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Sāmsalas ziemeļrietumu daļā jūrā iestiepjas iespaidīgā Tagameizas pussala (Tagamõisa poolsaar). Tās ziemeļrietumu daļā meklējama mazāka – ap 5 km garā Harilaidas pussala (Harilaid). Pussalas vidusdaļā viļņojas Lajalepas ezers (Laialepa järv) - bijušais jūras līcis, kas zemes garozai ceļoties, kļuvis par iekšēju ūdenstilpi. Arī pati Harilaida (igauniski „laid” nozīmē „saliņa”) vairāk nekā trīs gadsimtus atpakaļ bijusi sala. Harilaidu iecienījuši ne tikai migrējošie putni, bet arī roņi, kurus piesaista vientuļi līči un akmeņainās sēres. Harilaidu var apmeklēt tikai ar kājām vai ar divriteni, bet spēkrati ir jāatstāj autostāvlaukumā. No tā ~ 1 km attālumā atrodas vieta, kur pēc 17. gs. radies Harilaidas savienojums ar Sāmsalu. Šeit paveras nepierasti klaja un akmeņaina ainava. Pārējā Harilaidas daļa ir apmežota pirms ~ 40 gadiem. Kopumā būs jāveic ~ 10 km garš pārgājiens. |
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Karulas augstienes augstākais reljefa punkts (137 m.vjl.), kas virs tuvākās apkārtnes paceļas par ~ 60 m. Torņa kalnā ir uzbūvēts skatu tornis ar ļoti plašu apkārtskatu. Uz tā platformas ir novietoti panorāmas fotoattēli, kuros atzīmēti zīmīgākie plašākā apkaimē redzamie objekti – apdzīvotas vietas, pilskalni, baznīcu torņi u.c. Turpat izveidota atpūtas vieta un meklējams Rebases ainavu takas sākums. |
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This reserve dates back to Lake Ancilus, which was one of the original elements of what is now the Baltic Sea. The lake’s ancient shores feature wetlands, forests and flora which are all protected by the reserve.
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Gas mixture is the main raw material for Estonia’s energy and chemical industries, and it is extracted in our day from open quarries or underground shafts. This layer was established during the Ordovician Period between 450 and 480 million years ago, and it is made up of the remnants of plants and animals from that age. In the Kohtla-Nõmme suburb, there is a shaft which can be toured in the company of a guide who will tell you that this is the only layer of its kind in the Baltic States. He will tell you about how the gas mixture has been extracted over the course of history.
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This is one of the greatest waterfalls in the Baltic States – 8 m high and up to 70 m wide. It is most impressive in the spring and after strong rains. The waterfall and its ~300 m canyon emerged from the limestone of the Ordovician Period. You may spot some fossils there. When the water is low, courageous people try to ford the river both above and below the waterfall. The limestone and the falling water have established a unique “tunnel” there.
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One of the largest karst areas in Estonia is found here. The unique Witch’s well is one of the most interesting parts of this area. During spring floods (not every year, and for only a short period of time), the well erupts with underground river waters to create an unusually powerful karst stream that can pump out as much as 100 litres per hour.
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Bijušā piecstāvīgā metāla skatu torņa apkaimē plešas Lemmjegi upes palieņu pļavas. Netālu atrodas kādreizējā Oksas kroga (Oksa kõrts) vieta, kur saglabājies iespaidīgs manteļskurstenis. Apkaimes apskatei izveidota 0,8 km gara koka laipu taka. |
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Litorīnas jūras laikā (pirms ~ 6000 gadiem) Saleveres Salumegi kalns bija sala, bet mūsdienās tas kā izteikta kāple (īpaši - ziemeļu pusē) paceļas virs Piejūras līdzenuma. Salumegi ziemeļu pusē slejas 4 - 5 metrus augsts kaļķakmens atsegums – silūra perioda (> 400 mlj. gadu) koraļļu rifa paliekas, kuru noskalojuši Litorīnas jūras viļņi. Atseguma piekājē izplūst Acu avots, kam piedēvē dziednieciskas īpašības. Salumegi apskates nolūkos izveidota lokveida taka (1,5 km). No kalna augšas paveras labs skats uz Matsalu līci. Šeit atradies arī sens pilskalns. |
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This is a “peripheral” island in the Bay of Finland, 9 km from the Dirhami port. The special fact about this island is that it offers fields of juniper, a rocky and grassy seashore that is around 2 km long, and limestone cliffs that are a few metres high along the northern and the eastern shores of the island. These are designated with the words Osmussaare pank.
