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Zeitschriftenartikel zum Thema „Polje (Geomorphology)“

Autor: Grafiati

Veröffentlicht am 4. Juni 2021

Zuletzt aktualisiert am 29. Juli 2025

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1

Phu, Huynh, Le Canh Tuan, Nguyen Ly Ngoc Thao, Huynh Thi Ngoc Han, and Cao Minh Thuy. "Characteristic of Lang Son Karst Poljes in Vietnam and Geohazards." Iraqi Geological Journal 55, no. 2B (2022): 170–82. http://dx.doi.org/10.46717/igj.55.2b.15ms-2022-08-31.

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In the karst regions of Vietnam, there are many different terrains. The most important one is karst polje. Because there are a lot of residential areas and important economic regions. Based on the study of Geomorphology, geological structure analysis, Geophysics document analysis, and karstification process research at Lang Son karst polje. The author gives conclusions: Lang Son karst polje was formed from the limestone of Bac Son Formation, 700 – 800 m thick. Lang Son karst polje was formed from anticline structure, the limestone of Bac Son Formation that has high karstification level. Lang S

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2

DOĞAN, Uğur, Serdar YEŞİLYURT, Gönül MUTLU, and Ali KOÇYİĞİT. "Base-level poljes in the Sivas gypsum karst, Türkiye." Jeomorfolojik Araştırmalar Dergisi, no. 9 (November 15, 2022): 19–37. http://dx.doi.org/10.46453/jader.1125343.

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The Sivas Basin, Central Anatolia, includes one of the most outstanding gypsum karst terrains in the world, covering an area of 2140 km2. The karst landscapes are developed on late Eocene gypsum deposits. The fact that the polje shapes that are commonly seen in the limestone karst terrain also seen in the Sivas gypsum karst area further increases the importance of this area in terms of geomorphology. This study is focused on the explanation of the morphometric properties and formation mechanism of poljes around the Kızılırmak River in the Sivas gypsum karst area. The geomorphological evolution

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3

Kranjc, Andrej, and Christophe Gauchon. "Balthasar Hacquet, pionnier de la karstologie." Karstologia : revue de karstologie et de spéléologie physique 61, no. 1 (2013): 45–52. https://doi.org/10.3406/karst.2013.2740.

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Balthasar Hacquet (1739/40-1815), the Pioneer of Karst Geomorphologists. Besides other sciences, B. Hacquet dedicated his research to geology and geomorphology fas we call them now). His most important work "Oryctographia Carniolica or Physical (= geological) description of Carniola..." (1778-1789) contains descriptions of rocks, ores, fossils, as well as surface and underground features. In Carniola (i.e. Slovenia), karst is prevailing and therefore there is a lengthy description of karst geology and geomorphology included. His classification of mountains specially mentions Montes secundarii

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4

Goy, José Luis, Jose Luis Corvea, Irene de Bustamante, et al. "Geomorphological Heritage in Viñales National Park (Aspiring UNESCO Geopark): Geomatic Tools Applied to Geotourism in Pinar del Río, Cuba." Sustainability 15, no. 7 (2023): 5704. http://dx.doi.org/10.3390/su15075704.

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A detailed analysis of the Viñales National Park (VNP) was carried out to evaluate the main geosites of geomorphological interest inside the park. This allowed the selection of areas (AIG) and localities (LIG) with 20 geosites of geological interest (PIG) suitable to evaluate their importance as geoheritage. Moreover, three field trips and one virtual itinerary encompassing the park aimed to improve the geological–geomorphological knowledge to be used in geotouristic and preservation issues. The methodology included preparing five maps: relief, drainage pattern, slopes, lithology and geomorpho

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Paxman, Guy J. G., Stewart S. R. Jamieson, Fausto Ferraccioli, et al. "Subglacial Geology and Geomorphology of the Pensacola‐Pole Basin, East Antarctica." Geochemistry, Geophysics, Geosystems 20, no. 6 (2019): 2786–807. http://dx.doi.org/10.1029/2018gc008126.

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6

Zelnik, Igor, Urška Kuhar, Matej Holcar, Mateja Germ, and Alenka Gaberščik. "Distribution of Vascular Plant Communities in Slovenian Watercourses." Water 13, no. 8 (2021): 1071. http://dx.doi.org/10.3390/w13081071.

