Средњоевропска низија — разлика између измена

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[[Image:Europe landforms - North European Plain.svg|thumb|right|300px|Средњоевропска низија је обојена зелено.]]
[[Датотека:Europe landforms - North European Plain.svg|thumb|right|300px|Средњоевропска низија је обојена зелено.]]
[[File:Europe topography map en.png|thumb|300px|Топографија Европе.]]
[[Датотека:Europe topography map en.png|thumb|300px|Топографија Европе.]]


'''Средњоевропска низија,''' '''Прибалтичка низија''' или '''Немачко-пољска низија''', је [[низија]] која се простире у дужини од око 600 -{km}- (и упола толико по ширини) и налази на северу [[Средња Европа|средње Европе]]. Она захвата северне делове [[Њемачка|Немачке]] и [[Пољска|Пољске]] (одатле јој и назив ''Немачко-пољска низија'')
'''Средњоевропска низија,''' '''Прибалтичка низија''' или '''Немачко-пољска низија''', је [[низија]] која се простире у дужини од око 600 -{km}- (и упола толико по ширини) и налази на северу [[Средња Европа|средње Европе]]. Она захвата северне делове [[Њемачка|Немачке]] и [[Пољска|Пољске]] (одатле јој и назив ''Немачко-пољска низија'')

It consists of the low [[plain]]s between the [[Hercynian Europe]]<ref>{{Cite journal|last=Martínez Catalán|first=José R.|date=2012-07-01|title=The Central Iberian arc, an orocline centered in the Iberian Massif and some implications for the Variscan belt|journal=International Journal of Earth Sciences|language=en|volume=101|issue=5|pages=1299–1314|doi=10.1007/s00531-011-0715-6|bibcode=2012IJEaS.101.1299M| s2cid=195334509 |issn=1437-3262}}</ref><ref>{{Cite journal|last1=Crespo-Blanc|first1=Ana|last2=Orozco|first2=Miguel|date=1991-10-01|title=The boundary between the Ossa-Morena and Southportuguese Zones (Southern Iberian Massif): Major suture in the European Hercynian Chain|journal=Geologische Rundschau|language=en|volume=80|issue=3|pages=691–702|doi=10.1007/BF01803695|bibcode=1991GeoRu..80..691C|s2cid=128688878|issn=1432-1149}}</ref><ref>{{Cite journal |url=https://pubs.er.usgs.gov/usgspubs/b/b1871 |title=Geology of petroleum and coal deposits in the North China Basin, Eastern China |last=Lee |first=K. Y. |journal=USGS Bulletin 1871 |year=1989 |postscript=. Table 1, p. 3. |access-date=2017-09-17 |archive-date=2019-09-13 |archive-url=https://web.archive.org/web/20190913035632/https://pubs.er.usgs.gov/publication/b1871 |url-status=dead }}</ref> ([[Central European Highlands]]<ref>{{Citation|last1=Pusch|first1=Martin|title=Chapter 14 - Rivers of the Central European Highlands and Plains|date=2009-01-01|url=https://www.sciencedirect.com/science/article/pii/B978012369449200014X|work=Rivers of Europe|pages=525–576|editor-last=Tockner|editor-first=Klement|place=London|publisher=Academic Press|language=en|doi=10.1016/b978-0-12-369449-2.00014-x|isbn=978-0-12-369449-2|access-date=2021-09-29|last2=Behrendt|first2=Horst|last3=Gancarczyk|first3=Aleksandra |last4=Kronvang|first4=Brian |last5=Sandin|first5=Leonard|last6=Stendera|first6=Sonja|last7=Wolter|first7=Christian|last8=Andersen|first8=Hans E.|last9=Fischer|first9=Helmut|s2cid=128731308 |editor2-last=Uehlinger|editor2-first=Urs|editor3-last=Robinson|editor3-first=Christopher T.}}</ref><ref>{{cite book |chapter-url=https://www.researchgate.net/publication/285992779 |doi=10.1016/B978-0-12-369449-2.00014-X |via=[[ResearchGate]]|chapter=Rivers of the Central European Highlands and Plains |title=Rivers of Europe |year=2009 |last1=Pusch |first1=Martin |last2=Behrendt |first2=Horst |last3=Gancarczyk |first3=Aleksandra |last4=Kronvang |first4=Brian |last5=Sandin |first5=Leonard |last6=Stendera |first6=Sonja |last7=Wolter |first7=Christian |last8=Andersen |first8=Hans E. |last9=Fischer |first9=Helmut |last10=Hoffmann |first10=Carl. C. |last11=Nowacki |first11=Franciszek |last12=Schöll |first12=Franz |last13=Svendsen |first13=Lars M. |last14=Bäthe |first14=Jürgen |last15=Friberg |first15=Nikolai |last16=Hachoł |first16=Justyna |last17=Pedersen |first17=Morten L. |last18=Scholten |first18=Matthias |last19=Wnuk-Gławdel |first19=Ewa |pages=525–576 |isbn=9780123694492 |s2cid=128731308 }}</ref><ref>{{Cite web|title=Central European highlands and their hydrological role, with special|url=https://studylib.net/doc/7578183/central-european-highlands-and-their-hydrological-role--w|access-date=2021-09-29|website=studylib.net|language=en}}</ref>) to the south and coastlines of the [[North Sea]] and the [[Baltic Sea]] to the north. These two seas are separated by the [[Jutland]] [[Peninsula]] (Denmark). The North European Plain is connected to the [[East European Plain]], together forming the majority of the [[Great European Plain]] (European Plain).

