Hydrogen Exploration: A Case Study from Tanjung Api, Sulawesi." Riset Geologi dan Pertambangan 35, no. 1 (2025): 37. https://doi.org/10.55981/risetgeotam.2025.1357.

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Natural hydrogen exploration has been proven to be a challenging endeavor due to many factors. In this paper we present a new insight to hydrogen exploration by using tectonic geomorphology to identify key target area based on its tectonic activity in relation to the occurrence of active fault. Tectonic geomorphology analysis is performed using 3 morphometric indices such as mountain front sinuosity, basin shape index and drainage density to determine the index of relative tectonic activity in this region. Field observation shows that hydrogen seeps occurred in the area with high to very high

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12

Faturrakhman, Muhammad Luthfi, Indra Sanjaya, Jamal Jamal, Dian Hari Saputro, and Rully Setiawan. "Tectonic Geomorphology Analysis in Natural Hydrogen Exploration: A Case Study from Tanjung Api, Sulawesi." Riset Geologi dan Pertambangan 35, no. 1 (2025): 37. https://doi.org/10.55981/rgp.2025.1357.

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Natural hydrogen exploration has been proven to be a challenging endeavor due to many factors. In this paper we present a new insight to hydrogen exploration by using tectonic geomorphology to identify key target area based on its tectonic activity in relation to the occurrence of active fault. Tectonic geomorphology analysis is performed using 3 morphometric indices such as mountain front sinuosity, basin shape index and drainage density to determine the index of relative tectonic activity in this region. Field observation shows that hydrogen seeps occurred in the area with high to very high

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13

Singh, Vinod K. "Geology, Geomorphology and Tectonics of India: Introduction." Journal of Geoscience, Engineering, Environment, and Technology 4, no. 2-2 (2019): 1. http://dx.doi.org/10.25299/jgeet.2019.4.2-2.2447.

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The earth crustal growth since its formation still need in depth research is the conclusion of the three International Conferences on Precambrian Continental Growth and Tectonism, in 2005, 2009 and 2013, organised at the Institute of Earth Sciences of Bundelkhand University, Jhansi, India and its proceedings have valuable source for advance research published the great ideas and achievements from scientists (Chandra et al. 2007; Singh and Chandra, 2011 and Singh et al., 2015). Therefore, this thematic issue planned for consider of crustal growth and tectonic evolution of Indian shield which in

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Zovoili, E., E. Konstantinidi та I. K. Koukouvelas. "TECTONIC GEOMORPHOLOGY OF ESCARPMENTS: THE CASES OF KOMPOTADES AND ΝΕΑ ANCHIALOS FAULTS". Bulletin of the Geological Society of Greece 36, № 4 (2004): 1716. http://dx.doi.org/10.12681/bgsg.16579.

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Most active processes on the surface imply that tectonics and geomorphology converge in a way that landscape change may be used as a tectonic signal, given that erosion and weathering have been taken into account. We selected two faults, the Kompotades and the Nea Anchialos faults in the Sperchios and South Thessaly rift zones respectively, and we performed a morphometric analysis. This analysis comprises geomorphic indices that have been used successfully in studies of active tectonics, as the mountain front sinuosity index (Smf), stream gradient index (SL) and valley floor width to valley he

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Ghosh, Sandipan, and Soumya Kundu. "Transient Fluvial Response and Topographic Disequilibrium in the Rivers of the Darjeeling Sikkim Himalaya, India: Geospatial Inference on Tectonic Geomorphology." Journal Of The Geological Society Of India 101, no. 4 (2025): 551–64. https://doi.org/10.17491/jgsi/2025/174125.

