Lodowiec Malaspina
Zdjęcie lodowca Malaspina wykonane z pokładu wahadłowca Atlantis, podczas misji STS-66 (1994) | |
Państwo | |
---|---|
Stan | |
Powierzchnia | 4000 km² |
59°55′09″N 140°31′59″W/59,919200 -140,533000 |
Lodowiec Malaspina – lodowiec podgórski (piedmontowy) na południowym wybrzeżu Alaski, w USA, u podnóża Góry Świętego Eliasza. Jego powierzchnia wynosi około 4000 km². Nazwa lodowca pochodzi od nazwiska włoskiego odkrywcy Alessandro Malaspina.
Media użyte na tej stronie
Autor: Alexrk2, Licencja: CC BY 3.0
Location map of Alaska, USA
Equirectangular projection, N/S stretching 210.0 %. Geographic limits of the map:
- N: 72.0° N
- S: 51.0° N
- W: 172.0° E
- E: 129.0° W
Autor: Uwe Dedering, Licencja: CC BY-SA 3.0
Location map of North America with national borders.
- Projection: Lambert azimuthal equal-area projection.
- Area of interest:
- N: 90.0° N
- S: 5.0° N
- W: -140.0° E
- E: -60.0° E
- Projection center:
- NS: 47.5° N
- WE: -100.0° E
- GMT projection: -JA-100/47.5/20.0c
- GMT region: -R-138.3726888474925/-3.941007863604182/2.441656573833029/50.63933645705661r
- GMT region for grdcut: -R-220.0/-4.0/20.0/90.0r
- Made with Natural Earth. Free vector and raster map data @ naturalearthdata.com.
The flag of Navassa Island is simply the United States flag. It does not have a "local" flag or "unofficial" flag; it is an uninhabited island. The version with a profile view was based on Flags of the World and as a fictional design has no status warranting a place on any Wiki. It was made up by a random person with no connection to the island, it has never flown on the island, and it has never received any sort of recognition or validation by any authority. The person quoted on that page has no authority to bestow a flag, "unofficial" or otherwise, on the island.
MALASPINA GLACIER, ALASKA (STS066-117-014). Malaspina Glacier can be seen in this north-northeastern photograph taken in figure 12. The glacier, located in the south shore of Alaska is a classic example of a piedmont glacier lying along the foot of a mountain range. The principal source of ice for the glacier is provided by the Seward Ice Field to the north (top portion of the view) which flows through three narrow outlets onto the coastal plain. The glacier moves in surges that rush earlier-formed moraines outward into the expanding concentric patterns along the flanks of the ice mass.