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| fpetel115. 04. 2009 21:51:20 |
Last week on Friday it was snow-free from Brezje almost to the hut height (to cca. 1450m). To the top there's still about a meter of snow that sinks to the waist in places if we go our own way.
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| jozev18. 04. 2009 14:43:36 |
I'd like to correct user fpetel1. Not from Brezja but from Brezij. I'm from Brezij (Sv. Neža) myself and go to Dobrča especially in winter two to three times. Snow really starts at the hunting hut.
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| matic419. 04. 2009 11:06:39 |
jozev those pics aren't all from yesterday. If you're posting them all in order, write at least the date in the comment. Only 5th and 6th are from yesterday.
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| meri13. 05. 2009 07:57:02 |
Last weekend on Sunday I was on Dobrča and must say I haven't seen such a natural 'garden'. Meadows full of dark blue gentians, yellow and purple globeflowers and excellent dandelions I picked enough for a proper salad Really worth checking out.
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| zamet28. 05. 2009 20:55:36 |
I'm curious about the path to Dobrča. Last year I drove from Begunje-Tržič direction, and somewhere in the middle I think it's the village Hudi graben, there was a sign for Dobrča by the road in the forest, how far from there to the top or can you park the car there..
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| serajko28. 05. 2009 21:12:52 |
Approx. 1h 30min. There is also parking for a couple of cars. (easy marked path) lp
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| zamet28. 05. 2009 21:19:37 |
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| zamet30. 05. 2009 13:48:00 |
This morning on Dobrča to the hut: no issues except unmarked starting point, then at the hut snow, lightly whitened, to the top still lightly snowing, after half an hour sun came out and it went away.
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| PUHI14. 07. 2009 08:22:39 |
On Thursday 9.7. on Dobrča after long time no rain. Meadows all blooming, lots of thyme, highly recommended family outing.
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| MarkoK21. 12. 2009 14:03:54 |
Yesterday's day dedicated to visiting Dobrča, which turned out to be a very nice, panoramic mountain in wonderful, albeit slightly cold weather. But this weather allowed "proper" views in all directions, as evidenced by the photos in the attachment. The trail is well-trodden, the hut open and very friendly, everything is good. Especially nice view from Šentanski vrh. Start from Brezje above Tržič, ascent via the transverse path, descent via Bistriška planina to the starting point. I recommend it.
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| esther3. 01. 2010 18:20:08 |
If you meant me, I'm not Anja but Esther Regards
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| viharnik3. 01. 2010 18:26:51 |
Yes, Esther, sorry, and attach some group photo. Regards
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| Tadej3. 01. 2010 19:32:44 |
A few more photos from today's trip to Dobrča.
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| viharnik4. 01. 2010 16:19:03 |
Tadej, as far as I know Dobrča belongs to Karavanke. Only the massif of Tolsti vrh together with Storžič belongs to K.S. Alps. If wrong (Stanko Klinar-Karavanke, editor Franci Savenc), correct me. Lp-Rok
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| Tadej4. 01. 2010 16:26:08 |
The Kamnik-Savinja Alps extend all the way to Žirovnica. Thus including Dobrča and the Brezniške peči ridge. Lp Tadej
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| viharnik4. 01. 2010 16:31:55 |
Then it holds according to the new one. Guide from '83, 3rd revised edition didn't account for that then. I was taught so too. Thanks and good luck!
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| viharnik4. 01. 2010 16:40:09 |
Yes, I see, damn it, thanks rerze11, back then K.S. already ended in Tržič. 
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| JusAvgustin4. 01. 2010 17:36:08 |
It depends on which perspective you look from. I myself have quite some knowledge about geology (that's one criterion), the second criterion is the average elevation of the relief, and we could find some more criteria. The fact is that the border between ranges runs through geologically unexplored territory (that's why there was/is and will be an eternal dilemma among geologists what is what). I am of the opinion that the Karavanke are nicely separated from KS Alps, namely by the age of rocks, geotectonic structures and slopes. We can discuss on this forum where the dividing line is and why it's there. I follow the geological (lithological) dividing line, as I think it's the most correct. By the way, Boč falls under Karavanke... if anyone has interest to learn a bit more, I have a whole bunch of literature on the topic. A clear difference is visible in the rock transition (from Mesozoic to the new age of geological history). What new did we learn? We just additionally complicated the matter...
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