Narzędzia help

Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
first last
cannonical link button

http://yadda.icm.edu.pl:80/baztech/element/bwmeta1.element.baztech-article-BUS2-0015-0031

Czasopismo

Przegląd Geologiczny

Tytuł artykułu

Application of digital elevation models to geological and geomorphological studies - some examples

Autorzy Badura, J.  Przybylski, B. 
Treść / Zawartość http://www.pgi.gov.pl/oferta-inst/wydawnictwa/czasopisma/przeglad-geologiczny.html
Warianty tytułu
Języki publikacji EN
Abstrakty
EN Analysis of the Earth’s surface using three-dimensional models provides a wealth of new interpretation opportunities to geologists and geomorphologists. Linear elements, not visible on classical maps, become distinct features; it is also possible to interpret both small-scale glacial landforms and entire complexes of postglacial landscapes at the regional scale. Geomorphic features are frequently difficult to recognise in the field, either due to their scale or field obstacles. Three-dimensional visualization of the Earth’s surface and its examination at different angles and differently orientated source of light is extremely helpful in geological and geomorphological studies. This tool is, however, relatively seldom used due to either limited access to digital data bases or time-consuming procedures of individual construction of such bases from the existing cartographic data. For instance, analysis of small-scale glacial, fluvial or aeolian landforms in lowland areas requires cartographic data of resolution compatible with 1 : 10,000 scale. Nevertheless, less detailed digital elevation models, constructed at the scale of 1 : 50,000, are also extremely helpful, since they allow for regional interpretations of those morphostructures which are associated not only with neotectonics, but also with ice-flow directions, block disintegration of an ice-sheet, subglacial drainage, stages of fluvial erosion, or location of dune belts. A possibility of superposition of geological or geomorphological maps onto 3-D models is equally important, enhancing readability of the maps and providing clues to verification of the origin of landforms and proper cross-cutting relationships drawn on the map.
Słowa kluczowe
EN digital elevation model (DEM)   geological cartography   SW Poland  
Wydawca Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
Czasopismo Przegląd Geologiczny
Rocznik 2005
Tom Vol. 53, nr 10/2
Strony 977--983
Opis fizyczny Bibliogr. 25 poz., rys.
Twórcy
autor Badura, J.
autor Przybylski, B.
Bibliografia
1. BADURA J. 1996 - Morfotektonika Obniżenia Żytawsko-Zgorzelec- kiego. Prz. Geol., 46: 1239-1243.
2. BADURA J. 1999 - The influence of Cainozoic tectonic movements on geomorphological development of the Niemcza-Strzelin Hills. Quaternary Studies in Poland, Specl. Iss.: 219-225.
3. BADURA J., JAMROZ O. & ZUCHIEWICZ W. 2003a - Recent crustal mobility of the Upper Nysa Kłodzka Graben, SW Poland. Acta Montana, IRSM AS CR (2003), Ser. A, 24, 131: 65-71.
4. BADURA J., PÉCSKAY Z., KOSZOWSKA E., WOLSKA A., ZUCHIEWICZ W. & PRZYBYLSKI B. 2006 (in print) - Nowe dane o wieku i petrologii kenozoicznych bazaltoidów dolnośląskich. Prz. Geol.
5. BADURA J. & PRZYBYLSKI B. 1995 - Neotektoniczne aspekty rzeźby przedpola Sudetów Wschodnich. Prz. Geol., 43: 762-766.
6. BADURA J. & PRZYBYLSKI B. 1999 - Examples of young tectonic activity from the Sudetic Foreland, SW Poland - application of condensed contour map. Techn. Poszuk. Geol. Geosynopt. Geoter.: 38-45
