Mons Rainier
Appearance

Mons Rainier seu Tahoma est mons ignifer in civitate Vasingtonia Civitatum Foederatarum. Altitudo eius est 4391 metra, altissimum Vasingtoniae. Ob magnam probabilitatem eruptionis in proximo futuro et propinquitatem ad magnam aream urbanam, Seattlum Tacomaque inclusis, Mons Rainier inter periculosissimos vulcanos in mundo habetur.
Bibliographia
[recensere | fontem recensere]- Crandell, Dwight (1969). Surficial Geology of Mount Rainier National Park, Washington. U.S. Geological Survey
- Jerry F. Franklin; William H. Moir; Miles A. Hemstrom; Sarah E. Greene; Bradley G. Smith (1988). The Forest Communities of Mount Rainier National Park. National Park Service
- Haines, Aubrey L. (1962). Mountain fever, historic conquests of Rainier. Portlandiae: Oregon Historical Society
- F. E. Matthes (1928). Mount Rainier and Its Glaciers. National Park Service
- Edmond S. Meany, ed. (1916). Mount Rainier: A Record of Exploration. Novi Eboraci: The Macmillan Company
Nexus interni
[recensere | fontem recensere]Nexus externi
[recensere | fontem recensere]| Vicimedia Communia plura habent quae ad Rainier montem spectant. |
| Situs geographici et historici: Locus: 46°51′6″N 121°45′37″W • GeoNames • Thesaurus Getty • Peakbagger • Global Volcanism Program • Store norske Lexikon • "1533614" apud USGS |
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Haec stipula ad geographiam spectat. Amplifica, si potes! |