==Geography==
Elevations vary between 0 and 200 m (0 to about 650 ft). While mostly used as farmland, the region also contains [[bog]]s, [[heath (habitat)|heath]] and lakes.
The [[Wadden Sea]], a large [[tide|tidal]] area, is located on the [[North Sea]] coast.

A number of freshwater lagoons including the [[Szczecin Lagoon]],<ref>Gerald Schernewski, ''Baltic coastal ecosystems: structure, function, and coastal zone management'', Springer, 2002, p.79, {{ISBN|3-540-42937-9}}</ref><ref name=Schiewer115>Ulrich Schiewer, ''Ecology of Baltic coastal waters'', Springer, 2008, {{ISBN|3-540-73523-2}}</ref> the [[Vistula Lagoon]]<ref>{{Cite book|last=Górski|first=Karol|title=Związek Pruski i poddanie się Prus Polsce: zbiór tekstów źródłowych|year=1949|publisher=Instytut Zachodni|location=Poznań|language=pl|pages=51, 56}}</ref> and the [[Curonian Lagoon]]<ref>{{cite web|publisher=[[Encyclopædia Britannica]]|url=http://www.britannica.com/EBchecked/topic/140578/Curonian-Lagoon|title=Curonian Lagoon|accessdate=2009-10-17}}</ref><ref name=sus>{{cite book|title=Sustainable Use and Development of Watersheds|publisher=[[Springer Science+Business Media|Springer]]|author=I. Ethem Gönenç, Angheluta Vadineanu|url=https://books.google.com/books?id=s1SmQ5TYB6YC&q=Curonian+Lagoon+watershed&pg=PA404|year=2008 | isbn=978-1-4020-8557-4}}</ref> are found on the [[Baltic Sea]] coast.


