Kalmit (Haardt)
The Kalmit is the highest peak in the Palatinate Forest and the second highest (after the Donnersberg) in the Palatinate region of Germany. It is and located south of the town of Neustadt an der Weinstraße. The mountain attracts many tourists thanks to the numerous footpaths leading to its summit, its mountaintop restaurant, extensive views over the Palatinate wine region and striking rock formations on its forest-clad mountainsides. Geography Location The mountain lies within the municipal forest of the wine village of Maikammer and southwest of the independent town of Neustadt an der Weinstraße. Several lower peaks are grouped around the main summit, including the Zwergberg (589.3 m) to the north, the Taubenkopf (603.8 m) to the northeast, the Kanzel (531.7 m) and the Wetterkreuzberg (400.7 m) to the southeast, the Breitenberg (545.2 m) to the south and the Hüttenberg (591.2 m) to the southwest. On the Hüttenberg ridge there is a ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Kleine Kalmit
The Kleine Kalmit ("Little Kalmit"; from Lat. ''calvus mons'' = ''bare hill'') is a hill, high, just outside the eastern edge of the Palatine Forest, and the Haardt range, in the German state of Rhineland-Palatinate. Parts of the hill have been designated as a Nature reserve bearing the same name. Geography The Kleine Kalmit lies about 15 km south of its namesake, the 672.6 m high Kalmit, and about 6 km southwest of Landau outside the Haardt itself. Most of the hill, including its symbol, the little chapel on the summit dome which is visible for many miles, lies on the territory of the parish of Arzheim in the borough of Landau. Its south and southwest sides, with their vineyards, belong to the municipality of Ilbesheim. This latter area includes the only place in the Palatinate where saffron is grown. Flora and fauna The Kleine Kalmit is a botanical jewel with a rich community of the rare pasque flower and is designated as a Nature reserve. Its species-ric ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Black Forest
The Black Forest (german: Schwarzwald ) is a large forested mountain range in the state of Baden-Württemberg in southwest Germany, bounded by the Rhine Valley to the west and south and close to the borders with France and Switzerland. It is the source of the Danube and Neckar rivers. Its highest peak is the Feldberg with an elevation of above sea level. Roughly oblong in shape, with a length of and breadth of up to , it has an area of about 6,009 km2 (2,320 sq mi). Historically, the area was known for forestry and the mining of ore deposits, but tourism has now become the primary industry, accounting for around 300,000 jobs. There are several ruined military fortifications dating back to the 17th century. History In ancient times, the Black Forest was known as , after the Celtic deity, Abnoba. In Roman times (Late antiquity), it was given the name ("Marcynian Forest", from the Germanic word ''marka'' = "border"). The Black Forest probably represented the bo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Odenwald
The Odenwald () is a low mountain range in the German states of Hesse, Bavaria and Baden-Württemberg. Location The Odenwald is located between the Upper Rhine Plain with the Bergstraße and the ''Hessisches Ried'' (the northeastern section of the Rhine rift) to the west, the Main and the Bauland (a mostly unwooded area with good soils) to the east, the Hanau-Seligenstadt Basin – a subbasin of the Upper Rhine Rift Valley in the Rhine-Main Lowlands – to the north and the Kraichgau to the south. The part south of the Neckar valley is sometimes called the ''Kleiner Odenwald'' ("Little Odenwald"). The northern and western Odenwald belong to southern Hesse, with the south stretching into Baden. In the northeast, a small part lies in Lower Franconia in Bavaria. Geology The Odenwald, along with other parts of the Central German Uplands, belongs to the Variscan, which more than 300 million years ago in the Carboniferous period ran through great parts of Europe. The cause ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Taunus
The Taunus is a mountain range in Hesse, Germany, located north of Frankfurt. The tallest peak in the range is ''Großer Feldberg'' at 878 m; other notable peaks are ''Kleiner Feldberg'' (825 m) and ''Altkönig'' (798 m). The Taunus range spans the districts of Hochtaunuskreis, Main-Taunus-Kreis, Rheingau-Taunus, Limburg-Weilburg, and Rhein-Lahn. The range is known for its geothermal springs and mineral waters that formerly attracted members of the European aristocracy to its spa towns. The car line Ford Taunus is named after it. Description It is a relatively low range, with smooth, rounded mountains covered with forest. The Taunus is bounded by the valleys of the Rhine, Main, and Lahn rivers and it is part of the Rhenish Slate Mountains. On the opposite side of the Rhine, The Taunus range is continued by the Hunsrück. For geographical, ecological and geological purposes the Taunus is divided in three parts: *Anterior Taunus ''(Vortaunus'' or ''Vordertaunus)'' in the south, ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Hunsrück
The Hunsrück () is a long, triangular, pronounced upland in Rhineland-Palatinate, Germany. It is bounded by the valleys of the Moselle-Saar (north-to-west), the Nahe (south), and the Rhine (east). It is continued by the Taunus mountains, past the Rhine and by the Eifel past the Moselle. To the south of the Nahe is a lower, hilly country forming the near bulk of the Palatinate region and all of the, smaller, Saarland. Below its north-east corner is Koblenz. As the Hunsrück proceeds east it acquires north-south width and three notable gaps in its southern ridges. In this zone are multi-branch headwaters including the Simmerbach ending at Simmertal on the southern edge. This interior is therefore rarely higher than above sea level. Peaks and escarpments are principally: the (Black Forest) Hochwald, the Idar Forest, the Soonwald, and the Bingen Forest. The highest mountain is the Erbeskopf (816 m; 2,677 ft), towards the region's south-west. Notable towns are Simmern, ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Vosges
