No Name Description
12
This is the largest rock in the Baltic States and, according to some sources, in all of the segment of Northern Europe which was affected by the last Ice Age. Its size is 930 m3! The rock is 7.5 m high, 16.5 m long and 14 m high, with a circumference of 48.5 m. The rock resembles a huge pebble from a distance, and it is on the sandy and rocky beach. Depending on the season, it can be out in the water. The Ice Age carried the rock to its current location from the southern shore of Finland. It is made of pegmatite.
21

This is actually a group of nine craters, and some of them are as much as 100 m in diameter and 16 m in depth. This is the most visually expressive meteorite crater in the Baltic States and, indeed, in all of Europe. Remnants of the meteorite – some 2.5 kg in all – yielded iron and nickel. It is thought that this pan-Baltic natural catastrophe occurred 2,600 to 4,000 years ago.

Kaali Visitor Centre comprises the meteoritics and limestone museum, a conference hall and a hotel.The museum exhibits genuine meteorite pieces amongst other items. The hotel has all modern conveniences, tasty food is provided at Kaali Tavern nearby.

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Ap 7 km garš lokveida pārgājienu maršruts (marķēts), kas ved pa dažādiem biotopiem – mežiem, mitrājiem un pļavām, mezdams līkumus pa stāvo pauguru nogāzēm. Takas malās ir izvietoti informācijas stendi un norādes. Rebases ainavu taka ir domāta tiem, kurus nebaida garāka iešana un orientēšanās pa ļoti dabisku un mazapdzīvotu apvidu.

33
This is a highland swamp with several little lakes. At the SE of the area is a wooden trail.
32
This is one of the most beautiful ancient river valleys in Estonia – 12 km long with nearly 40 revealed Devonian sandstone cliffs. Among these, the most important ones are Viira müür, Kalamatu müür, and Põdramüür.
10
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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This is the 11th largest Estonian island, and its central section is covered by a broadleaf forest (linden, oak, elm and other trees) that is more than 100 years old. Along the shores, the Abruka Island has meadows and small areas of wetlands. Only the northern part of the island is populated. Few tourists come to call, which means that the island is relatively untouched by humankind.
9
This is one of Estonia’s most beautiful karst fields, covering 125 hectares which feature different karst processes – subterranean streams, the dry Jõelähtme River bed, karst streams, funnels, ditches, caves, cliffs, a unique rock “mushroom,” etc. During the spring, the field is flooded, but at other times of the year, its contents are easily visible.
8
This is the second largest rock in the Baltic States in terms of size (728 m3). It is the only rock in the Baltic States with this form and size. It is 7 m high, 19 m long, 11 m wide, and 58 m in perimeter. Kabelikivi looks like a cliff that is halfway sunk into the earth. During the Ice Age, the rock “travelled” to this location from southern Finland. It is made of granite, and there are two other very impressive rocks alongside it.
14
This is a cliff with various levels. Known as the North Estonian cliff, it stretches all along the shore of the Bay of Rīga in Estonia, including some of the local islands. The most expressive part in geological and landscape terms is the Saka-Ontika-Toila cliff, which is around 22 km long and offers an unusual natural environment. The cliff is as much as 53 m high, and it has a fairly virginal forest along its slopes. The layers of clay, sandstone, limestone, etc., come from the Cambrian and Ordovician periods. The Valaste juga (Valaste waterfall) is 24 metres high. After a longer period of freezing temperatures, the waterfall has a particularly impressive appearance. Seasonal waterfalls (8-10 m) can be found near the villages of Ontika and Toila.

1,7 km gara lokveida taka, kas iepazīstina ar dažādiem meža biotopiem, to iemītniekiem un meža apsaimniekošanas pamatprincipiem. Apmeklētāju ērtības nolūkā ir izveidotas koka laipas un neliels skatu tornis.

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The company provides wildlife tours – seal watching, walking, cycling or skiing trips, rubber boat trips to Vilsandi and other islands, orchid trips, and trips to learn about culture and life of the manors, towns and villages, crafts and seafaring. Miku forest park in Vilsandi National Park is where visitors can learn about and try various forestry jobs.
The Vilsandi NP centre is in Loona Manor along with a guesthouse and café-restaurant (www.loonamanor.ee).

17
The Kassari Island is the fifth largest Estonian island, and it is found to the South of the Hiiumaa Island. There are two dams between the two islands, and a road for motor vehicles has been installed atop them.
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Der weiteste Nordpunkt der Insel Hiiumaa. Der höchste Leuchtturm Estlands aus Roheisen (1873 – 1875) und das Denkmal zur Errinerung an die bei dem Unglück des Schiffes ‘Estonia” Umgekommenen.

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The company runs wildlife tours: kayak trips at sea in summer, bogshoeing in bogs in autumn, snowshoeing trips in winter and canoeing on rivers in spring.
Nature lovers enjoy our wildlife viewing tours: brown bear safaris and birdwatching in spring, elk, seal and wolf-themed tours in autumn.


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.


Nacionālā parka dienvidrietumdaļā jūrā iestiepjas Eldas pussala – skaists un ļoti  omaļš ar kadiķu mežu (alvāriem) noaudzis zemes pleķītis ar interesantu jūras krastu, kur atsedzas silūra perioda nogulumieži. No pussalas gala, kurā slejas vecs Padomju armijas robežsargu tornis (apmeklējumam bīstams!), paveras visaptverošs skats uz Vilsandi salu (atpazīstama pēc bākas), Lonalaidas salu (Loonalaid) – otru lielāko Vilsandi arhipelāgā, Salavu (Salava) un citām mazākām saliņām. Dabas mīļotāji var uzmeklēt Eldas klinti (Elda pank) – ~ 2 m augstu un 0,4 km garu atsegumu, kura piekājē var atrast interesantas ūdens izskalotas fosilijas.


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.


No vairākiem parka ūdenskritumiem noteikti ir jāapmeklē divi. 1,2 m augstais vienpakāpes Nemmeveski ir izveidojies uz Valgejegi upes (Valgejõgi), vietā kur tā šķērso Ziemeļigaunijas glintu. Šeit Valgejegi atgādina krāčainu (īpaši – pavasaros) kalnu upi, kas plūst pa vairākus metrus augstu klinšu ieskautu kanjonu. Palu laikā šo upes posmu ir iecienījuši ekstrēmie ūdenssporta veidu cienītāji. Pie ūdenskrituma un tālāk pa upi lejup redzamas ap 1920. g. celtās hidroelektrostacijas konstrukciju paliekas.


Divus kilometrus garās lokveida takas sākums ir meklējams pie Somā nacionālā parka apmeklētāju centra (atklāts 2000. gadā) – Tēramā ciemā. Tā ved gar Mardu strauta (Mardu oja) krastu, kur krustām šķērsām ir sakrituši bebru nogāztie koki, radot diezgan juceklīgu skatu. Apmeklētāju centrā var iegūt nepieciešamo informāciju, noskatīties videofilmu un nacionālajam parkam veltītu ekspozīciju.