At Klaipeda, the Curonian Bay begins. A remarkable peninsula, the Curonian Spit or Neringa, leads southwards along the coast, mile after mile. Behind the peninsula is a large lagoon, the sheltered Curonian Bay.The peninsula "locking in" the Curonian lagoon is also, particularly in the north at Klaipeda, a recreation area. There you will find a yacht club, some restaurants, an outdoor museum and on the Baltic sea side - the beaches. The whole split is built up by sand dunes. The inner parts are forested.
To sail here is a strange experience. The nature is very different to the western shores of the Baltic with it's skerries, islands and islets. This is rather a land of gigantic sand dunes!
Close to the fairway they dunes loom and in some places the reach 60 m high.The lagoon itself could be navigated by yachts. You can sail all the way down to Nida.
After a days run south from Klaipeda, close to the Russian border, you will arrive at your destination, the old health resort and fishing village Nida
The Sahara of LithuaniaThe people of the Curonian
spit (Kursiu spit) have won their fight against the shifting sands, but now
the battle is on to save the dunes themselves. The same dunes that swallowed 14
villages since their relentless advancement during the 18th and 19th centuries
are now in danger of disappearing into the Baltic Sea. A massive forestation
program in the middle of the last century pinned most of the territory of the
spit in place and provided a windbreak for the villages there, but the height of
the uninhabited littoral dunes near Nida is decreasing. Could this spectacular
natural treasure be lost in just a few centuries? In a poetic way, this is more or less true. Instead of a benevolent goddess, however, an underwater river of sand carried the materials to make the spit. The sand originated on the cliffs of the Sambian peninsula to the south and was carried northward by a deep sea current. Hills on the sea floor arrested the current, changed its course and forced it to leave some of its cargo behind. Thus the Kursiu spit grew, roughly north to south. It was the wind, however, not the waves, that
expanded the spit from west to east. When the sand first emerged from the sea,
the wind began its work, carrying the loose top layer of sand eastward and
shaping it into neat, even rows of parabolic dunes cutting the spit crosswise.
These are preserved today only near Juodkrante, but protective fences and
forests hide the unique shape. These first settlers lived off the sea and
considered the forest sacred, as if sensing that its shallow root system alone
formed a safety net securing the dunes and the ecosystem there. Foreign invaders
disrupted this existence, with attacks from the Vikings in the 8th century and
the Teutonic Order in the 13th century. With the advent of the crusaders, the
area gradually became Germanised and forestry supplemented the fishing industry.
As the forest was exploited for timber and tar, the spit reverted to its earlier
desert-like stage and the sands were on the move again. The drifting dunes took
their first village in the 16th century. In 1961 the towns of Juodkrante, Pervalka, Preila and Nida - were no longer on the run - but united into the municipality of Neringa. Most of the Lithuanian territory of the spit (from Kopgalis to Nida) was declared a national park in 1991, enacting protective restrictions on the activities permitted in the forests and on the dunes. But measures taken so far are for the most part passive: efforts are being made to inform the public of the perilous situation of the dunes, but little active research or restoration is being done. The unstoppable flow of holiday traffic that supports the area's economy is on the rise, and age-old habits - such as picking mushrooms and berries in the forests, even in restricted areas - die hard. As a result of traffic the Nida dunes, said to have once reached a height of 50m above the water, are decreasing with every year. As a testament to the fragile ecosystem of the spit, just note the oddly consistent tilt of the pine trees as you drive down the main road to Nida, caused by a persistent west wind and a shallow layer of topsoil (1cm in some places) on the loose sand. But the tenacious villages of Neringa themselves have survived and have set down deep roots in the area once known as "the Sahara of Lithuania". That name belongs only to history now. |