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ABSTRACT The assessment of regional tectonic deformation on the earth’s surface, tectonically active landscapes, and the geomorphic manifestation of active tectonics through the use of sophisticated geospatial tools, short-term geodetic data, and longer-term geologic data is made possible here by tectonic geomorphology. The central-southern region of the Darjeeling Sikkim Himalaya (DSH), which is known for its transient fluvial landforms and active tectonics, is primarily characterized by the Lesser Himalaya and Quaternary piedmont fans. The complex river systems of the Tista and Jaldhaka drai

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Martono, Hasria, Suryawan Asfar, et al. "Morphotectonic Control of Land Movements at Wundulako Region, Kolaka Regency, Southeast Sulawesi Province, Indonesia." Journal of Geoscience, Engineering, Environment, and Technology 7, no. 2 (2022): 80–86. http://dx.doi.org/10.25299/jgeet.2022.7.2.9235.

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This research is located at Wundulako District, Kolaka Regency, Southeast Sulawesi Province. The purpose of this study are to determine the level of tectonic activity and the effect of tectonic activity on the land movement of the study area. Based on the DEM (Digital Elevation Model) analysis, geomorphology of the study area is dominated by mountains unit that indicate the influence of tectonic activity. Geomorphological aspects were analyzed to determine the tectonic classes in the study area such as watershed and non-watershed analysis. The results showed that, tectonic class of the study a

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17

Hidayat, Edi, Dicky Muslim, Zufialdi Zakaria, Haryadi Permana, and Dimas Aryo Wibowo. "TECTONIC GEOMORPHOLOGY OF THE KARANGSAMBUNG AREA, CENTRAL JAVA, INDONESIA." Rudarsko-geološko-naftni zbornik 36, no. 4 (2021): 85–105. http://dx.doi.org/10.17794/rgn.2021.4.8.

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Karangsambung, located in Central Java, Indonesia has complex geological conditions of the tectonic evolution of Java Island due to the subduction process of the India-Australia plate with the Eurasian plate in the Cretaceous-Paleocene. The tectonic movements in the subduction zone have resulted in diverse geological structures and rock types and impact the morphological shape of the study area. The level of tectonic activity in the study area can be determined using a tectonic geomorphological approach. A digital elevation model and geographic information systems are used for geomorphic data

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18

Whitehouse, Ian E. "Tectonic geomorphology: recent studies of faulting and tectonic landforms." Progress in Physical Geography: Earth and Environment 16, no. 3 (1992): 361–69. http://dx.doi.org/10.1177/030913339201600306.

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19

Ren, Zhikun, Peizhen Zhang, Takashi Oguchi, and Zhongtai He. "Remote Sensing Perspectives on Geomorphology and Tectonic Processes." Remote Sensing 15, no. 9 (2023): 2327. http://dx.doi.org/10.3390/rs15092327.

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The quantity and quality of remote sensing measurements of tectonic deformation have increased dramatically over the past two decades, improving our ability to observe active geomorphological tectonic processes. High-precision and high-resolution topography is the basis for the quantitative study of active geomorphological and tectonic processes. Recently, with the rapid development of computer visual science and the growing application of light detection and ranging (LiDAR), small unmanned aerial vehicles (UAVs) and structure from motion (SfM) photogrammetry have shown great potential in prov

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20

Arian, Mehran, and Hamideh Noroozpour. "Tectonic Geomorphology of Iran’s Salt Structures." Open Journal of Geology 05, no. 02 (2015): 61–72. http://dx.doi.org/10.4236/ojg.2015.52006.

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21

Mohammed, Pshtiwan Ali, and Azzaden Jumha Darweesh. "Evaluation of the activity of the tectonic processes in the channel of the lower Zab river from Delga to Derband of Rania." Journal of University of Raparin 10, no. 2 (2023): 233–58. http://dx.doi.org/10.26750/vol(10).no(2).paper10.