== Одлике и рељеф ==
== Одлике и рељеф ==
Средњоевропска низија је широка од 150 -{km}- на [[запад]]у до више од 400 -{km}- на [[исток]]у, благо нагнута од средогорја према [[север]]у. На крајњем југу низије, на прелазу према средогорју, пространа су подручја прекривена [[прапор]]ом, према [[север]]у све је више слабије плодног [[Моренски материјал|моренског материјала]]. [[Глацијални процес|Морене]] су преобликоване у благо валовите платое између којих су влажније прадолине, обликоване токовима који су за леденог доба текли испод и рубом леденог покрова. Најсевернији део низије покривен је наносима, слабије се одводњава па се местимично јављају [[Мочвара|мочваре]], посебно у источном делу.
Средњоевропска низија је широка од 150 -{km}- на [[запад]]у до више од 400 -{km}- на [[исток]]у, благо нагнута од средогорја према [[север]]у. На крајњем југу низије, на прелазу према средогорју, пространа су подручја прекривена [[прапор]]ом, према [[север]]у све је више слабије плодног [[Моренски материјал|моренског материјала]]. [[Глацијални процес|Морене]] су преобликоване у благо валовите платое између којих су влажније прадолине, обликоване токовима који су за леденог доба текли испод и рубом леденог покрова. Најсевернији део низије покривен је наносима, слабије се одводњава па се местимично јављају [[Мочвара|мочваре]], посебно у источном делу.

==Location==
The North European Plain covers [[Flanders]] (northern Belgium and Northern France), the Netherlands, [[Northern Germany]], Denmark, and most of central-western Poland; it touches the Czech Republic and southwestern part of Sweden as well.

Parts of [[eastern England]] can also be considered part of the same plain; as they share its low-lying character and were connected by land to the continent during the [[Pleistocene|last ice age]]. The Northern European Plains are located also under the Baltic Sea.
==Rivers==
Major river-drainage basins include, from west to east: the
[[Rhine]], [[Ems (river)|Ems]], [[Weser]], [[Elbe]], [[Oder]] and [[Vistula]].

The bases of these rivers are heavy with thin soil, making it hard for the farming to thrive near these rivers.

==Sub-regions==
===Low Countries===
Historically, especially in the [[Middle Ages]] and [[Early modern period]], the western section has been known as the [[Low Countries]].

===North German Plain===
The [[North German Plain]] is located north of the [[Central Uplands]] of Germany.

===Polish Plain===
The part in modern-day Poland is called the "Polish Plain" ({{lang-pl|Niż Polski}} or ''Nizina Polska'') and stretches from the Baltic Sea in the north to the [[Sudetes]] and [[Carpathian Mountains|Carpathians]]

===English flatlands===
The extension of the plain into England consists mainly of the flatlands of [[East Anglia]], [[the Fens]] and [[Lincolnshire]], where the landscape is in parts strikingly similar to that of the [[Netherlands]].

== Референце ==
{{reflist|}}


== Литература ==
== Литература ==
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* {{cite book |url=https://books.google.com/books?id=9dx2AgAAQBAJ&q=%22a+higher+density+of+lakes+than+Poland%22 |title=Poland |publisher=ABDO Publishing |author=Christine Zuchora-Walske |year=2013 |page=28 |isbn=978-1-61480-877-0 |chapter=The Lakes Region |quote=''Insert:'' Poland is home to 9,300 lakes. Finland is the only European nation with a higher density of lakes than Poland.}}
* {{cite book |url=https://books.google.com/books?id=m8_rUrXWSsUC&q=Gop%C5%82o-Kruszwica+Popiel |title=Jewish Poland &ndash; legends of Origin: Ethnopoetics and Legendary Chronicles |publisher=Wayne State University Press |author=Ḥayah Bar-Yitsḥaḳ |year=2001 |page=93 |isbn=0-8143-2789-3}}
* {{cite web |url=http://www.tripadvisor.ca/TravelersChoice-Destinations-cTop-g274723 |title=Top 10 Destinations &ndash; Poland |publisher=TripAdvisor.ca The world largest travel site |work=Travelers' Choice 2013 (winners) |access-date=25 August 2014 |author=TripAdvisor |pages=1 of 10}}
* {{cite journal | last1=Uzarowicz | first1=Łukasz | last2=Charzyński | first2=Przemysław | last3=Greinert | first3=Andrzej | last4=Hulisz | first4=Piotr | last5=Kabała | first5=Cezary | last6=Kusza | first6=Grzegorz | last7=Kwasowski | first7=Wojciech | last8=Pędziwiatr | first8=Artur | title=Studies of technogenic soils in Poland: past, present, and future perspectives | journal=[[Soil Science Annual]] | publisher=[[Soil Science Society of Poland]] | volume=71 | issue=4 | date=2021-01-14 | issn=2300-4967 | doi=10.37501/soilsa/131615 | pages=281–299| s2cid= | doi-access=free }}

