![]() |
![]() |
![]() |
|||
|
From
the mineralogical point of view, ice is a mineral - the crystalline phase
of hydrogen oxide. Analogue to calcite, ice is subject to dripstone formation
in caves, were it builds up stalagmites, stalactites, draperies and even
helectites quite similar to the ones made by calcium carbonate. During
cold winter spells, we can observe time-lapse dripstone formation in the
entrance areas of some caves. A transient decoration, vanishing as soon
as temperatures rise again. In alpine caves, where temperatures are permanently
below freezing, most water contributes to the build up of ice, leading
to the formation of sometimes giant ice domes.
|
||||
www.speleo-foto.de
- cave photography by Max Wisshak
© Max Wisshak 2002-2012 - Alle Rechte vorbehalten
© Max Wisshak 2002-2012 - All rights reserved