Szczegóły publikacji
Opis bibliograficzny
Cechy geomorfologiczne i sedymentologiczne misy jeziornej Morskiego Oka i górnej części Doliny Rybiego Potoku w świetle badań geofizycznych — Geomorphological and sedimentological features of Morskie Oko Lake and upper reach of Rybi Potok Valley in the light of geophysical investigation / Maria Baumgart-Kotarba, Jerzy DEC, Adam Kotarba, Ryszard ŚLUSARCZYK // W: Z badań fizycznogeograficznych w Tatrach, 2 = Physical geography study in the Tatra mountains / pod red. Adama Kotarby. — Wrocław : Wydawnictwo Continuo, 1996. — (Dokumentacja Geograficzna ; ISSN 0012-5032 ; 4). — ISBN: 83-86682-09-4. — S. 9–31. — Bibliogr. s. 30–31, Summ. — J. Dec, R. Ślusarczyk - brak afiliacji AGH
Autorzy (4)
- Baumgart-Kotarba Maria
- AGHDec Jerzy
- Kotarba Adam
- AGHŚlusarczyk Ryszard
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 67967 |
|---|---|
| Data dodania do BaDAP | 2012-09-27 |
| Tekst źródłowy | URL |
| Rok publikacji | 1996 |
| Typ publikacji | fragment książki |
| Otwarty dostęp |  |
| Czasopismo/seria | Dokumentacja Geograficzna |
Abstract
Natural environment of the Tatra National Park is strictly protected by law. Therefore geophysical investigation has been adopted in geomorphological and sedimentological research in the upper reach of the Rybi Potok Valley, including glacial cirque of the Morskie Oko Lake. The main aim of these studies is to learn about Late Glacial and Holocene sediments, first of all thickness of lacustrine sediments in the Morskie Oko basin, as well as to determine granite bedrock morphology. During the period between 1993 and 1995 experimental seismic investigation has been carried out. For the sediment thickness investigation vertical array of hydrophones hanging in water and seismic source "sparker" has been applied. Both hydrophones and elastic wave source are environmental friendly. In order to define basement morphology seismic reflection method has been applied. Investigation of granite basement has been extended over Rybi Potok Valley in order to define a shape and depth of a basement in the foreland of the Morskie Oko Lake. For this purpose the refraction method with the accelerated weighting drop (as a seismic waves source) was applied. On illustrations some results of investigation are presented.