{{refend}}


== Спољашње везе ==
== Спољашње везе ==
{{Commons category-lat|North European Plain}}
{{Commons category|North European Plain}}
* -{[https://web.archive.org/web/20080608155752/http://www.baltic-lagoon.net/ Baltic Lagoons]}-
* -{[https://web.archive.org/web/20080608155752/http://www.baltic-lagoon.net/ Baltic Lagoons]}-
* -{[http://lowlands-l.net/ Lowlands-L, an international discussion community dealing with the North European Plain, its cultures, language varieties, history, etc.; also dealing with Lowlands-based heritage in Britain, North America, Australia, etc.]}-
* -{[http://lowlands-l.net/ Lowlands-L, an international discussion community dealing with the North European Plain, its cultures, language varieties, history, etc.; also dealing with Lowlands-based heritage in Britain, North America, Australia, etc.]}-
* -{[http://www.ecosystema.ru/08nature/world/geoworld/geomap-euras.htm Clickable map] (''in Russian'')}-
* -{[http://www.ecosystema.ru/08nature/world/geoworld/geomap-euras.htm Clickable map] (''in Russian'')}-

{{Клица-географија}}


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Верзија на датум 31. март 2023. у 03:17

Средњоевропска низија је обојена зелено.
Топографија Европе.

Средњоевропска низија, Прибалтичка низија или Немачко-пољска низија, је низија која се простире у дужини од око 600 km (и упола толико по ширини) и налази на северу средње Европе. Она захвата северне делове Немачке и Пољске (одатле јој и назив Немачко-пољска низија)

It consists of the low plains between the Hercynian Europe[1][2][3] (Central European Highlands[4][5][6]) to the south and coastlines of the North Sea and the Baltic Sea to the north. These two seas are separated by the Jutland Peninsula (Denmark). The North European Plain is connected to the East European Plain, together forming the majority of the Great European Plain (European Plain).

Geography

Elevations vary between 0 and 200 m (0 to about 650 ft). While mostly used as farmland, the region also contains bogs, heath and lakes. The Wadden Sea, a large tidal area, is located on the North Sea coast.

A number of freshwater lagoons including the Szczecin Lagoon,[7][8] the Vistula Lagoon[9] and the Curonian Lagoon[10][11] are found on the Baltic Sea coast.

Одлике и рељеф

Средњоевропска низија је широка од 150 km на западу до више од 400 km на истоку, благо нагнута од средогорја према северу. На крајњем југу низије, на прелазу према средогорју, пространа су подручја прекривена прапором, према северу све је више слабије плодног моренског материјала. Морене су преобликоване у благо валовите платое између којих су влажније прадолине, обликоване токовима који су за леденог доба текли испод и рубом леденог покрова. Најсевернији део низије покривен је наносима, слабије се одводњава па се местимично јављају мочваре, посебно у источном делу.

Location

The North European Plain covers Flanders (northern Belgium and Northern France), the Netherlands, Northern Germany, Denmark, and most of central-western Poland; it touches the Czech Republic and southwestern part of Sweden as well.

Parts of eastern England can also be considered part of the same plain; as they share its low-lying character and were connected by land to the continent during the last ice age. The Northern European Plains are located also under the Baltic Sea.

Rivers

Major river-drainage basins include, from west to east: the Rhine, Ems, Weser, Elbe, Oder and Vistula.

The bases of these rivers are heavy with thin soil, making it hard for the farming to thrive near these rivers.

Sub-regions

Low Countries

Historically, especially in the Middle Ages and Early modern period, the western section has been known as the Low Countries.

North German Plain

The North German Plain is located north of the Central Uplands of Germany.