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Rivers and streams are heterogenous ecosystems that host a great number of vascular plant communities. The territory of Slovenia is highly diverse regarding geomorphologic, geologic, climatic, and edaphic conditions. We presumed that environmental variability will also affect the distribution of hygrophilous vascular plants in running waters and consequently the structure of plant communities they form. We analyzed macrophyte, spatial, and environmental parameters in 906 stretches of the watercourses occurring in the Dinaric, Pannonian, and Po lowland hydro-ecoregions. We determined 87 vascula

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7

Tieszen, Larry L., Nel Caine, and R. M. Koerner. "Physiological Ecology of North American Plant Communities, Geomorphology, On Skis to the North Pole." Arctic and Alpine Research 18, no. 3 (1986): 353–55. http://dx.doi.org/10.1080/00040851.1986.12004097.

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8

Radoš, Denis, Sanja Lozić, and Ante Šiljeg. "Morfometrijske značajke šireg područja Duvanjskog polja, Bosna i Hercegovina." Geoadria 2, no. 1 (1997): 177. http://dx.doi.org/10.15291/geoadria.248.

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The objects of this study are the hillslopes in the broader area of Duvanjsko polje (Bosnia and Herzegovina). Slopes can be defined as relief surfaces determined by geographical position, slope inclination (related with horizontal surface), aspect, and degree of curvature (profile and planar).Recent slope shapes can be defined as results of series of natural and anthropogenic factors during relief genesis and evolution. It is possible to correlate slope characteristics with geological structure and other natural geographic features (climate, soils, vegetation etc.) using geomorphometrical anal

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Radoš, Denis, Sanja Lozić, and Ante Šiljeg. "Morfometrijske značajke šireg područja Duvanjskog polja, Bosna i Hercegovina." Geoadria 17, no. 2 (2012): 177. http://dx.doi.org/10.15291/geoadria.352.

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The objects of this study are the hillslopes in the broader area of Duvanjsko polje (Bosnia and Herzegovina). Slopes can be defined as relief surfaces determined by geographical position, slope inclination (related with horizontal surface), aspect, and degree of curvature (profile and planar).Recent slope shapes can be defined as results of series of natural and anthropogenic factors during relief genesis and evolution. It is possible to correlate slope characteristics with geological structure and other natural geographic features (climate, soils, vegetation etc.) using geomorphometrical anal

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10

Dill, Harald G. "An overview of the pegmatitic landscape from the pole to the equator – Applied geomorphology and ore guides." Ore Geology Reviews 91 (December 2017): 795–823. http://dx.doi.org/10.1016/j.oregeorev.2017.08.020.

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11

Wueller, Lukas, Wajiha Iqbal, Thomas Frueh, Carolyn H. van der Bogert, and Harald Hiesinger. "Geologic History of the Amundsen Crater Region Near the Lunar South Pole: Basis for Future Exploration." Planetary Science Journal 5, no. 6 (2024): 147. http://dx.doi.org/10.3847/psj/ad2c04.

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Abstract We provide the first detailed 1:100,000 scale geomorphologic map of the ∼100 km Amundsen crater region, which is of high scientific relevance for future exploration, e.g., NASA’s VIPER mission, the Artemis program, and the Chinese International Lunar Research Station. We investigated the complex geological history of the region before and after the formation of Amundsen crater on the rims of the South Pole–Aitken (SPA) and Amundsen–Ganswindt basins. We present a new Amundsen crater formation age of ∼4.04 Ga, which, in contrast to previously derived ages, is based on non-light-plains t

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Mua, Kang Edwin, and Kometa Sunday Shende. "The Response of Stream Competence to Topographic and Seasonal Variations in The Bamenda-Menchum Drainage Basin, North West Region, Cameroon." Journal of Geography and Geology 11, no. 2 (2019): 21. http://dx.doi.org/10.5539/jgg.v11n2p21.

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The flow direction of streams remains an establishing mechanism in understanding drainage basin function and stream competence. The ability of streams to erode, transport and deposit loads in fluvial geomorphology exert a benchmark precursor for slope dynamics given the differential geological outcrop of the Bamenda-Menchum basin. Such competence in stream network generates slope instability as materials continuously move down slope from the volcanic escarpment face of Bamenda highlands to the sedimentary lowland area of Lower Bafut-Menchum basin. This paper investigate the influence of stream

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13

Zhou, Yinjun, Yu Gao, Qinjing Shen, et al. "Response of Channel Morphology to Climate Change over the Past 2000 Years Using Vertical Boreholes Analysis in Lancang River Headwater in Tibetan Plateau." Water 14, no. 10 (2022): 1593. http://dx.doi.org/10.3390/w14101593.