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This research is about geomorphology and geometric of the Lower Zab river channel between Delga into to Derband of Rania in Pshdar district, it is by using of some coefficient geomorphology index for river basin with the way of occurring. It can show the tectonic activities in the research area; the purpose of this research is to evaluate the activity of the tectonics in the fourth round of the Lower Zab River Path in the research area, along the foot of the Asos Mountain Range on the right side of the path. The river is from Dalga village to Darband of Rania, and the importance of this resear

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22

Faturrakhman, Muhammad Luthfi, Dian Novita, Akbar Cita, Rohman, and Inge Triguri. "Tectonic Geomorphology of Ultramafic Complex in Asera, North Konawe Regency." Jurnal Geologi dan Sumberdaya Mineral 25, no. 3 (2024): 161–68. http://dx.doi.org/10.33332/jgsm.geologi.v25i3.853.

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Ultramafic complex in Sulawesi have many potential from mining to environmental aspects. The process of weathering and tectonic is a key factor in understanding how to utilize these potential. Tectonic geomorphology by using morphometric indices and field observation has proven to be a beneficial method in distinguishing the topography and morphogenetic development of a region due to the complex interaction between erosional processes and tectonic movements. IAT measurement of 71 sub-basins shows that tectonic activity in the research area are divided into 4 classes with values ranging from 1,

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23

Panjaitan, Yohanes Anugrah, and Endang Wiwik Dyah Hastuti. "Analisa Morfotektonik Daerah Bayunglencir dan Sekitarnya, Kabupaten Musi Bayuasin, Sumatera Selatan." Journal of Geology Sriwijaya 1, no. 1 (2023): 34–41. https://doi.org/10.5281/zenodo.8240434.

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<em>Geomorphology is the appearance of landscapes and developments that occur due to the influence of tectonic </em><em>activities. Morphotectonics is a branch of geomorphology that deals with tectonic activity. Morphotectonic analysis uses calculation variables and drainage basin</em><em> </em><em>analysis is carried out through geospatial information systems. This research aims to determine the level of tectonic activity in the Bayunglencir area and its surroundings. The parameters used in this research consisted of four parameters, namely the width of the valley floor to the ratio of the va

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24

Frohlich, Cliff. "Exercise in Active Tectonics: An Introduction to Earthquakes and Tectonic Geomorphology." Eos, Transactions American Geophysical Union 77, no. 33 (1996): 323. http://dx.doi.org/10.1029/96eo00224.

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Green, D. J. "Exercises in Active Tectonics An Introduction to Earthquakes and Tectonic Geomorphology." Environmental & Engineering Geoscience III, no. 3 (1997): 462–63. http://dx.doi.org/10.2113/gseegeosci.iii.3.462.

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26

Ramírez-Herrera, M. T., M. A. Summerfield, and M. A. Ortiz-Pérez. "Tectonic geomorphology of the Acambay graben, Mexican Volcanic Belt." Zeitschrift für Geomorphologie 38, no. 2 (1994): 151–68. http://dx.doi.org/10.1127/zfg/38/1994/151.

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Raj, Rachna, D. M. Maurya, and L. S. Chamyal. "Tectonic Geomorphology of the Mahi River Basin, Western India." Journal Geological Society of India 54, no. 4 (1999): 387–98. http://dx.doi.org/10.17491/jgsi/1999/540406.

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Abstract Neotectonic activity along pre-Quaternary tectonic trends has played a major role in the evolution of Mahi drainage basin. The Mahi basin is controlled by NE-SW and WNW-ESE Aravalli trend in the uplands and by NNW-SSE Tertiary basement faults in the distal part. Lineament analysis shows three structural trends in the area which are related to major regional tectonic trends. Stream orientations indicate that the NNE-SSW and NNW-SSE trends represent lineaments which were active during the youngest tectonic phase. The NE-SW and WNW-ESE trends are slightly older. The evolution of overall

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Verrios, S., V. Zygouri, and S. Kokkalas. "MORPHOTECTONIC ANALYSIS IN THE ELIKI FAULT ZONE (GULF OF CORINTH, GREECE)." Bulletin of the Geological Society of Greece 36, no. 4 (2004): 1706. http://dx.doi.org/10.12681/bgsg.16578.