7. BADURA J. & PRZYBYLSKI B. 2000 - Digital model ofterrain as an identification method of potential fault scarps in mountain and foreland areas - examples from SW Poland. [In:] W. Stackebrandt, S. Lorenc (eds.) Tagungsband zur 9. Jahrestagung der Gesellschaft fur Geowissenschaften e.V. Frankfurt/O Słubice 20-25.09.2000. Exkursionsfuhrer und Veroffentlichungen der Gesellschaft fur Geowissenschaften e. V. Berlin, Bd. 209: 34.
8. BADURA J., ZUCHIEWICZ W., GÓRECKI A., SROKA W., PRZYBYLSKI B. & ŻYSZKOWSKA M. 2003b - Morphotectonic properties of the Sudetic Marginal Fault, SW Poland. Acta Montana, IRSM AS CR (2003), Ser. A,23,131: 21-49.
9. CLARK C. D. 1997 - Reconstructing the evolutionary dynamics of former ice sheets using multi-temporal evidence, remote sensing and GIS. Quater. Sc. Rev., 16: 1067-1092.
10. CLARK C. D. & MEEHAN R. T. 2001 - Subglacial bedform geomorphology of the Irish Ice Sheet reveals major configuration changes during growth and decay. Jour. Quater. Sc., 16: 483-496.
11. CLARK C. D., EVANS D. J. A., KHATWA A., BRADWELL T., JORDAN C. J., MARSH S. H., MITCHELL W., A., BATEMAN M. D. 2004 - Map and GIS of glacial landforms and features related to the last British Ice Sheet. Boreas, 33: 359-375.
12. FISHER T. G. & TAYLOR L. D. 2002 - Sedimentary and stratigra- phic evidence for subglacial flooding, south-central Michigan, USA. Quater. Inter., 90: 87-115.
13. GRANICZNYM. 1994 Strefynieciągłościtektonicznychwświetle korelacji wielotematycznych danych geologicznych na przykładzie okolic Żarnowca i Ziemi Kłodzkiej. Instrukcje i Metody Badań Geol., 54: 1-82.
14. GRYGAR R. & JELINEK J. 2003 - The Upper Morava an Nysa pull-apart grabens- the evidence of neotectonic dextral transtention on the Sudetic fault system. Acta Montana, IRSM AS CR (2003), Ser. A, 23, 131: 51-59.
15. JORGENSEN F. & PIOTROWSKI J. A. 2003 - Signature of the Baltic Ice Stream on Funen Island, Denmark during the Weichselian glaciation. Boreas, 32: 242-255.
16. MIGON P. 1996 - Struktura morfotektoniczna centralnej części Sudetów Zachodnich w świetle mapy zagęszczonych poziomic. Czas. Geograf., 67: 233-244.
17. MUNRO M. & SHAW J. 1997 - Erosional origin of hummocky terrain in south central Alberta, Canada. Geology, 25: 1027-1030.
18. MUNRO-STASIUK M. J. & SHAW J. 2002 - The Blackspring Ridge Flute Field, South-central Alberta, Canada: evidence for subglacial sheetflow erosion. Quater. Intern., 90: 75-86.
19. OSTAFICZUK S. 2003 - Znaczenie wysokościowego numerycznego modelu terenu w kartografii geologicznej. Techn. Poszuk. Geol. Geosynopt. i Geoter., 224: 53-58.
20. PRZYBYLSKI B. 1998 - Glacial and neotectonic constraints on the Quaternary evolution of the Fore-Sudetic reach of the Nysa Kłodzka River. Geol. Quarter., 42: 221-238.
21. PRZYBYLSKI B. & BADURA J. 2004 - Czy struktury koliste w Sudetach mogą mieć genezę uderzeniową? Prz. Geol., 52: 971-978.
22. RAUNHOLM S., SEJRUP H. P. & LARSEN E. 2003 - Lateglacial landform associations at Jaren (SW Norway) and their glaci-dynamic implications. Boreas, 32: 462-475.
23. SHERROD B. L., BROCHER T. M., WEAVER C. S., BUCKNAM R. C., BLAKELY R. J., KELSEY H. M., NELSON A. R. &HAUGERUD R. 2004 - Holocene fault scarps near Tacoma, Washington, USA. Geology, 32: 9-12.
24. SJORGEN D. B., FISHER T. G., TAYLOR L. D., JOL H. M. & MUNRO-STASIUK M. J. 2002 - Incipient tunnel channels. Quater. Intern., 90: 41-56.
25. ZUCHIEWICZ W. 1995 -Neotectonics of Poland: a state-of-the-art review. Folia Quater., 66: 7-37.
Kolekcja BazTech
Identyfikator YADDA bwmeta1.element.baztech-article-BUS2-0015-0031
Identyfikatory