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This cache has been archived.

Leptoceratops: Hello!
I'm archiving your cache as it has been disabled for more than a one month and it is lost, completely damaged or inappropriate. Caches should be visited and maintained within 30 days after disabling.
Archiving a geocache is meant to be a permanent action. If a cache is archived by a reviewer or staff for lack of maintenance, it will not be unarchived.

If there are still leftovers from container I would appreciate if other players could collect them so that there are no trash in the nature.

Happy geocaching!

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Gleznotājkalns

A cache by SimpleGuy_yt Send Message to Owner Message this owner
Hidden : 04/03/2016
Difficulty:
2 out of 5
Terrain:
2.5 out of 5

Size: Size: micro (micro)

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Geocache Description:


[LV] Ainavu, kas paveras no Paradīzes (gleznotājkalna) kalna, savās gleznās iemūžinājuši tādi slaveni latviešu gleznotāji kā Jūlijs Feders, Vilhelms Purvītis un Janis Rozentāls - tā arī radies vietas nosaukums – Gleznotājkalns. No Gleznotājkalna vērojams skats pat 12 kilometru attālumā. Pāri ielejai skatam paveras Turaidas pils tornis, lejā, pamatkrasta piekājē saskatāma seno Kalna Klauku māju vieta. Visizteiksmīgāko ainavu veido Gaujas senieleja un 80 metrus zemāk esošā Gauja. Agrāk par senielejas galveno rašanās cēloni uzskatīja senās ledāja kušanas ūdeņu straumes, taču izrādās, ka zem tagadējās redzamās Gaujas ielejas atrodas cita, daudz senāka, dziļi devona iežos iegrauzta ieleja. Gaujas senieleja sākusi veidoties pirms 370-300 miljoniem gadu, tagadējo veidolu tā ieguvusi pirms 12-13 tūkstošiem gadu, kad to pārveidojuši ledāja kušanas ūdeņu sanesumi.

[EN] Landscape that opens from Paradise Hill, immortalized in his paintings such famous Latvian painters as July Feder, Wilhelm Purvitis and Janis Rosenthal - it also created a place - Gleznotājkalns. From Gleznotājkalna observed in view of up to 12 kilometers away. Across the valley overlook Turaida castle tower, downstairs, bank of the foot of the ancient hill visible Klauku house place. Very best landscape consists of Gauja Valley and 80 meters below the existing permit. In the past, the main valley of the cause considered ancient glacier melting water currents, but it turns out that under the current visible Gauja Valley is another, much older, deep Devonian rocks iegrauzta valley. Gauja Valley started to form from 370 to 300 million years ago, the current form, it acquired 12-13 thousand years ago, when it transformed the glacier melting water silt.

Additional Hints (Decrypt)

Bgen frar. Nhtšn

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)



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