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Łapino
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(Utworzył nową stronę „== Przypisy == <references /> == Bibliografia == * Stępniewski Marian, Borucki Jerzy, (2001), '''Pseudometeorite from Łapino (Pomerania, North Poland).''' ''Ge...”) |
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| + | ;Fragment pracy<ref>Stępniewski et al. 2001</ref> | ||
| + | :The boul der was found in sum mer 1954 in a gravel pit on the slope of the Radunia val ley, near the lit tle set tle ment of Lower Łapino (18°28’20” E, 54°16’20” N) in the Pomerania | ||
| + | re gion, some 20 km south from Gdansk. The pit was ac tive here from 1888 till about 1975, and at pres ent the partly drowned work ings are cov ered with young trees and bushes. The boulder was no ticed by min ers in 1954 and its me te or itic or i gin was suggested because of its notable magnetic suscepti bil ity and un usual ap pear ance. The boul der Łapino is quite unlike the erratic boul ders (mostly granitoids and gneiss es) brought from | ||
| + | Scandinavia by Quaternary continen tal glaciers, which are abun dant in the gla cial deposits (Rühle, 1974). The boul der was con veyed to the As tro nom i cal Ob ser va tory of the War saw Uni ver sity, where it was stored up till 1996. Then it was transferred to the Pol ish Geo log i cal In sti tute, to resolve the or i gin of the stone (Stepniewski, 1997; Stepniewski and Pilski, 1998). | ||
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== Przypisy == | == Przypisy == | ||
Wersja z 01:16, 2 sty 2011
- Fragment pracy[1]
- The boul der was found in sum mer 1954 in a gravel pit on the slope of the Radunia val ley, near the lit tle set tle ment of Lower Łapino (18°28’20” E, 54°16’20” N) in the Pomerania
re gion, some 20 km south from Gdansk. The pit was ac tive here from 1888 till about 1975, and at pres ent the partly drowned work ings are cov ered with young trees and bushes. The boulder was no ticed by min ers in 1954 and its me te or itic or i gin was suggested because of its notable magnetic suscepti bil ity and un usual ap pear ance. The boul der Łapino is quite unlike the erratic boul ders (mostly granitoids and gneiss es) brought from Scandinavia by Quaternary continen tal glaciers, which are abun dant in the gla cial deposits (Rühle, 1974). The boul der was con veyed to the As tro nom i cal Ob ser va tory of the War saw Uni ver sity, where it was stored up till 1996. Then it was transferred to the Pol ish Geo log i cal In sti tute, to resolve the or i gin of the stone (Stepniewski, 1997; Stepniewski and Pilski, 1998).
Spis treści |
Przypisy
- ^ Stępniewski et al. 2001
Bibliografia
- Stępniewski Marian, Borucki Jerzy, (2001), Pseudometeorite from Łapino (Pomerania, North Poland). Geological Quartely, vol. 45 (3), 2001, s. 343-348. Plik PDF .
Linki zewnętrzne
Co brakuje na stronie?
- fotografia pseudometeorytu
