|
Mainz Sand Dunes
The Mainz Sand Dunes (german: Großer Sand) are a small geological and botanical supra-region and important nature preserve in Mainz, Germany. Within this protected area rare plants and animals can be found. Some of the species represented here, such as the Purple Golden-drop, (''Onosma arenaria'') grow only here and in small numbers. The sand dunes developed after the last ice age (Würm glaciation) and the first resettlement of grassland plants occurred approximately 12,000 years ago. The dry sandy soils are poor of nutrients but relict flora from the glaciation grasslands grow favorably. These plants are found otherwise only in southeast-European, inner-Asiatic (Pontic Steppe) areas and in the Mediterranean respectively. The effective surface of the protected landscape is rather small at 1.27 square kilometers. The Sand Dunes can be found between the suburbs Gonsenheim and Mombach and stretches up to the floodplains beginning in Mombach. Bordering the dunes is the Lennebergwald ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mainz Sand Dunes
The Mainz Sand Dunes (german: Großer Sand) are a small geological and botanical supra-region and important nature preserve in Mainz, Germany. Within this protected area rare plants and animals can be found. Some of the species represented here, such as the Purple Golden-drop, (''Onosma arenaria'') grow only here and in small numbers. The sand dunes developed after the last ice age (Würm glaciation) and the first resettlement of grassland plants occurred approximately 12,000 years ago. The dry sandy soils are poor of nutrients but relict flora from the glaciation grasslands grow favorably. These plants are found otherwise only in southeast-European, inner-Asiatic (Pontic Steppe) areas and in the Mediterranean respectively. The effective surface of the protected landscape is rather small at 1.27 square kilometers. The Sand Dunes can be found between the suburbs Gonsenheim and Mombach and stretches up to the floodplains beginning in Mombach. Bordering the dunes is the Lennebergwald ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mainz
Mainz () is the capital and largest city of Rhineland-Palatinate, Germany. Mainz is on the left bank of the Rhine, opposite to the place that the Main (river), Main joins the Rhine. Downstream of the confluence, the Rhine flows to the north-west, with Mainz on the left bank, and Wiesbaden, the capital of the neighbouring state Hesse, on the right bank. Mainz is an independent city with a population of 218,578 (as of 2019) and forms part of the Frankfurt Rhine-Main, Frankfurt Rhine-Main Metropolitan Region. Mainz was founded by the Roman Empire, Romans in the 1st century BC as a military fortress on the northernmost frontier of the empire and provincial capital of Germania Superior. Mainz became an important city in the 8th century AD as part of the Holy Roman Empire, capital of the Electorate of Mainz and seat of the Elector of Mainz, Archbishop-Elector of Mainz, the Primate (bishop), Primate of Germany. Mainz is famous as the birthplace of Johannes Gutenberg, the inventor of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Floodplain
A floodplain or flood plain or bottomlands is an area of land adjacent to a river which stretches from the banks of its channel to the base of the enclosing valley walls, and which experiences flooding during periods of high discharge.Goudie, A. S., 2004, ''Encyclopedia of Geomorphology'', vol. 1. Routledge, New York. The soils usually consist of clays, silts, sands, and gravels deposited during floods. Because the regular flooding of floodplains can deposit nutrients and water, floodplains frequently have high soil fertility; some important agricultural regions, such as the Mississippi river basin and the Nile, rely heavily on the flood plains. Agricultural regions as well as urban areas have developed near or on floodplains to take advantage of the rich soil and fresh water. However, the risk of flooding has led to increasing efforts to control flooding. Formation Most floodplains are formed by deposition on the inside of river meanders and by overbank flow. Whereve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Mainz
Geography (from Greek: , ''geographia''. Combination of Greek words ‘Geo’ (The Earth) and ‘Graphien’ (to describe), literally "earth description") is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of Earth. The first recorded use of the word γεωγραφία was as a title of a book by Greek scholar Eratosthenes (276–194 BC). Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be. While geography is specific to Earth, many concepts can be applied more broadly to other celestial bodies in the field of planetary science. One such concept, the first law of geography, proposed by Waldo Tobler, is "everything is related to everything else, but near things are more related than distant things." Geography has been called "the world discipline" and "the bridge between the human and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dunes Of Germany
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called ''ergs'' or ''sand seas''. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter ''slip face'' in the lee side. The valley or trough between dunes is called a ''dune slack''. Dunes are most common in desert environments, where the lack of moisture hinders the growth of vegetation that would otherwise interfere with the development of dunes. However, sand deposits are not restricted to deserts, and dunes are also found along sea shores, along streams in semiarid climates, in areas of glacial outwash, and in other areas where poorly cemented sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhine
), Surselva, Graubünden, Switzerland , source1_coordinates= , source1_elevation = , source2 = Rein Posteriur/Hinterrhein , source2_location = Paradies Glacier, Graubünden, Switzerland , source2_coordinates= , source2_elevation = , source_confluence = Reichenau , source_confluence_location = Tamins, Graubünden, Switzerland , source_confluence_coordinates= , source_confluence_elevation = , mouth = North Sea , mouth_location = Netherlands , mouth_coordinates = , mouth_elevation = , progression = , river_system = , basin_size = , tributaries_left = , tributaries_right = , custom_label = , custom_data = , extra = The Rhine ; french: Rhin ; nl, Rijn ; wa, Rén ; li, Rien; rm, label= Sursilvan, Rein, rm, label= Sutsilvan and Surmiran, Ragn, rm, label=Rumantsch Grischun, Vallader and Puter, Rain; it, Reno ; gsw, Rhi(n), inclu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rheinhessen
Rhenish Hesse or Rhine HesseDickinson, Robert E (1964). ''Germany: A regional and economic geography'' (2nd ed.). London: Methuen, p. 542. . (german: Rheinhessen) is a region and a former government district () in the German state of Rhineland-Palatinate. It is made up of territories west of the Upper Rhine river that were part of the Grand Duchy of Hesse and its successor in the Weimar Republic, the People's State of Hesse from 1816 to 1945. The hilly countryside is largely devoted to vineyards, comprising the Rheinhessen wine region. Geography Rhine Hesse stretches from the Upper Rhine Plain on the west bank of the Rhine up to the Nahe and Alsenz rivers in the west and down to the mouth of the Isenach in the south. The region borders on the Rhineland in the northwest, on the Palatinate in the southwest, and on South Hesse beyond the Rhine. The Rhenish-Hessian Hills along the Selz river, also called the "land of the thousand hills", reach up to at the summit of the Kapp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lennebergwald
The Lennebergwald is a forest in the north of Rheinhessen in Rhineland-Palatinate in Germany. The approximately 700 ha sized stretches north-west of Mainz between the urban districts of Mombach, Gonsenheim, Finthen and the municipalities of Budenheim and Heidesheim am Rhein in the district of Mainz-Bingen. Most of the area belongs to Budenheim. Characteristic of the Lennebergwald is its dry and sandy soil, resulting in a high ground temperature during summer days. Due to this primarily pine and oak trees as well as dry and calcareous grassland are growing here like in the neighbouring Mainz Sand Dunes. The climate is temperate and semi-arid to semi-humid. Considering the aspect of ecology, the Lenneberg forest has a high importance as a recreation area for people performing general fitness training such as jogging, nordic walking, mountainbiking as well as for people strolling around the wooded area. Within the Lennebergwald some cultural heritage monuments of Budenheim, such ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mombach
Mombach, with 13,875 inhabitants (Apr. 2021), is a borough in the northwest corner of Mainz, Germany. Mombach can be reached via Mainz-innenstadt (downtown) or Bundesautobahn 643. Location Mombach is located on the southern (left) bank of the river Rhine, flowing from east to west after converging with the Main. The Rhine is the northern border. Mombach lies in the Mainz basin below the Rheinhessen Plateau. Climate Like Rheinhessen, Mombach is protected by Hunsrück, Taunus, Odenwald and Donnersberg. The average yearly temperature of Mombach is 11.5 degrees Celsius (53 °F). The annual rainfall is below 500 liters per square meter (19.7 in) and comes near to a semi-arid to mediterranean climate. There are around 1,665 hours of sunshine per year. History In 2006 Mombach celebrated its 750-year jubilee. Mombach had been originally a location of farmers, mariners and fishermen. Prehistory to Middle Ages Archeological excavations prove that the site of Mombach ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Onosma
''Onosma'' is a genus of flowering plants in the family Boraginaceae. They are native to the Mediterranean and western Asia. They grow in dry, sunny habitats with rocky, sandy substrates.Koyuncu, O., et al. (2013)A new ''Onosma'' (Boraginaceae) species from central Anatolia, Turkey.''Plant Syst Evol'' Some are popular as rock garden plants.Hammerton, John Alexander (1920). ''Harmsworth's Household Encyclopedia''. Harmsworth Encyclopedias. Estimates of the number of species in the genus range from about 85''Onosma''. Flora of Pakistan. or 88Aytaç, Z., and Z. Türkmen. (2011) A new ''Onosma'' L.(Borag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gonsenheim
Gonsenheim is a borough in the northwest corner of Mainz, Germany. With about 25,000 inhabitants, it is the second-most populated borough of Mainz, before Oberstadt and after Neustadt. History Protohistory The history of Gonsenheim reaches back to the Neolithic Era, the Chalcolithic Europe (2800 to 2400 B.C.). Finds of prehistoric people in Gonsenheim can be dated back to the late Neolithic period (2800 BC to 2200 BC). The Beilde pot find in the Gewann Auf dem Kästrich (today: "An der Ochsenwiese") near the Gonsenheim railway station is probably of supra-regional significance for Gonsenheim's prehistory. Here, in 1850, five polished flat Jadeite axes were found in the sand dunes typical of Gonsenheim, which can be assigned to the Late Neolithic period. These axes were of high material value at that time and were probably imported from the Maritime Alps. From the time of the hill grave culture (1600-1300/1200 BC) there are some grave finds from hill graves in Gonsenheim; the set ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