The Vosges ( , ; german: Vogesen ; Franconian and gsw, Vogese) are a range of low mountains in Eastern France, near its border with Germany. Together with the Palatine Forest to the north on the German side of the border, they form a single geomorphological unit and low mountain range of around in area. It runs in a north-northeast direction from the Burgundian Gate (the Belfort–Ronchamp– Lure line) to the Börrstadt Basin (the Winnweiler– Börrstadt–Göllheim line), and forms the western boundary of the Upper Rhine Plain. The Grand Ballon is the highest peak at , followed by the Storkenkopf (), and the Hohneck ().IGN maps available oGéoportail/ref> Geography Geographically, the Vosges Mountains are wholly in France, far above the Col de Saverne separating them from the Palatinate Forest in Germany. The latter area logically continues the same Vosges geologic structure but traditionally receives this different name for historical and political reasons. From ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Radio Tower
Radio masts and towers are typically tall structures designed to support antennas for telecommunications and broadcasting, including television. There are two main types: guyed and self-supporting structures. They are among the tallest human-made structures. Masts are often named after the broadcasting organizations that originally built them or currently use them. In the case of a mast radiator or radiating tower, the whole mast or tower is itself the transmitting antenna. Terminology The terms "mast" and "tower" are often used interchangeably. However, in structural engineering terms, a tower is a self-supporting or cantilevered structure, while a mast is held up by stays or guys. Broadcast engineers in the UK use the same terminology. A mast is a ground-based or rooftop structure that supports antennas at a height where they can satisfactorily send or receive radio waves. Typical masts are of steel lattice or tubular steel construction. Masts themselves play no part in t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Weather Station
A weather station is a facility, either on land or sea, with instruments and equipment for measuring atmospheric conditions to provide information for weather forecasts and to study the weather and climate. The measurements taken include temperature, atmospheric pressure, humidity, wind speed, wind direction, and precipitation amounts. Wind measurements are taken with as few other obstructions as possible, while temperature and humidity measurements are kept free from direct solar radiation, or insolation. Manual observations are taken at least once daily, while automated measurements are taken at least once an hour. Weather conditions out at sea are taken by ships and buoys, which measure slightly different meteorological quantities such as sea surface temperature (SST), wave height, and wave period. Drifting weather buoys outnumber their moored versions by a significant amount. Weather instruments Typical weather stations have the following instruments: * Thermometer for ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Palatine Forest Club
The Palatine Forest Club (german: Pfälzerwald-Verein) is a hiking club in the former Bavarian Palatinate, i.e. the southern part of the German state of Rhineland-Palatinate and the Saarland county of Saarpfalz-Kreis. In 2011 it had 221 local branches with around 27,000 members.Mitgliederzeitschrift „Pfälzerwald“, 2 The first branch was founded on 27 November 1902 in Ludwigshafen. Its first chairman was the industrialist, Anton Fasig. After other branches had formed the following year, the umbrella organization was founded in 1903. One of the founding members of the Palatine Forest Club, formed at the initiative of Ludwigshafen railway official, Otto Link, was the Palatine artist, Heinrich Strieffler. Karl Albrecht von Ritter was elected by the founding members as the managing director (Regierungsdirektor). Since 1908 the club has commemorated places of historical or natural significance by erecting and maintained a total of 306 so-called Ritter Stones ('' Ritterstei ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Kalmithaus
The Kalmithaus, also called the Ludwigshafener Hut, near Maikammer in the Rhineland-Palatinate county of Südliche Weinstraße is a refuge hut in the Palatinate Forest run by the Ludwigshafen-Mannheim branch of the Palatinate Forest Club. It is located in the southern part of the Haardt mountains at the summit of its highest peak, the Kalmit (), and is thus the highest hut in the Palatinate Forest. From its terrace there is "a splendid view of the Upper Rhine Plain and German Wine Road as far as the foothills of the southern Odenwald and northern Black Forest. at pfalz-info.com. Retrieved 3 September 2022. Immediately next to the hut is the [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Upper Rhine Plain
The Upper Rhine Plain, Rhine Rift Valley or Upper Rhine Graben (German: ''Oberrheinische Tiefebene'', ''Oberrheinisches Tiefland'' or ''Oberrheingraben'', French: ''Vallée du Rhin'') is a major rift, about and on average , between Basel in the south and the cities of Frankfurt/Wiesbaden in the north. Its southern section straddles the France–Germany border. It forms part of the European Cenozoic Rift System, which extends across Central Europe. The Upper Rhine Graben formed during the Oligocene, as a response to the evolution of the Alps to the south. It remains active to the present day. Today, the Rhine Rift Valley forms a downfaulted trough through which the river Rhine flows. Formation The Upper Rhine Plain was formed during the Early Cenozoic era, during the Late Eocene epoch. At this time, the Alpine Orogeny, the major mountain building event that was to produce the Alps, was in its early stages. The Alps were formed because the continents of Europe and Africa colli ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |