Areas & Ranges
Page Type: Area/Range
Julian Alps, Slovenia, Europe
46.38000°N / 13.85000°E
Hiking, Mountaineering, Trad Climbing, Sport Climbing, Via Ferrata, Skiing
Spring, Summer, Fall, Winter
9396 ft / 2864 m
Created/Edited: Nov 7, 2004 / Mar 13, 2016
Object ID: 153307
Page Score: 96.87%
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What's New On This Page?> September 21th, 2015: Geological Outline added
> SP V3 design updated.
> December 24th, 2006 - new pictures embedded.
> March 28th, 2005 - Links to the new page inserted: Rz.
> February 13th, 2005 - Links to the new page inserted: Zadnjiški Ozebnik.
The Purpose of This PageOn this page I would like to give an overview information of Triglav subgroup (Julian Alps), in order not to be repeated on all distinct summit pages. The map below links you to distinct summit pages on SummitPost! Regarding pictures and routes, this page is the place only for overall information.
General about Triglav Group
Triglav subgroup from the NE, from Karavanke range.
|Triglav Subgroup stands on the very NE part of Julian Alps, where these lower significantly to forehills (beyond Sava Bohinjka river) and to Gorenjska plane. Borders of the group are: Luknja pass - Vrata valley - Sava Dolinka valley - Sava Bohinjka valley - The Upper Bohinj valley - Voje valley - Mišeljska dolina (valley) - Hribarice plateau - Prehodavci Pass - Zadnjica valley - Luknja pass.|
All the highest peaks of this group are concentrated on its western part. In the central and southern part there's a broad high plateau, named Pokljuka, covered almost completely with beautiful forests and nice alpine meadows. On the NE part, beyond Radovna valley, there is a mountain range, or high plateau, named Mežaklja, which still belongs to Julian Alps, but its highest peak reaches only the altitude of 1593 m.
Geological OutlineIn the geological sense the Triglav group is not very complex. In a simplified version we could actually say that its mountains are built of Triassic limestone, some 205-235 million years old). Still scholars would find some interesting differences in those rocks.
Most of the massif - including the huge North Wall of Triglav and many mountain peaks - are made of the young Dachstein limestone (Norian and Rhaetian era). But the very summit of Triglav and also the broad area south of it are a bit older by origin (a few million years). Those massive, also layered limestones belong to the so-called "Slatenska plošča" ("Slatna Plate"), which is thrusted over the younger rocks. Finally, as it is typical for the whole group of Julian Alps, the northern parts of the group are made of stratified limestone and dolomitic rocks from the Carnian era (some 20 million years older than the Dachstein limestone). And that's basically it. Only some distinct rock structures in the group are even older - made of Ladinian limestone.
Still, this outline refers only to the high mountains. Describing the lower areas of the massif - down to the Gorenjska Plane around Bled - that would require a bit more time and details.
Some Geography and Characteristics of Mountains