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Cultural space of Kihnu (www.kultuuriruum.ee) is incorporated in the UNESCO list of Masterpieces of Oral and Intangible Heritage of Humanity, and is a quaint mix of old and modern. The local history museum displays tools, clothes, handicraft and furniture. |
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This is one of the few places in the Baltic States where one can find Devonian period sandstone cliffs featuring abrasion caves, arches, etc. The cliffs are on the shores of Lake Peipsi (Peipsi järv), near Kallaste, and they are between two and four (in some cases – nine) metres high, stretching for a distance of around one km.
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Metāla tornis Kazari upes kreisajā krastā, ~ 5 km attālumā no Matsalu līča. No torņa redzamās Kazari deltas palieņu pļavas atrodas tikai 0,3 – 1 m augstumā virs jūras līmeņa, tādēļ pavasara palos un stipru vētru (īpaši rietumvēju) laikā ūdens appludina milzīgu teritoriju. Uzskata, ka platības ziņā šīs ir vienas no lielākajām Eiropas palieņu pļavām, kas ir nozīmīga dažādu tārtiņveidīgo putnu sugu ligzdošanas, dzērvju un zosveidīgo putnu atpūtas un barošanās vieta. Ir pagājis laiks, kad zemnieki Matsalu pļavās ganīja govis un pļāva sienu, tādēļ šobrīd pļavu apsaimniekošanu veic nacionālā parka administrācija. |
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Ein 3,5 km langer Pfad quert den Viru Moos in Richtung Süd–Nord. Von einem Holzaussichtsturm eröffnet sich einen Blick auf eine typische Hochmoorlandschaft mit einigen Seen, Aushöhlungen und morastigen Stellen. |
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This park was set up to protect the landscape and cultural environment of the Haanja highland. At the central part of the park are the two highest hills in the Baltic States – Suur Munamägi, which stands 318 m above sea level, and Vällamägi, which is 304 m above sea level. The ancient Rõuge River valley (Rõuge ürgorg) is found in the western part of the park. It is 7.5 km long and up to 60 m deep. The valley dates back to the Ice Age, and it has seven lakes, including the deepest one (38 m) in Estonia – Lake Rõuge Suurjärv.
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The national park was established to protect the 100 or so small islands that make up the archipelago of the local area. The largest island, the Vilsandi Island, is 6 km long and up to 2 km wide. You can rent a boat to get there, or, during appropriate conditions, you can walk across the sea and the small islands from the southern end of the Kuusnõmme peninsula.
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This park is in a region of hillocks in the Karula highlands, and Lake Ähijärve is at its centre. The park offers a cultural environment of small farms, and it was set up to protect the unique cupola-shaped hillocks of the area. Main attractions: Scenic Lake Ähijärv (176ha), Rebasemõisa Tornimägi hill (137.8 m above sea level), undulating landscapes. |
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The word “Soomaa” means “land of the swamps” in Estonian. There are several major swamps in this area, along with rivers, lowland meadows, wetland forests, and other biotopes that are of key importance in terms of the diversity of species. Major floods occur here in the spring, which is known by locals as the “fifth season''. The fifth season is the best time to explore the landscape of Soomaa. |
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This is the most visually impressive drumlin field in the Baltic States, and it is close to the village of Tabivere. The drumlins were established by ice glaciers, and they point in the direction in which the ice moved long ago. In terms of their appearance, the drumlins resemble loaf-shaped hillocks. From their “backs,” there are lovely views of the local landscape and the lakes that are around the area. The visitor centre is in the village of Äksi.
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This cliff is made of sandstone (its lower part) and limestone (the upper part). It is up to 30 m high, and it is part of the Northern Estonian set of cliffs along the shore of the Bay of Finland. This is a popular tourism destination and viewing location. Recommended Hike along the bottom of the cliff (a rocky beach) in one direction, and then along the top of the cliff to get back (~2 km). From the top of the cliff, you can see a broad segment of the shoreline territory, all the way to Tallinn.
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The highest and most beautiful wall of cliffs on Saaremaa Island (up to 21 m high), stretching along some 3 km. During strong winds from the W or NW, a part of the cliff is washed by the waves of the sea. The open face of the cliff has limestone, marls and dolomite, and there is a wealth of fossils at the base of the cliff – corals, stromatoporids, etc.
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