The Lower Morava Valley (; ; ) is a
geomorphological
Geomorphology () is the scientific study of the origin and evolution of topography, topographic and bathymetry, bathymetric features generated by physical, chemical or biological processes operating at or near Earth#Surface, Earth's surface. Ge ...
formation (special type of
valley
A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over ...
) in the
Czech Republic
The Czech Republic, also known as Czechia, and historically known as Bohemia, is a landlocked country in Central Europe. The country is bordered by Austria to the south, Germany to the west, Poland to the northeast, and Slovakia to the south ...
and
Slovakia
Slovakia, officially the Slovak Republic, is a landlocked country in Central Europe. It is bordered by Poland to the north, Ukraine to the east, Hungary to the south, Austria to the west, and the Czech Republic to the northwest. Slovakia's m ...
.
It is formed by the depression in the
Western Carpathians
The Western Carpathians () are a mountain range and geomorphological province that forms the western part of the Carpathian Mountains.
The mountain belt stretches from the Low Beskids range of the Eastern Carpathians along the border of Poland w ...
(
Ždánice Forest,
Kyjov Hills and
Mikulov Hills) in the west and
Bílé Karpaty and
Chvojnice Hills in the east. The drainage to the
Morava River of the
Danube basin runs finally to the
Black Sea
The Black Sea is a marginal sea, marginal Mediterranean sea (oceanography), mediterranean sea lying between Europe and Asia, east of the Balkans, south of the East European Plain, west of the Caucasus, and north of Anatolia. It is bound ...
.
It includes the low
watershed of the Dyje-Morava in
Lanžhot
Lanžhot () is a town in Břeclav District in the South Moravian Region of the Czech Republic. It has about 3,600 inhabitants. Located on the border with Austria and Slovakia, it is the southernmost Moravian town.
Etymology
The original Latin name ...
.
Geography
The Lower Morava Valley is a nordest part of the
Vienna Basin
The Vienna Basin (, , , Hungarian: ''Bécsi-medence'') is a geologically young tectonic burial basin and sedimentary basin in the seam area between the Alps, the Carpathians and the Pannonian Plain. Although it topographically separates the Al ...
(
Western Carpathians
The Western Carpathians () are a mountain range and geomorphological province that forms the western part of the Carpathian Mountains.
The mountain belt stretches from the Low Beskids range of the Eastern Carpathians along the border of Poland w ...
) and the corridor to
Napajedla Gate, Upper Morava Valley,
Moravian Gate
The Moravian Gate (, , , ) is a geomorphological feature in the Moravian region of the Czech Republic and the Upper Silesia region in Poland. It is formed by the depression between the Carpathian Mountains in the east and the Sudetes in the west. ...
and later in the final goal, the
North European Plain
The North European Plain ( – North German Plain; ; – Central European Plain; and ; French: ''Plaine d'Europe du Nord'') is a geomorphological region in Europe that covers all or parts of Belgium, the Netherlands (i.e. the Low Countries), ...
(
Poland
Poland, officially the Republic of Poland, is a country in Central Europe. It extends from the Baltic Sea in the north to the Sudetes and Carpathian Mountains in the south, bordered by Lithuania and Russia to the northeast, Belarus and Ukrai ...
-
Lower Silesia
Lower Silesia ( ; ; ; ; ; ; ; ) is a historical and geographical region mostly located in Poland with small portions in the Czech Republic and Germany. It is the western part of the region of Silesia. Its largest city is Wrocław.
The first ...
–
Galicia) since ancient times. Here ran one arm of the most important trade routes from southern Europe to the
Baltic Sea
The Baltic Sea is an arm of the Atlantic Ocean that is enclosed by the countries of Denmark, Estonia, Finland, Germany, Latvia, Lithuania, Poland, Russia, Sweden, and the North European Plain, North and Central European Plain regions. It is the ...
(e.g. the
Amber Road
The Amber Road was an ancient trade route for the transfer of amber from coastal areas of the North Sea and the Baltic Sea to the Mediterranean Sea. Prehistoric trade routes between Northern and Southern Europe were defined by the amber trade. ...
– eastern branch) and also routes from Moravia to
Upper Silesia
Upper Silesia ( ; ; ; ; Silesian German: ; ) is the southeastern part of the historical and geographical region of Silesia, located today mostly in Poland, with small parts in the Czech Republic. The area is predominantly known for its heav ...
and Lesser Poland. The
Emperor Ferdinand Northern Railway
The Emperor Ferdinand Northern Railway (; ; ) was a railway company during the time of the Austrian Empire. Its main line was intended to connect Vienna with the salt mines in Bochnia near Kraków. The name is still used today in referring to a ...
(one part) built in 1840–41 from
Břeclav
Břeclav (; ) is a town in the South Moravian Region of the Czech Republic. It has about 25,000 inhabitants. Located at the Czech-Austrian state border and near the Czech–Slovak state border, it is an important railway hub.
Administrative divis ...
(Vienna) to
Přerov
Přerov (; ) is a city in the Olomouc Region of the Czech Republic. It has about 41,000 inhabitants. It lies on the Bečva River. In the past it was a major crossroad in the heart of Moravia in the Czech Republic. The historic city centre is we ...
also traversed the Lower Morava Valley.