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The Qinghai-Tibetan Plateau, known as the world’s “third pole”, is home to several large rivers in Asia. Its geomorphology is exceptionally vulnerable to climate change, which has had a significant impact on historical riverbed development through runoff and sedimentation processes. However, there is limited research combining climate change, sedimentology, and chronology with river dynamics to investigate riverbed evolution patterns in geological-historical time scales and their changes in overland flow capacity. In the current study, the evolution of a representative portion of the river cha

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14

Scalera, Giancarlo. "Geodynamics of the Wadati-Benioff zone earthquakes: The 2004 Sumatra earthquake and other great earthquakes." Geofísica Internacional 46, no. 1 (2007): 19–50. http://dx.doi.org/10.22201/igeof.00167169p.2007.46.1.2150.

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   The displacement of the Earth’s instantaneous rotation pole – observed at ASI of Matera, Italy – the seismic data (USGS) in the two days following the main shock, the high frequency P-wave radiation, the geomorphologic data, and the satellite data of uplift/subsidence of the coasts (IGG) converge toward a new interpretation of the Great Sumatran earthquake (TU=26 December 2004 - 00h 58m, Lat=3.3°N, Lon=95.8°E, H=10 km, M=9.3) based on the second conjugate – nearly vertical – CMT fault plane solution. In a non-double-couple treatment that considers non-negligible non-elasti

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15

Tukur, Rahmat S., Olatunji S. Ayanninuola, Etim D. Uko, and Charles O. Ofoegbu. "ANALYSIS OF AEROMAGNETIC ANOMALIES OVER PART OF THE UPPER BENUE TROUGH (SHEET NUMBERS 171,172,192, AND 193), NIGERIA." Journal of Technology & Innovation 4, no. 2 (2024): 54–62. https://doi.org/10.26480/jtin.02.2024.54.62.

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A total of four Aeromagnetic Sheets of 1:100,000 scale comprising of Sheets Yuli-171, Futuk-172, Bashar-192 and Muri-193 which covers part of the Upper Benue trough were subjected to both qualitative and quantitative analysis and interpretation in order to understand the magnetic signature, intrusive magmatic activities, basement structural orientation, basement geomorphology, sedimentary thickness and the relationship between the anomalies to the mineralization potential of the study area. To achieve this, various techniques such as filtering, reduction-to-the-Pole, reduction to the Equator (

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16

Scalera, G. "Great and old earthquakes against great and old paradigms – paradoxes, historical roots, alternative answers." Advances in Geosciences 14 (January 2, 2008): 41–57. http://dx.doi.org/10.5194/adgeo-14-41-2008.

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Abstract. The similarity of the vertical displacements shown by case-history extreme-magnitude earthquakes are scrutinised (Chile 1960, Alaska 1964, Sumatra 2004, ...). A common interpretation – an uprising of lithospheric material – can be found, which is supported by the irregularities of the hypocentres distribution along the Wadati-Benioff zones. In the case of major South American earthquakes, a volcanic eruptions-earthquakes correlation is recognisable. Further support to this interpretation is the displacement of the Earth's instantaneous rotation pole – ≈3.0 mas (≈10 cm), observed at A

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17

Stepišnik, Uroš, Mateja Ferk, Petra Gostinčar, and Luka Černuta. "Holocene high floods on the Planina Polje, Classical Dinaric Karst, Slovenia." Acta Carsologica 41, no. 1 (2012). http://dx.doi.org/10.3986/ac.v41i1.44.

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The Planina Polje is located in the northwestern part of Notranjsko Podolje, Slovenia. Annual floods cover the flattened floor of the polje at elevation 445 m a.s.l. and reach the depth of approximately 8 meters. Loamy sediments which were found on surface and subsurface features from the inflow part of Planina Polje up to the elevations of about 495 m a.s.l., indirectly show that floods in the past must have been much more extensive than the recent ones. Radiocarbon dating of flowstone layer from side passage Tiha Jama in Planina Cave revealed that the last such extreme floods appeared around

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18

Frelih, Martina. "Geomorphology of Karst Depressions: Polje or Uvala - a Case Study of Lučki dol." Acta Carsologica 32, no. 2 (2016). http://dx.doi.org/10.3986/ac.v32i2.341.

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19

Abu-Safat, Mohammed. "Geomorphology and the Possibilities of Resolving Sinking Problem in Marj Sanour." An-Najah University Journal for Research - B (Humanities), January 1992. http://dx.doi.org/10.35552/0247.6.1.492.

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Marj Sanour "al Gharaq" is one of the close karst plain "Polje" which spreads within the West-Bank mountains. The creation of this plain was a result of the cross faults, which took place in contemporary with the Jordan rift valley. The karst process had changed it to a close typical Polje. The geomorphological processes closed the only outlet as a result of the construction of the alluvial fan of Wadi Umm Khurrameyeh and Wadi Sanour, and the differential between the lowest point in the Marj and the highest one of the outlet is 24m. Since its closure, it has become an internal run flow. As a r

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20

Filipović, Ivona Ivkić, Nikolina Ilijanić, Slobodan Miko, et al. "Late Quaternary geomorphology and sedimentary processes in the Prološko Blato karst wetland (Imotsko Polje, Croatia)." Geomorphology, April 2025, 109765. https://doi.org/10.1016/j.geomorph.2025.109765.

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21

Parise, Mario. "Surface and subsurface karst geomorphology in the Murge (Apulia, Southern Italy)." February 5, 2016. https://doi.org/10.3986/ac.v40i1.30.

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The Murge (Apulia, southern Italy) is the main karst area in the central part of the region, extending from the inland plateau to the Adriatic coastline. Along this transect, a relief energy of a few hundred meters is reached. Even thoughsuchrelief may seem small when compared to mountain karst areas, actually it is not for Apulia, a very flat carbonate region that acted as the foreland during the building up of the Apenninic Chain in Miocene time. Murge can be subdivided into two sectors: HighMurge, the inland plateau, where remnants of an ancient tropical karst are still recognizable; and Lo

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22

Meysam, Jamali, Moghimi Ebrahim, and Alabden Jafarpour Zean. "Geomorphology of Karst Features of Shiraz City and Arjan Plain and Development Limitations." January 3, 2015. https://doi.org/10.5281/zenodo.1098952.

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Karst term is the determiner of a variety of areas or landforms and unique perspectives that have been formed in result of the of the ingredients dissolution of rocks constituter by natural waters. Shiraz area with an area of 5322km2 is located in the simple folded belt in the southern part of Zagros Mountain of Fars, and is surrounded with Limestone Mountains (Asmari formation). Shiraz area is located in Calcareous areas. The infrastructure of this city is lime and absorbing wells that the city can influence the Limestone dissolution and those accelerate its rate and increase the cavitation b

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23

Meysam, Jamali, Moghimi Ebrahim, and Alabden Jafarpour Zean. "Geomorphology of Karst Features of Shiraz City and Arjan Plain and Development Limitations." International Journal of Earth, Energy and Environmental Sciences 8.0, no. 1 (2015). https://doi.org/10.5281/zenodo.1338078.

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Karst term is the determiner of a variety of areas or landforms and unique perspectives that have been formed in result of the of the ingredients dissolution of rocks constituter by natural waters. Shiraz area with an area of 5322km2 is located in the simple folded belt in the southern part of Zagros Mountain of Fars, and is surrounded with Limestone Mountains (Asmari formation). Shiraz area is located in Calcareous areas. The infrastructure of this city is lime and absorbing wells that the city can influence the Limestone dissolution and those accelerate its rate and increase the cavitation b

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24

Bertoli, Silvia, Alice Lucchetti, Maurizio Pajola, et al. "Geomorphology of craters located at Mercury’s north pole." Journal of Maps 20, no. 1 (2024). http://dx.doi.org/10.1080/17445647.2024.2349788.

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25

Zeng, Xingguo, Dawei Liu, Yuan Chen, et al. "Landing site of the Chang’e-6 lunar farside sample return mission from the Apollo basin." Nature Astronomy, July 31, 2023. http://dx.doi.org/10.1038/s41550-023-02038-1.

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AbstractTo address questions about the multiple lunar nearside–farside dichotomies and to provide new insights into both the early impact history of the Solar System and the geological evolution of the Moon, the Chang’e-6 (CE-6) landing zone has been selected to lie within the lunar farside South Pole–Aitken (SPA) basin in the southern part of the Apollo basin (150–158° W, 41–45° S), a site that provides access to a diversity of SPA material. Here, we describe the geomorphology, geology and chronology of three candidate sampling sites within this zone that are likely to ensure safe landing and

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26

Kwasnitschka, Tom, Thor H. Hansteen, Ricardo S. Ramalho, et al. "Geomorphology and Age Constraints of Seamounts in the Cabo Verde Archipelago, and Their Relationship to Island Ages and Geodynamic Evolution." Geochemistry, Geophysics, Geosystems 25, no. 3 (2024). http://dx.doi.org/10.1029/2023gc011071.

