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Mikulov Highlands
The Mikulov Highlands ( cs, Mikulovská vrchovina) is a mountain range in the South Moravian Region of the Czech Republic. The Highlands, together with the Waschberg Zone and Lower Austria Inselberg threshold, form the South-Moravian Carpathians. Geography The Mikulov Highlands rise to the south of the Thaya between Nový Přerov, the Nové Mlýny reservoirs, Bulhary, Mikulov, and the Austrian border. The Highlands have an area of and an average height of . The highest peak is Děvín at ; other peaks are ''Obora'' (), ''Stolova hora'' (), ''Pálava'' (), ''Stará hora'' (), and ''Turold '' (). To the north is the Thaya River valley, the natural border with Lower Morava Valley. To the east is the mountainous region between the Thaya and Včelínek, also from the Lower Morava Valley. To the southeast is the March Field, and to the southwest a ridge in Austria in the Waschberg Zone which forms the western border of the Thaya valley. Geomorphological subunits form Pálava ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Děvín
Děvín (german: Mayden Berg) is a double peak mountain in the Pavlov municipality in the South Moravian Region of the Czech Republic. With an elevation of , it is the highest mountain of the Pavlov Hills within the Mikulov Highlands, and of the Pálava Protected Landscape Area. It is located right on trace where runs line of drainage divide of Upper Thaya drainage and Thaya/Morava mesodrainage. History The summit of Děvín has the remains of a huge Iron Age hill fort, while the ancient Amber Route runs neighbors of the mountains base, and all archaic roads in landscape, originally created by animals and later overtaken by humans. The area around base of the mountain is permanently settled longer than last 30,000 years. Since Cromagnos hunters, ower Celtic tribes settlement, Roman fortress, Great Moravia hillforts ( Strachotín and Děvín). Geology The entire Děvín massif consists mainly by Jurassic limestone, i.e. series of rocks generated during sedimentation. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Morava Valley
The Lower Morava Valley ( cs, Dolnomoravský úval, Jihomoravská pánev; sk, Dolnomoravský úval; german: Nieder March Talsenke) is a geomorphological formation (special type of valley) in the Czech Republic and Slovakia. It is formed by the depression in the Western Carpathians (Ždánice Forest, Kyjov Hills and Pálava Protected Landscape Area, Mikulov Hills) in the west and Bílé Karpaty and Chvojnice Hills in the east. The drainage to the Morava (river), Morava River of the Danube basin runs finally to the Black Sea. It includes low drainage divide, watershed Dyje-Morava in Lanžhot. Geography The Lower Morava Valley is a nordest part of Vienna Basin (Western Carpathians) and the corridor to Napajedla Gate, Upper Morava Valley, Moravian Gate and later in final goal North European Plain (Poland- Lower Silesia – Galicia (Eastern Europe), Galicia) since ancient times. Here ran one arm of the most important trade routes from southern Europe to the Baltic Sea (e.g. the Amb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of The Western Carpathians
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of The Czech Republic
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Biosphere Reserve
A nature reserve (also known as a wildlife refuge, wildlife sanctuary, biosphere reserve or bioreserve, natural or nature preserve, or nature conservation area) is a protected area of importance for flora, fauna, or features of geological or other special interest, which is reserved and managed for purposes of conservation and to provide special opportunities for study or research. They may be designated by government institutions in some countries, or by private landowners, such as charities and research institutions. Nature reserves fall into different IUCN categories depending on the level of protection afforded by local laws. Normally it is more strictly protected than a nature park. Various jurisdictions may use other terminology, such as ecological protection area or private protected area in legislation and in official titles of the reserves. History Cultural practices that roughly equate to the establishment and maintenance of reserved areas for animals date back t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
World Heritage Site
A World Heritage Site is a landmark or area with legal protection by an international convention administered by the United Nations Educational, Scientific and Cultural Organization (UNESCO). World Heritage Sites are designated by UNESCO for having cultural, historical, scientific or other form of significance. The sites are judged to contain " cultural and natural heritage around the world considered to be of outstanding value to humanity". To be selected, a World Heritage Site must be a somehow unique landmark which is geographically and historically identifiable and has special cultural or physical significance. For example, World Heritage Sites might be ancient ruins or historical structures, buildings, cities, deserts, forests, islands, lakes, monuments, mountains, or wilderness areas. A World Heritage Site may signify a remarkable accomplishment of humanity, and serve as evidence of our intellectual history on the planet, or it might be a place of great natural beauty. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mikulovská Wine
Mikulovská is one of four Czech wine regions within southern Moravia, Czech Republic. The Mikulovská wine region, containing 30 wine villages, is famed for producing white wines grown in the limestone soils, particularly in and around the area of the Pálava Landscape Protected Area.Wine of the Czech Republic, 'Viticulture of Bohemia and Moravia'', pg 10-11, Accessed: January 11th, 2011 Historically a centre of viticulture and winemaking in Moravia, Mikulovská is home to the historical town of Mikulov, and the Czech National Wine Centre (Czech: ''Národní Vinařské Centrum'') and Wine Salon of the Czech Republic, located at Valtice Castle. History In the 2nd Century CE, the Roman 10th Legion based at Vindobona built an extensive outpost near the Amber Road and the Pálava Hills in Mikulovská, near the present-day village of Pasohlávky. Around the year 278, the Roman Emperor Marcus Aurelius Probus annulled the edict of Emperor Domitian that had prohibited the planting o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vineyards
A vineyard (; also ) is a plantation of grape-bearing vines, grown mainly for winemaking, but also raisins, table grapes and non-alcoholic grape juice. The science, practice and study of vineyard production is known as viticulture. Vineyards are often characterised by their ''terroir'', a French term loosely translating as "a sense of place" that refers to the specific geographical and geological characteristics of grapevine plantations, which may be imparted to the wine itself. History The earliest evidence of wine production dates from between 6000 and 5000 BC. Wine making technology improved considerably with the ancient Greeks but it wasn't until the end of the Roman Empire that cultivation techniques as we know them were common throughout Europe. In medieval Europe the Church was a staunch supporter of wine, which was necessary for the celebration of the Mass. During the lengthy instability of the Middle Ages, the monasteries maintained and developed viticultural prac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geomorphology
Geomorphology (from Ancient Greek: , ', "earth"; , ', "form"; and , ', "study") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or near Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform and terrain history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphologists work within disciplines such as physical geography, geology, geodesy, engineering geology, archaeology, climatology, and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field. Overview Earth's surface is modified by a combination of surface processes that shape landscapes, and geologic processes that cause tectonic uplift and subsidence, and shape the coastal geography. Surface processes co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austria
Austria, , bar, Östareich officially the Republic of Austria, is a country in the southern part of Central Europe, lying in the Eastern Alps. It is a federation of nine states, one of which is the capital, Vienna, the most populous city and state. A landlocked country, Austria is bordered by Germany to the northwest, the Czech Republic to the north, Slovakia to the northeast, Hungary to the east, Slovenia and Italy to the south, and Switzerland and Liechtenstein to the west. The country occupies an area of and has a population of 9 million. Austria emerged from the remnants of the Eastern and Hungarian March at the end of the first millennium. Originally a margraviate of Bavaria, it developed into a duchy of the Holy Roman Empire in 1156 and was later made an archduchy in 1453. In the 16th century, Vienna began serving as the empire's administrative capital and Austria thus became the heartland of the Habsburg monarchy. After the dissolution of the H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