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Morphotectonic analysis using geomorphic indices has been developed as a basic reconnaissance tool in order to identify areas experiencing rapid tectonic deformation or estimate relative variations of tectonic activity in a specific area. We applied this analysis in Eliki fault zone, which is located in the western part of the Gulf of Corinth. Eliki fault zone was selected because it displays a spectacular geomorphic expression and hosts historic and recent seismicity. The intensity of active tectonics is interpreted through a detailed geomorphic study of the fault-generated mountain fronts an

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Mosavi, Elahe Javadi, and Mehran Arian. "Tectonic Geomorphology of Atrak River, NE Iran." Open Journal of Geology 05, no. 03 (2015): 106–14. http://dx.doi.org/10.4236/ojg.2015.53010.

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Lemenkova, Polina. "Seafloor Mapping of the Atlantic Ocean by GMT: Visualizing Mid-Atlantic Ridge Spreading, Sediment Distribution and Tectonic Development." Acta Geobalcanica 6, no. 3 (2020): 145–57. https://doi.org/10.18509/AGB.2020.16.

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The study presents the insights of the tectonic development and geological settings of the Atlantic Ocean supported by cartographic visualization in Generic Mapping Tools (GMT). The aim is to study geologic situation and trends in the tectonic development of the Mid-Atlantic Ridge and Atlantic Ocean seafloor. The objective is to find out impact of various factors (such as volcanic, tectonic, hydrothermal and sedimentary processes) that sculpt seafloor geomorphology, and correlation between early history of crust formation, geological processes and present submarine landforms. Other assignments

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31

Brzák, Martin. "Contribution to the geomorphology of the southernmost part of the Třebíč Massif." Geografie 105, no. 4 (2000): 347–60. http://dx.doi.org/10.37040/geografie2000105040347.

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Geological maps, with the exception of the newest ones, present this part of the Třebíč Massif in the studied area incorrectly as a part of the Moldanubicum. Conspicuous Neogene tectonic forms (e. g. fault-line valleys, fault-angle valleys) were discovered in the SE marginal part of the massif. Relations between the Tertiary and the older (mainly Variscan) tectonics were studied. Regularity of spatial distribution of the most frequent durbachite forms, as low exfoliation domes, was founded.

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Adams, John, and John J. Clague. "Neotectonics and large-scale geomorphology of Canada." Progress in Physical Geography: Earth and Environment 17, no. 2 (1993): 248–64. http://dx.doi.org/10.1177/030913339301700209.

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Canada includes active convergent and strike-slip plate boundaries, several major mountain systems, two passive continental margins, and a stable craton. Neotectonic activity, as indicated by earthquake occurrence, is highest along the west coast and lowest in the interior of the country. Correlations between tectonics and physiography are strongest in the west. Here, the landscape bears a strong imprint of convergent and strike-slip plate regimes. Late Mesozoic and early Cenozoic tectonic events established the setting in which the present physiography of western Canada developed, but the lan

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Lemenkova, Polina. "STATISTICAL ANALYSIS OF THE MARIANA TRENCH GEOMORPHOLOGY USING R PROGRAMMING LANGUAGE." Geodesy and cartography 45, no. 2 (2019): 57–84. http://dx.doi.org/10.3846/gac.2019.3785.

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This paper introduces an application of R programming language for geostatistical data processing with a case study of the Mariana Trench, Pacific Ocean. The formation of the Mariana Trench, the deepest among all hadal oceanic depth trenches, is caused by complex and diverse geomorphic factors affecting its development. Mariana Trench crosses four tectonic plates: Mariana, Caroline, Pacific and Philippine. The impact of the geographic location and geological factors on its geomorphology has been studied by methods of statistical analysis and data visualization using R libraries. The methodolog

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Lemenkova, Polina. "Statistical Analysis of the Mariana Trench Geomorphology Using R Programming Language." Geodesy and Cartography 45, no. 2 (2019): 57–84. https://doi.org/10.3846/gac.2019.3785.

