Kvartérní modelace zarovnaných po vrchů masivu Plechého na Šumavě = Quaternary modellation ot Ievelled surfaces ot the Plechý massif in the Šumava mts
Three types of levelled surfaces - platforms have been distinguished in the geomorphological district of the Plechý massif. The summit, saddle and slope platforms can au be found to contain relics of cryogenic weathering. The platforms within the massif lie in four altitude regions. The increase of the maximum altitude span of individual groups of platforms … celý popis
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Podrobná bibliografie
- Hlavní autor
- Typ dokumentu
- Články
- Fyzický popis
- 20 il.
- Publikováno v
- Acta Universitatis Carolinae. Geographica. -- 10, 1-2 (1975), s. 43-59
- Témata
- Popis jednotky
- 8 obr., 2 tab., 10 foto
Abstrakt © vydavatel - Bibliografie
- Literatura
Instituce:
Geografická bibliografie ČR online
MARC
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| 100 | 1 | |a Votýpka, Jan, |d 1938- |7 jk01150839 |4 aut | |
| 245 | 1 | 0 | |a Kvartérní modelace zarovnaných po vrchů masivu Plechého na Šumavě = |b Quaternary modellation ot Ievelled surfaces ot the Plechý massif in the Šumava mts / |c Jan Votýpka |
| 246 | 1 | 3 | |a Quaternary modellation ot Ievelled surfaces ot the Plechý massif in the Šumava mts |
| 300 | |b 20 il. | ||
| 500 | |a 8 obr., 2 tab., 10 foto | ||
| 500 | |a Abstrakt © vydavatel | ||
| 504 | |a Literatura | ||
| 520 | 3 | |a Three types of levelled surfaces - platforms have been distinguished in the geomorphological district of the Plechý massif. The summit, saddle and slope platforms can au be found to contain relics of cryogenic weathering. The platforms within the massif lie in four altitude regions. The increase of the maximum altitude span of individual groups of platforms is characteristically proportional to the decrease of the altitude above sea level. The platforms whose altitude above sea level is given in Table occur within the area consisting of plutonic rocks and are thought to represent the relics of early levelled surface which was broken and shifted into different heights | |
| 546 | |a Anglické resumé | ||
| 611 | 2 | 4 | |a Česko-polské geografické seminarium |n (6 : |d 1974 : |c Praha, Česko) |
| 650 | 0 | 7 | |a fyzická geografie |7 ph120423 |2 czenas |
| 650 | 0 | 7 | |a geomorfologické útvary |7 ph422363 |2 czenas |
| 650 | 0 | 7 | |a tektonika |7 ph116414 |2 czenas |
| 650 | 0 | 4 | |a physical geography |
| 650 | 0 | 4 | |a geomorphological features |
| 650 | 0 | 4 | |a geotectonics |
| 650 | 0 | 4 | |a geomorphological research |
| 651 | 7 | |a Plechý (Šumava, Česko) |7 ge339031 |2 czenas | |
| 650 | 0 | 4 | |a geomorfologický výzkum |
| 651 | 4 | |a Šumava | |
| 773 | 0 | |t Acta Universitatis Carolinae. Geographica |g 10, 1-2 (1975), s. 43-59 |q 10:1/2 |9 1975 | |
| 997 | |a AN | ||