Sardinia is the second-largest island in the Mediterranean Sea (after Sicily and before Cyprus), with an area of 24,100 square kilometres. It is situated between 38° 51′ and 41° 18′ latitude north (respectively Isola del Toro and Isola La Presa) and 8° 8′ and 9° 50′ east longitude (respectively Capo dell’Argentiera and Capo Comino). To the west of Sardinia is the Sea of Sardinia, a unit of the Mediterranean Sea; to Sardinia’s east is the Tyrrhenian Sea, which is also an element of the Mediterranean Sea.[12]Lake Omodeo, the largest reservoir in Italy
The nearest land masses are (clockwise from north) the island of Corsica, the Italian Peninsula, Sicily, Tunisia, the Balearic Islands, and Provence. The Tyrrhenian Sea portion of the Mediterranean Sea is directly to the east of Sardinia between the Sardinian east coast and the west coast of the Italian mainland peninsula. The Strait of Bonifacio is directly north of Sardinia and separates Sardinia from the French island of Corsica.
The coasts of Sardinia 1,849 kilometres long are generally high and rocky, with long, relatively straight stretches of coastline, many outstanding headlands, a few wide, deep bays, rias, many inlets and with various smaller islands off the coast.
The island has an ancient geoformation and, unlike Sicily and mainland Italy, is not earthquake-prone. Its rocks date in fact from the Palaeozoic Era (up to 500 million years old). Due to long erosion processes, the island’s highlands, formed of granite, schist, trachyte, basalt (called jaras or gollei), sandstone and dolomite limestone (called tonneri or “heels”), average at between 300 to 1,000 metres (984 to 3,281 feet). The highest peak is Punta La Marmora (Perdas Carpìas in Sardinian language)(1,834 m (6,017 ft)), part of the Gennargentu Ranges in the centre of the island. Other mountain chains are Monte Limbara (1,362 m (4,469 ft)) in the northeast, the Chain of Marghine and Goceano (1,259 m (4,131 ft)) running crosswise for 40 kilometres (25 miles) towards the north, the Monte Albo (1,057 m (3,468 ft)), the Sette Fratelli Range in the southeast, and the Sulcis Mountains and the Monte Linas (1,236 m (4,055 ft)). The island’s ranges and plateaux are separated by wide alluvial valleys and flatlands, the main ones being the Campidano in the southwest between Oristano and Cagliari and the Nurra in the northwest.
Sardinia has few major rivers, the largest being the Tirso, 151 km (94 mi) long, which flows into the Sea of Sardinia, the Coghinas (115 km) and the Flumendosa (127 km). There are 54 artificial lakes and dams that supply water and electricity. The main ones are Lake Omodeo and Lake Coghinas. The only natural freshwater lake is Lago di Baratz. A number of large, shallow, salt-water lagoons and pools are located along the 1,850 km (1,150 mi) of the coastline.
Lauterbrunnen lies at the bottom of a U-shaped valley that extends south and then south-westwards from the village to meet the 8 kilometers Lauterbrunnen Wall. The Lauterbrunnen Valley (Lauterbrunnental) is one of the deepest in the Alpine chain when compared with the height of the mountains that rise directly on either side. It is a true cleft, rarely more than one kilometre in width, between limestones precipices, sometimes quite perpendicular, everywhere of extreme steepness. It is to this form of the valley that it owes the numerous waterfalls from which it derives its name. The streams descending from the adjoining mountains, on reaching the verge of the rocky walls of the valley, form cascades so high that they are almost lost in spray before they reach the level of the valley. The most famous of these are the Staubbach Fall within less than one kilometres of the village of Lauterbrunnen. The height of the cascade is between 240 and 270 m, one of the highest in Europe formed of a single unbroken fall.
The river Weisse Lütschine flows through Lauterbrunnen and overflows its banks about once a year. The source of the river comes from melting snow high in the mountains, thus making it a very pure and clean source of water. It is common practice in the camp sites to chill drinks in the water. Trummelbach Falls is 3 km (1.9 mi) from Lauterbrunnen, connected by bus from the station.
The municipality of Lauterbrunnen extends a considerable distance beyond the village and valley, with an area of 164.51 km2. It reaches as far as the peaks of the Eiger, Mönch and Jungfrau to the east, the Gletscherhorn, Mittaghorn, Grosshorn, Breithorn and Tschingelhorn to the south, and the Gspaltenhorn and Schilthorn to the west. The Kleine Scheidegg Pass crosses over to Grindelwald to the east, whilst the Sefinenfurgge Pass crosses to Griesalp and Reichenbach im Kandertal to the west; both passes carry hiking trails that form part of the Alpine Pass Route, a long-distance hiking trail across Switzerland between Sargans and Montreux. Besides the village of Lauterbrunnen, the municipality also includes the villages of Wengen, Mürren, Gimmelwald, Stechelberg, and Isenfluh.
The preservation of historic buildings is a one-way street. There is no chance to renovate or to save a historic site once it’s gone. And we can never be certain what will be valued in the future. This reality brings to light the importance of locating and saving buildings of historic significance―because once a piece of history is destroyed, it is lost forever.
Snow makes whiteness where it falls,
The bushes look like popcorn balls.
The places where I always play,
Look like somewhere else today.
The Black Forest stretches from the High Rhine in the south to the Kraichgau in the north. In the west it is bounded by the Upper Rhine Plain (which, from a natural region perspective, also includes the low chain of foothills); in the east it transitions to the Gäu, Baar and hill country west of the Klettgau. The Black Forest is the highest part of the South German Scarplands and much of it is densely wooded, a fragment of the Hercynian Forest of Antiquity. It lies upon rocks of the crystalline basement and Bunter Sandstone, and its natural boundary with the surrounding landscapes is formed by the emergence of muschelkalk, which is absent from the Black Forest bedrock. Thanks to the fertility of the soil which is dependent on the underlying rock, this line is both a vegetation boundary as well as the border between the Altsiedelland (“old settlement land”) and the Black Forest, which was not permanently settled until the High Middle Ages. From north to south the Black Forest extends for over 160 km, attaining a width of up to 50 kilometres in the south, and up to 30 kilometres in the north. Tectonically the range forms a lifted fault block, which rises prominently in the west from the Upper Rhine Plain, whilst seen from the east it has the appearance of a heavily forested plateau.
“It was, as I have said, a fine autumnal day; the sky was clear and serene, and nature wore that rich and golden livery which we always associate with the idea of abundance. The forests had put on their sober brown and yellow, while some trees of the tendered kind had been nipped by the frosts into brilliant dyes of orange, purple, and scarlet.” ― Washington Irving
“Clouds of insects danced and buzzed in the golden autumn light, and the air was full of the piping of the song-birds. Long, glinting dragonflies shot across the path, or hung tremulous with gauzy wings and gleaming bodies.” ― Sir Arthur Conan Doyle