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Parnu

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Pärnu 

(formerly Pernau or Pernov), a city under republic jurisdiction and administrative center of Pärnu Raion, Estonian SSR. Population, 49,000 (1974). Situated on the Pärnu River at the point where the river empties into the Gulf of Riga, Pärnu is a seaport and river landing. It has a railroad station 129 km south of Tallinn.

Pärnu is a seaside climatic and mud-bath health resort. Summers are moderately warm, with an average July temperature of 17°C, and winters are fairly mild, with an average January temperature of -5°C. Annual precipitation totals 540 mm. The city’s facilities offer climatotherapy and pelotherapy with sea mud for those suffering from diseases of the circulatory, musculoskeletal, and nervous systems, the digestive tract, and reproductive organs. The city has sanatoriums, a balneopelotherapy facility, and houses of rest. There is a sandy beach and a park.

Industry is represented by fish-canning and linen-textile combines and machine-building, food-processing, and lumber enterprises. This city has a dramatic theater, a museum of local lore, a memorial museum of the poet Lydia Koidula, and a tourist center.

Pärnu has been known since 1251. A settlement on the right bank of the Pärnu River, belonging to the see of Ösel-Wiek, was called Vana-Pärnu (Old Pärnu), while Uus-Pärnu (New Pärnu) was situated on the left bank and ruled by the Livonian Order. In the 14th century, Pärnu, which by then had become a major port, joined the Hanseatic League. From the 15th to early 18th centuries it was alternately dependent upon the Livonian Order, Poland, and Sweden. In 1599 the Poles razed the old city on the right bank. In 1710, during the Northern War (1700–21), Pärnu was captured by Russian troops and made part of Russia. In the 18th century it became a district capital of the Province of Livonia, and by the end of the 19th century it had become a famous health resort of the Baltic Region. From 1918 to 1940, Pärnu was part of bourgeois Estonia. In July 1940 it was occupied by fascist German invaders; it was liberated by the Soviet Army on Sept. 23, 1944.

REFERENCE

Grodinskii, F. M. Piarnu: Putevoditel’. Tallinn, 1974.


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It was here, close to the country's summer capital of Parnu - around 80 miles from Tallinn - that we encountered the bizarre spectacle of a line dancing festival in a field of mud.
The lowermost part of the section, the Rezekne and Parnu Fms, is mostly represented by weakly claycemented siliciclastic rocks, containing rare interlayers of dolostone and dolomitic marlstone.
The 50 mm precipitation threshold was exceeded in all hydrological and precipitation stations (where the entire 45-year period was measured) and in all meteorological stations, except the one in Parnu.
 
 
 
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