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This paper introduces an application of R programming language for geostatistical data processing with a case study of the Mariana Trench, Pacific Ocean. The formation of the Mariana Trench, the deepest among all hadal oceanic depth trenches, is caused by complex and diverse geomorphic factors affecting its development. Mariana Trench crosses four tectonic plates: Mariana, Caroline, Pacific and Philippine. The impact of the geographic location and geological factors on its geomorphology has been studied by methods of statistical analysis and data visualization using R libraries. The methodolog

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35

Lemenkova, Polina. "Cartographic Processing of the Multi-Source Geospatial Datasets by GMT for Mapping Variability in Geologic Setting and Bathymetry of the Pacific Ocean." Mercator 20 (April 21, 2021): 1–18. https://doi.org/10.5281/zenodo.4706741.

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The paper presents spatial analysis of the geological settings and topographic structure of the Pacific Ocean by Generic Mapping Tools (GMT). Its tectonic and geomorphic features have complex character and include, among others, trenches, ridges, East Pacific Rise, basins, fracture zones, rifts, rises, fault systems. Such topographic complexity results in the variability of the seafloor fabric and sedimentation reflecting correlations between the tectonic geomorphic markers and bathymetry. The methodology of this paper is based on the advanced cartographic toolset GMT which utilizes a shell sc

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WHITEHOUSE, IAN E. "Geomorphology of the Himalaya: A Climato-Tectonic Framework." New Zealand Geographer 46, no. 2 (1990): 75–85. http://dx.doi.org/10.1111/j.1745-7939.1990.tb01961.x.

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Jadhav, Pradeep B., and K. Kshirsagar Lalitkumar. "Tectonic geomorphology in parts of Koyna region, Maharashtra." Journal of the Geological Society of India 90, no. 6 (2017): 738–41. http://dx.doi.org/10.1007/s12594-017-0784-7.

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Uchupi, Elazar, S. A. Swift, and D. A. Ross. "Tectonic geomorphology of the Gulf of Oman Basin." Geological Society, London, Special Publications 195, no. 1 (2002): 37–69. http://dx.doi.org/10.1144/gsl.sp.2002.195.01.04.

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Fahira, Ghina, Emi Sukiyah, and Dicky Muslim. "Quantitative Geomorphology Approach in the Assessment of Relative Tectonic Activity in Cikandang Watershed, South West Java." GEOID 20, no. 1 (2025): 22–35. https://doi.org/10.12962/geoid.v20i1.2619.

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Cikandang Watershed in Cisewu Block, South West Java, is an area with significant tectonic activity that is reflected in geomorphological characteristics. This study aims to evaluate the relative tectonic activity in the Cikandang watershed using a quantitative geomorphological approach. Research methods involved six morphotectonic parameters: Valley Height-Width Ratio (Vf), Mountain Face Sinusity (Smf), Basin Shape Index (Bs), Asymmetry Factor (Af), Integral Hypsometry (Hi), and River Length Gradient Index (SL). These parameters were analysed to determine the Index of Relative Tectonic Activi

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Saadouni, Hania, and Rabah Alouani. "Uplift Quantification and Erosion Rate Estimation in Northwestern Tunisia from Topographic and Lithologic Data." Environment and Pollution 10, no. 1 (2021): 15. http://dx.doi.org/10.5539/ep.v10n1p15.

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Digital elevation modeling (DEM) was used to determine key morphological features such as hypsometry, slopes and topographic evolution in correlation with tectonic regimes and erosion mechanisms. This contribution discusses the tectonic model of northern Tunisia, which since 1977 has been described by geologists as an allochthonous unity domain of the Serravallian-Tortonian. This study presents new data from the erosion rate calculation following the establishment of these units and then proposes another view on regional tectonics. Therefore, the example used of Oued Sedjnene gives a rising ra

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Dollar, Evan S. J. "Palaeofluvial geomorphology in southern Africa: a review." Progress in Physical Geography: Earth and Environment 22, no. 3 (1998): 325–49. http://dx.doi.org/10.1177/030913339802200302.

