This lost continent off the coast of Scotland disappeared beneath the ocean 55 million years ago. The Mysterious Dancing Forest of Kaliningrad. Located on the thin Curonian Spit that splits the Curonian Lagoon from the Baltic Sea, lies one of the strangest natural phenomena on Earth. Known as the Dancing Forest by caretakers of Curonian Spit National Park and as the Drunken Forest, by locals, this unusual pine forest is made of trees of various shapes, most of them twisted in circles and spirals, along the ground. According to tourists, the Dancing Forest looks more like a site near Chernobyl, with 20-year-old pines tied into natural knots and loops, like lumpy contortionists.
A few years ago, the park manager invited students from local universities to conduct studies, and get to the bottom of the mystery. Since then, several theories emerged, including one suggested by a psychic who said the forest is located on a spot where massive amounts of positive and negative energies collide. Whatever the reason, the Dancing Forest of Kaliningrad is definitely an interesting site, especially if you’re into strange natural phenomena. How_to_forecast_weather.jpg (JPEG Image, 1208×2579 pixels) HEALTH PROFILE LITHUANIA. The Postnational Monitor. The Mysterious Moeraki Boulders. If you go down to Koekohe beach in New Zealand you can be sure of a big surprise.
In front of you, scattered like enormous marbles from some long abandoned game between giants, are hundreds of giant spherical rocks. Or are they the egg shells of sea-born dragons? The Moeraki boulders present us with a mystery – what are they and how on earth did they get there? Some are isolated but may occur in clusters. That they are here is the result of three things – erosion, concretion and time. First the waves, inexorable and patient, have pounded the local bedrock for countless millennia. Many of the Moeraki boulders give the impression of being completely spherical – and they almost are.
They do, however, tend to form early on in the history of the deposited sediment – it is thought they occur before the rest hardens in to rock. What is significant about these concretions is their size. The material responsible for their concretion is a carbonate mineral called calcite.