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Keila Waterfall

Keila Waterfall, October 2023
Keila Waterfall, October 2023. / Gatis Pāvils, CC BY-SA 4.0

WorldBlue  In short

The most beautiful of the three major waterfalls in Estonia is Keila Waterfall. It is some 60-70 m wide and 6.1 m high.

4.1 out of 10 stars 40.5%

GPS coordinates
59.3955 N 24.295 E
Location, address
Europe, Estonia, Harjumaa, Lääne-Harju vald, on Keila River in Keila-Joa
Name in Estonian
Keila juga
Stream
Keila River (Keila jõgi)
Height
6.1 m
Drops
1
Width
60 – 70 m
Flow rate
1.32 – 49 m3/s (1.)

Map of the site

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WorldYellow In detail

Possibly, the most beautiful waterfall in Estonia

Keila Waterfall, May 2016
Keila Waterfall, May 2016./ Aleksandr Abrosimov, Wikimedia Commons / CC BY-SA 4.0

Keila Waterfall is one of the three largest waterfalls in Estonia next to Jagala Waterfall and Narva Waterfall. Most visitors though agree that Keila Waterfall is more picturesque than the two others.

To a large extent the beauty of landmarks depends on the vantage point – and in this respect, Keila Waterfall excels. The waterfall is located in an ancient park of the nearby manor, with trails on both sides of it. An especially beautiful sight opens from a hill on the left bank of the river (see the first image).

Geology of Keila Waterfall

Keila Waterfall
Keila Waterfall./ Zairon, Wikimedia Commons / CC BY-SA 4.0

Waterfall, most likely, started to form when Ancylus Lake (a former stage of the Baltic Sea after the end of the last ice age) started to retreat and this part of Estonia became a land. Then (some 7-9 thousand years ago) the Keila River started to fall over the Baltic Klint – a very long escarpment across the northern part of Estonia.

As Keila River is rather powerful, it washed out the sturdy limestone cliff and Keila Waterfall recedes upwards, against the current. The medium speed of this retreat is some 9.7 m every century (1.).

Keila Waterfall is a fine location to see several formations of the Ordovician sediments that were deposited more than 450 million years ago.

In the upper part of the falls is exposed a 0.6 m thick layer of Ordovician limestone of Kunda Stage. Then, below follows some 2 m thick layer of limestone of Volkhov Stage, then: a 2.5 m thick, softer glauconitic limestone of Volkhov or Billingen Stage. Next is some 0.7 m thick layer of glauconitic clay of Varangu Stage and the last visible is up to 2 m thick layer of dictyonema limestone. This last layer is exposed in the underwater pit, which is up to 2 m deep. This pit, most likely, was carved in the sturdy rock during the ice age by some powerful subglacial streams.

History

Already in 1555 it has been mentioned that a watermill exists on the waterfall. The currently visible watermill building on the right bank of the river was built in 1831-1833. In 1928 it was adjusted for the electricity production, but in 2005 the watermill was restored to its historical exterior from the early 20th century.

Further below the stream on the right bank is a beautiful manor house. This is the Keila-Joa manor house (Schloss Fall), the first Gothic Revival style structure in Estonia that was constructed in 1831-1833.

References

  1. Loodusmälestised. Loode-Eesti. Teaduste Akadeemia Kirjastus, 2010.

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