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This article presents an overview of palaeofluvial geomorphology research in southern Africa. For the purposes of this article this includes South Africa, Zimbabwe, Namibia, Lesotho, Swaziland and Botswana. Although interest in fluvial systems has a long history in southern Africa, the scientific study of rivers was initiated by the discovery of the first alluvial diamond along the banks of the Orange River in 1867. Since then, significant progress has been made in unravelling the fluvial history of southern Africa from the early Archaean Ventersdorp Contact Reef River to modern channel proces

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Pena-Castellnou, S., V. Steinritz, G. I. Marliyani, and K. Reicherter. "Active tectonics of the Yogyakarta area (Central Java, Indonesia): preliminary findings obtained from a tectonic-geomorphic evaluation." IOP Conference Series: Earth and Environmental Science 851, no. 1 (2021): 012005. http://dx.doi.org/10.1088/1755-1315/851/1/012005.

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Abstract Throughout the island of Java, several shallow faults located in the vicinity of densely populated areas accommodate the tectonic strain generated by the subduction of the Indo-Australian Plate beneath the Sunda Plate. These faults are characterized by a poor surface geomorphological expression due to the tropical climate that masks paleoseismological evidence making the identification of active faults in this environment challenging. We present preliminary data of a tectonic-geomorphic study that aims to identify and characterize active faults in the province of Yogyakarta (Central J

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Miccadei, Enrico, Cristiano Carabella, and Giorgio Paglia. "Morphoneotectonics of the Abruzzo Periadriatic Area (Central Italy): Morphometric Analysis and Morphological Evidence of Tectonics Features." Geosciences 11, no. 9 (2021): 397. http://dx.doi.org/10.3390/geosciences11090397.

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Drainage basin-scale morphometric analysis and morphological evidence of tectonics represent helpful tools to evaluate and investigate morphoneotectonic processes in tectonically active regions. In this perspective, we applied an integrated analysis to the Abruzzo Periadriatic Area, between the Tronto and Sinello rivers (Central Italy). It involved morphometric analysis, structural geomorphological field mapping, and detailed analysis of fluvial terraces. Geomorphic indexes and markers (e.g., Irta, SL index, ksn, and knickpoints) were used in this study to detect the response of landscapes to

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Obiegbu, Okechukwu Livinus, Andreas Laake, and Peter Brabham. "An estimation of regional geologic structures from the geomorphology to characterize the Wadi systems, southeast Sinai, Egypt." Interpretation 4, no. 3 (2016): T323—T336. http://dx.doi.org/10.1190/int-2015-0125.1.

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Complex regional geologic structural controls have generated a lot of interest in the engineering, oil, and gas industries within the past few years. Digital elevation models (DEMs), multispectral remote sensing images using ArcGIS software, in combination with data cube and geomorphologic characterization, provide important markers that aid in spatial information analysis for the study area. We have validated the characterization and classification of DEMs using spatial statistics by mineral spectroscopy of multispectral remote sensing data. Our characterization was initiated by a joint inter

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Goto, Hideaki, Kohsaku Arai, and Taichi Sato. "Topographic Anaglyphs from Detailed Digital Elevation Models Covering Inland and Seafloor for the Tectonic Geomorphology Studies in and around Yoron Island, Ryukyu Arc, Japan." Geosciences 8, no. 10 (2018): 363. http://dx.doi.org/10.3390/geosciences8100363.

