"Klint" redirects here. For the Swedish artist, see Hilma af Klint.
The Baltic Klint (Clint, Glint; Estonian: Balti klint, Swedish: Baltiska klinten, Russian: Балтийско-Ладожский уступ, Глинт) is an erosional limestone escarpment and cuesta on several islands of the Baltic Sea, in Estonia, in Leningrad Oblast of Russia and in the islands of Gotland and Öland of Sweden. It was featured on the reverse of the 50 krooni note of 1928 and on the 100 krooni note of 1992.
The Baltic Klint is active landform showing some retreat in the present.[1] However it is not known to which degree the Baltic Klint originated in postglacial time or if it evolved from cliff-like forms sculpted by the Fennoscandian Ice Sheet.[1] In Gotland 20th century cliff retreat rates have been estimated at 0.15 to 0.78 cm/year.[1] Retreat of the Baltic Klint in Gotland has widened shore platforms.[1]
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The BalticKlint (Clint, Glint; Estonian: Balti klint, Swedish: Baltiska klinten, Russian: Балтийско-Ладожский уступ, Глинт) is an erosional limestone...
the Bay of Kiel are parts of the Baltic Sea. Another usual border is the line between Falsterbo, Sweden, and Stevns Klint, Denmark, as this is the southern...
Panga Cliff (Estonian: Panga pank) (also Mustjala cliff) is a coastal cliff located on the northern shore of Saaremaa, at the end of the Kuressaare - Võhma...
Byrums raukar are a geological formation of a group of rauks (Swedish term for stacks) on the western shore in the north of Öland, Sweden (the island forming...
enclosed by chalk escarpments. Sweden, Estonia and Russia BalticKlint Gotland–Saaremaa Klint South Småland-Sub-Cambrian escarpment Malta Victoria Lines...
formed by Valaste Creek (Estonian: Valaste oja) as it flows over the BalticKlint not far from the shore of the Gulf of Finland. It is a popular tourist...
from the original on 29 December 2019. Retrieved 28 December 2019. "BalticKlint". UNESCO World Heritage Centre. Archived from the original on 29 December...
Sillamäe, wherever limestone comes to the surface near the seashore (see BalticKlint), as well as on the islands of the West Estonian archipelago. Estonia...
Tobias Estonia Theatre 1994 100 krooni €6.40 Light blue Lydia Koidula BalticKlint 1991, 1992, 1994, 1999, 2007 500 krooni €31.96 Purple Carl Robert Jakobson...
escarpment, the BalticKlint, with a height up to 55 m (180 ft). In the east, the gulf ends with Neva Bay; in the west it merges with the Baltic Sea. The gulf...
rauks are chiefly formed along or near the escarpment known as the BalticKlint. Gotland rauks consist of limestone representing reefs that existed in...
Narva Reservoir (Estonian: Narva veehoidla; Russian: Нарвское водохранилище, romanized: Narvskoye vodokhranilishche) is a reservoir by the Narva River...
rest, facing the Russian city of Ivangorod, the Narva flows over the BalticKlint, forming Narva Falls, once among the most powerful in Europe. Before...
rocks protrudes from the cover of younger deposits, cropping out in the BalticKlint at the coast and at a few places inland. The Ordovician rocks are made...
Rudolf Tobias The Estonia Opera House in Tallinn EEK 100 Lydia Koidula BalticKlint EEK 500 Carl Robert Jakobson A barn swallow flying over a landscape...
park is 5 ha. The protected area was founded in 2005 to protect BalticKlint, its klint forests (Estonian: pangamets) and theirs biodiversity. "Naage maastikukaitseala"...
is associated with the North Estonian Klint (itself a subsection of the BalticKlint). A separate relic klint island, Toompea lies about 1.5 km northwest...
Martsa Village The BalticKlint in Martsa. Martsa Location in Estonia Coordinates: 59°25′52″N 27°27′27″E / 59.43111°N 27.45750°E / 59.43111; 27.45750...