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Elephant Island

Profile

Path to the site

Antarktika / Westantarktis / Antarktische Halbinsel / South Shetland Islands / Elephant Island

Journey Description

Die Elephant Island ist die Größte einer kleinen Gruppe von Inseln, welche das N Ende der South Shetland Islands bedeuten.

Geology

Spheniscidit wurde unter Pinguin-Nestern gefunden und bildet sich durch Wechselwirkung einer Phosphat-Lösung aus dem Guano mit Glimmer- und Chlorit-Mineralien aus der Erde unter den Nestern.

Mineralienatlas short URL

https://www.mineralatlas.eu/?l=18073
Please feel free to link to this location

Shortened path specification

Elephant Island, South Shetland Islands, Antarktische Halbinsel, Westantarktis, AQ
Useful for image descriptions and collection inscriptions

Important: Before entering this or any other place of discovery you should have a permission of the operator and/or owner. Likewise it is to be respected that necessary safety precautions are kept during the visit.

Additional Functions

Minerals (Count: 2)

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Hint

- Click on one or more elements to see only minerals including this elements (green background).

- Click twice to exclude minerals with this element (green background, red text color).

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Legend

Mineral -> approved mineral
Mineral (TL) -> mineral type locality
Mineral -> not approved mineral
-> pictures present
 5 -> number of part localities with these mineral
 M -> Link to common mineral page
 i -> Information etc.
 r -> Reference
Mineral ? -> Occurrence douptful

Actuality: 25. Mar 2024 - 15:28:25

Rocks (Count: 1)

Refresh list | View legend

Legend

Rock -> name of the rock
Rock (TL) -> rock type locality
-> pictures present
 5 -> number of part localities with these rock
 R -> Link to common rock page
 i -> Information etc.
 r -> Reference
Rock ? -> Occurrence douptful

Actuality: 25. Mar 2024 - 15:28:25

Subsidiary Pages

Refresh list | Fold level: 2 - 3 - 4 - 5 - Unfold all

Actuality: 25. Mar 2024 - 15:28:25

Reference- and Source indication, Literature

Literatur:

  • Wilson, Bain (1986). Spheniscidit. Min. Mag. 50, 291. (Typ-Publ.)
  • Fehr, T. (1987). Neue Mineralien: Spheniscidit. Lapis, Jg.12, Nr.2, S.31-32.

IDs

GUSID (Global unique identifier short form) Tb0A8ocUfEeM-xO7doVIow
GUID (Global unique identifier) F200BD4D-1487-477C-8CFB-13BB768548A3
Database ID 18073