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Anaglyphs produced using a digital elevation model (DEM) are effective to identify the characteristic tectono–geomorphic features. The objective of this study is to reinvestigate the tectonic geomorphology and to present novel tectonic maps of the late Quaternary in and around the Yoron island based on the interpretation of extensive topographical anaglyphs along the map areas that cover the inland and seafloor. Vintage aerial photographs are used to produce the 3-m mesh inland digital surface model (DSM); further, the 0.6-s to 2-s-mesh seafloor DEM is processed using the cloud point data gene

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Law, Robert, and Mark B. Allen. "Diachronous Tibetan Plateau landscape evolution derived from lava field geomorphology." Geology 48, no. 3 (2020): 263–67. http://dx.doi.org/10.1130/g47196.1.

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Abstract Evolution of the Tibetan Plateau is important for understanding continental tectonics because of the plateau’s exceptional elevation (∼5 km above sea level) and crustal thickness (∼70 km). Patterns of long-term landscape evolution can constrain tectonic processes, but have been hard to quantify, in contrast to established data sets for strain, exhumation, and paleo-elevation. This study analyzes the relief of the bases and tops of 17 Cenozoic lava fields on the central and northern Tibetan Plateau. Analyzed fields have typical lateral dimensions of tens of kilometers, and so have an a

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Lemenkova, Polina. "The geomorphology of the Makran Trench in the context of the geological and geophysical settings of the Arabian Sea." Geology, Geophysics and Environment 46, no. 3 (2020): 205–22. https://doi.org/10.7494/geol.2020.46.3.205.

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The study focuses on the Makran Trench in the Arabian Sea basin, in the north Indian Ocean. The area is tectonically active, with a system of ridges and fracture zones morphologically separating the Arabian Sea. The study examined the relationships between the topographic structure of the Makran Trench and the re- gional settings of the Arabian Sea: geomorphology, sediment thickness, geophysical fields, geology and tectonic lineaments. The methodology is based on the GMT scripting toolset. The spatial analysis includes high-resolu- tion datasets GEBCO, EGM2008, GlobSed and data on tectonics, g

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Hikmy, Isbram Ginanjar, Alfend Rudyawan, Berta Syafira Putri, Benyamin Sapiie, and Indra Gunawan. "The uplift rate of Sulawesi East Arm and the activity of Batui Fault using a tectonic geomorphology approach in the Luwuk Area, Sulawesi." Jurnal Geologi dan Sumberdaya Mineral 26, no. 1 (2025): 1–15. https://doi.org/10.33332/jgsm.geologi.v26i1.663.

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Sulawesi is a tectonically active area with convergent triple-junction amidst Eurasian, Indo-Australian and Pacific Plate. The study area is located in the suture zone of sedimentary Banggai-Sula Microcontinent and East Sulawesi Ophiolite. This research is aimed to determine fault activity and rate of tectonic uplift of Luwuk mountainous area. Field geological mapping had been done to determine lithology and geological structure along with morphometric analysis to measure definitive result of tectonic activities. Geological structure features which encountered in this area are Batui Thrust, Pa

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Arroyo-Solórzano, Mario, and Adolfo Quesada-Román. "Unidades morfotectónicas de Costa Rica: caracterización y potencial para el ordenamiento ambiental." Revista Geográfica de América Central. 2, no. 75 (2025): 183–223. https://doi.org/10.15359/rgac.75-2.7.

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The tectonic and geomorphological dynamics of Costa Rica result from the interaction of four tectonic plates in a subduction zone, combined with tropical erosive processes. In this study, we extensively review the classifications and boundaries between morphotectonic units in Costa Rica. We propose an initial subdivision based on tectonic-structural elements and morphotectonic regions, whereby we establish thirteen main morphotectonic units that encompass similar relief and geomorphological characteristics. Finally, we analyze and related this classification with climatic factors, vegetation,

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OTA, Yoko. "Recent Studies on the Tectonic Geomorphology of New Zealand." Geographical Review of Japa,. Ser. A, Chirigaku Hyoron 62, no. 9 (1989): 636–66. http://dx.doi.org/10.4157/grj1984a.62.9_636.

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