The
Morava and
Thaya
The Thaya (, ) is a river in the Czech Republic and Austria, a right tributary of the Morava (river), Morava River. It flows through the South Moravian Region in the Czech Republic and through Lower Austria in Austria. It is formed by the conflue ...
rivers,
Myjava (river),
Chvojnice,
Trkmanka,
Kyjovka as well among others, finish here in their
floodplain
A floodplain or flood plain or bottomlands is an area of land adjacent to a river. Floodplains stretch from the banks of a river channel to the base of the enclosing valley, and experience flooding during periods of high Discharge (hydrolog ...
s.
FIELD TRIP to the floodplain forests of the Lower Morava Biosphere Reserve
/ref>
The largest towns in Lower Morava Valley are Břeclav
Břeclav (; ) is a town in the South Moravian Region of the Czech Republic. It has about 25,000 inhabitants. Located at the Czech-Austrian state border and near the Czech–Slovak state border, it is an important railway hub.
Administrative divis ...
, Hodonín
Hodonín (; ) is a town in the South Moravian Region of the Czech Republic. It has about 24,000 inhabitants.
Geography
Hodonín is located about southeast of Brno, on the border with Slovakia. It lies in a flat landscape of the Lower Morava Va ...
, Uherské Hradiště
Uherské Hradiště (; ) is a town in the Zlín Region of the Czech Republic. It has about 25,000 inhabitants. The agglomeration with the two neighbouring towns of Staré Město (Uherské Hradiště District), Staré Město and Kunovice has over ...
, Staré Město, Dubňany, and Strážnice
Strážnice () is a town in Hodonín District in the South Moravian Region of the Czech Republic. It has about 5,300 inhabitants. The historic town centre is well preserved and is protected as an Cultural monument (Czech Republic)#Monument zones, u ...
.
Soil horizon
A soil horizon is a layer parallel to the soil surface whose physical, chemical and biological characteristics differ from the layers above and beneath. Horizons are defined in many cases by obvious physical features, mainly colour and texture. ...
– mainly sand
Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is usually defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural ...
, fluvisol and loess
A loess (, ; from ) is a clastic rock, clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loesses or similar deposition (geology), deposits.
A loess ...
, partly chernozem
Chernozem ( ),; also called black soil, regur soil or black cotton soil, is a black-colored soil containing a high percentage of humus (4% to 16%) and high percentages of phosphorus and ammonia compounds. Chernozem is very fertile soil and can ...
.
Gallery
Geomorfologické clenení Ceska.jpg, Lower Morava Valley (olive green) down right
Dyje-Morava confluence 01.jpg, Riparian forest
A riparian forest or riparian woodland is a forested or wooded area of land adjacent to a body of water such as a river, stream, pond, lake, marshland, estuary, canal, Sink (geography), sink, or reservoir. Due to the broad nature of the definitio ...
by the Morava–Thaya confluence
Morava hodonin holic.jpg, Lower Morava Valley landscape Hodonín surrounding
Náklo (vrch), altán.jpg, View from Náklo Hill (265 m) to the Lower Morava Valley landscape
A landscape is the visible features of an area of land, its landforms, and how they integrate with natural or human-made features, often considered in terms of their aesthetic appeal.''New Oxford American Dictionary''. A landscape includes th ...
Uherské Hradiště, archeologická lokalita Sady "Špitálky".jpg, View of the Lower Morava Valley from the Sady archaeological site
An archaeological site is a place (or group of physical sites) in which evidence of past activity is preserved (either prehistoric or recorded history, historic or contemporary), and which has been, or may be, investigated using the discipline ...
See also
* Vyškov Gate
*Outer Subcarpathia
Outer Subcarpathia (; ; ; ) denotes the depression area at the outer (western, northern and eastern) base of the Carpathian arc, including foothills of the Outer Western Carpathians and Outer Eastern Carpathians. It stretches from northeaste ...
* South-Moravian Carpathians
*Upper Morava Valley
The Upper Morava Valley () is a lowland and a geomorphological mesoregion of the Czech Republic. It is located in the Olomouc and Zlín regions. Its name is derived from the Morava river that forms the axis of the territory.
Geomorphology
The Up ...
*Dyje–Svratka Valley
The Dyje–Svratka Valley () is a valley and a geomorphological mesoregion of the Czech Republic. It is located in the South Moravian Region. Its name is derived from the rivers Thaya (Dyje) and Svratka.
Geomorphology
The Dyje–Svratka Valley ...
References
Further reading
*(1993)'' Geografický místopisný slovník'', Academia, Praha.
*(1997) Plašienka, D., Grecula, P., Putiš, M., Kováč, M. a Hovorka, D.,: Evolution and structure of the Western Carpathians
The Western Carpathians () are a mountain range and geomorphological province that forms the western part of the Carpathian Mountains.
The mountain belt stretches from the Low Beskids range of the Eastern Carpathians along the border of Poland w ...
: an overview. ''Mineralia Slovaca'' – Monograph, Košice, p. 1–24.
{{Authority control
Valleys of the Czech Republic
Western Carpathians
Moravia