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AbstractThe Cabo Verde Archipelago is related to a mantle plume located close to the rotational pole of the African Plate. It consists of islands and seamounts arranged in a horseshoe‐shaped pattern open to the west, thus forming two volcanic chains, each with a weak east‐west age progression. High‐resolution swath bathymetry of 12 Cabo Verde seamounts is used here to assign each seamount to its pre‐shield, shield or post‐shield evolutionary stage, respectively. The eastern seamounts exhibit degraded and partially eroded morphologies, and are mainly in their post‐shield stage. A new 40Ar‐39Ar

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27

Gobashy, Mohamed M., Ehdaa Allah Sayed Abbas, Khalid S. Soliman, and Ahmed Abdelhalim. "Mapping of gold mineralization using an integrated interpretation of geological and geophysical data—a case study from West Baranes, South Eastern Desert, Egypt." Arabian Journal of Geosciences 15, no. 22 (2022). http://dx.doi.org/10.1007/s12517-022-10955-0.

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AbstractThe current study is mainly devoted to the integration, analysis, and interpretation of the available geologic, remote sensing, and potential field data (mainly magnetic) to delineate the subsurface geologic structural elements controlling the western part of Baranes, South Eastern Desert, Egypt, and its relation to the southwestern desert structural regime. Additionally, to detect potential mineralization zones for future mining plans in the study area. The Western part of Baranes has not had enough geomorphological mapping, consequently, potential discoveries of mineralization zones

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28

Brighi, Giancorrado. "Cassini Bistatic Radar Experiments: Preliminary Results on Titan’s Polar Regions." Aerotecnica Missili & Spazio, September 10, 2022. http://dx.doi.org/10.1007/s42496-022-00135-4.

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AbstractIn bistatic radar observations, reflected echoes from the surface of a target planet can be analyzed to infer its surface statistics and near-surface constituents. In this work, a preliminary inspection of two X-band bistatic radar observations gathered by the Cassini spacecraft about Titan’s polar regions is presented. Profiles of relative dielectric constant and root-mean-square (rms) surface slope are provided as outputs of the analysis, discussed, and compared with the present knowledge of Titan geomorphology. For the assessment of the rms slope, proportional to the spectral broade

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29

Borch, Annie, James Kelly Russell, and René W. Barendregt. "Cheakamus Basalt Lavas, British Columbia: A Pleistocene record of rapid, continuous eruption within a mountainous drainage system." Canadian Journal of Earth Sciences, June 27, 2023. http://dx.doi.org/10.1139/cjes-2023-0004.

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The Cheakamus basalts are voluminous (1.65 km3) Late Pleistocene, valley-filling lavas erupted from a vent situated near Conflict Lake, in the alpine Callaghan Valley near Whistler, British Columbia. Geochemical and petrographic properties suggest these olivine-plagioclase porphyritic basalts derive from a single magma batch affected by minor sorting of phenocrysts and xenocrystic plagioclase. Thirty-four sites sampled for paleomagnetic direction measurement record a mean pole direction of 345.2 ̊ / 73.0 ̊ (α95 = 1.3°), showing no statistical variation nor drift with stratigraphic position. Th

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Ait Barka, Abdellah, Jamila Rais, Ahmed Barakat, Elhassan Louz, and Samir Nadem. "The Karst Landscapes of Beni Mellal Atlas (Central Morocco): Identification for Promoting Geoconservation and Tourism." Quaestiones Geographicae, August 19, 2022. http://dx.doi.org/10.2478/quageo-2022-0027.

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Abstract The Atlas of Beni Mellal is located in the Moroccan central High Atlas, characterized by an important geo-diversity that attracts tourists every year. However, the number of visitors remains limited due to the lack of the promotion means, enhancement and mediation of this heritage. The obtained data indicate that the studied area preserves a great number of karst geosites, such as ruiniform landscapes, caves, poljes, sinkholes, Karren, shaft cave and many remarkable reliefs such as canyons and cliffs. This work concerns the inventory, the quantitative evaluation and the enhancement of

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Hidayat, Muslich, Djufri Djufri, Hairul Basri, and Nazli Ismail. "Vegetation Diversity in The Hot Spring Areas of Ie Suum and Ie Jue in Seulawah Agam Mountain, Aceh Besar District Aceh Province Indonesia." Elkawnie 9, no. 2 (2023). http://dx.doi.org/10.22373/ekw.v9i2.20087.

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Abstract: The structure and composition of vegetation in hot spring areas of Ie Suum and Ie Jue in Seulawah Agam mountain are influenced by the temperature of hot spring zones. Given that the geology and geomorphology of the hot spring area will undoubtedly influence the structure and composition of the vegetation, it is critical to know the data that comprise the vegetation. This study aims to identify plant species, vegetation habitus, and vegetation diversity index. This research was conducted in the area of hot springs Ie Suum and Ie Jue Seulawah Agam mountain Aceh Besar district Aceh prov

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