Polish Plain

The part in modern-day Poland is called the "Polish Plain" (пољ. Niż Polski or Nizina Polska) and stretches from the Baltic Sea in the north to the Sudetes and Carpathians

English flatlands

The extension of the plain into England consists mainly of the flatlands of East Anglia, the Fens and Lincolnshire, where the landscape is in parts strikingly similar to that of the Netherlands.

Референце

  1. ^ Martínez Catalán, José R. (2012-07-01). „The Central Iberian arc, an orocline centered in the Iberian Massif and some implications for the Variscan belt”. International Journal of Earth Sciences (на језику: енглески). 101 (5): 1299—1314. Bibcode:2012IJEaS.101.1299M. ISSN 1437-3262. S2CID 195334509. doi:10.1007/s00531-011-0715-6. 
  2. ^ Crespo-Blanc, Ana; Orozco, Miguel (1991-10-01). „The boundary between the Ossa-Morena and Southportuguese Zones (Southern Iberian Massif): Major suture in the European Hercynian Chain”. Geologische Rundschau (на језику: енглески). 80 (3): 691—702. Bibcode:1991GeoRu..80..691C. ISSN 1432-1149. S2CID 128688878. doi:10.1007/BF01803695. 
  3. ^ Lee, K. Y. (1989). „Geology of petroleum and coal deposits in the North China Basin, Eastern China”. USGS Bulletin 1871. Архивирано из оригинала 2019-09-13. г. Приступљено 2017-09-17. Table 1, p. 3. 
  4. ^ Pusch, Martin; Behrendt, Horst; Gancarczyk, Aleksandra; Kronvang, Brian; Sandin, Leonard; Stendera, Sonja; Wolter, Christian; Andersen, Hans E.; Fischer, Helmut (2009-01-01), Tockner, Klement; Uehlinger, Urs; Robinson, Christopher T., ур., „Chapter 14 - Rivers of the Central European Highlands and Plains”, Rivers of Europe (на језику: енглески), London: Academic Press, стр. 525—576, ISBN 978-0-12-369449-2, S2CID 128731308, doi:10.1016/b978-0-12-369449-2.00014-x, Приступљено 2021-09-29 
  5. ^ Pusch, Martin; Behrendt, Horst; Gancarczyk, Aleksandra; Kronvang, Brian; Sandin, Leonard; Stendera, Sonja; Wolter, Christian; Andersen, Hans E.; Fischer, Helmut; Hoffmann, Carl. C.; Nowacki, Franciszek; Schöll, Franz; Svendsen, Lars M.; Bäthe, Jürgen; Friberg, Nikolai; Hachoł, Justyna; Pedersen, Morten L.; Scholten, Matthias; Wnuk-Gławdel, Ewa (2009). „Rivers of the Central European Highlands and Plains”. Rivers of Europe. стр. 525—576. ISBN 9780123694492. S2CID 128731308. doi:10.1016/B978-0-12-369449-2.00014-X — преко ResearchGate. 
  6. ^ „Central European highlands and their hydrological role, with special”. studylib.net (на језику: енглески). Приступљено 2021-09-29. 
  7. ^ Gerald Schernewski, Baltic coastal ecosystems: structure, function, and coastal zone management, Springer, 2002, p.79, ISBN 3-540-42937-9
  8. ^ Ulrich Schiewer, Ecology of Baltic coastal waters, Springer, 2008, ISBN 3-540-73523-2
  9. ^ Górski, Karol (1949). Związek Pruski i poddanie się Prus Polsce: zbiór tekstów źródłowych (на језику: пољски). Poznań: Instytut Zachodni. стр. 51, 56. 
  10. ^ „Curonian Lagoon”. Encyclopædia Britannica. Приступљено 2009-10-17. 
  11. ^ I. Ethem Gönenç, Angheluta Vadineanu (2008). Sustainable Use and Development of Watersheds. Springer. ISBN 978-1-4020-8557-4. 

Литература

Спољашње везе