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Page title without namespace (page_title ) | 'Orava-Nowy Targ Basin' |
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New page wikitext, after the edit (new_wikitext ) | '[[File:Kramnica i Obłazowa a1.jpg|thumb|240px|Nowy Targ Basin with Pieniny Spiskie in the background]]
[[File:514.11 Kotlina Orawsko-Nowotarska.png|thumb|240px|The area within Poland]]
[[File:Frydman a1.jpg|thumb|240px|A fragment of the Nowy Targ basin ([[Frydman]]) and a view of the Gorce Mountains]]
[[File:Kotlina Nowotarska BŻ3.jpg|thumb|240px|A view of [[Babia Góra]] and [[Beskid Orawsko-Podhalański]]]]
{{commonscat|Kotlina Orawsko-Nowotarska}}
The '''Orava-Nowy Targ Basin''' ({{lang-pl|Kotlina Orawsko-Nowotarska}}) is the northern, lowest part of the [[Podhale-Magura Area]], between the [[Western Beskids]] in the north and the [[Spisko-Gubałowski Highlands]] in the south.
==Boundaries==
The boundaries are as follows.<ref name=Kondracki>{{cite book|first=Jerzy|isbn=83-01-12479-2|location=Warszawa|last=Kondracki|publisher=Wyd. Naukowe PWN|year=1998|title=Geografia regionalna Polski}}</ref>
* to the west, along the foothills of the Slovak [[Orava Beskids]], slightly to the west of the [[Orava (reservoir)|Orava reservoir]]
* to the north, the basin borders on the [[Działy Orawskie]], the [[Beskid Orawsko-Podhalański]] and the [[Gorce Mountains]]. The border runs on the northern side of the Orava reservoir, through the [[Czarna Orawa]] valley, [[Piekielnik (river)|Piekielnik]] (a tributary of Czarna Orawa), along the foot of the hills of the Działy Orawskie to [[Nowy Targ]], from here through the [[Dunajec]] valley to the [[Lake Czorsztyn]], which is located within the Nowy Targ Basin.
* eastern border: a dam on the Lake Czorsztyn
* from the south, the valley borders with the [[Pieniny]] Mountains, [[Pogórze Bukowińskie]] and [[Pogórze Gubałowskie]]. The border runs along the southern banks of the Lake Czorsztyn to the western end of [[Zielone Skałki]], from here along the northern foothills of the [[Pieniny Spiskie]] and [[Skalice Nowotarskie]] (from [[Obłazowa]] through [[Cisowa Skała]] and [[Ranisberg]]), further up, initially along the [[Wielki Rogoźnik]] stream, then along the north-western foothills of the [[Pogórze Gubałowskie]] on eastern side of the [[Czarny Dunajec (river)|Czarny Dunajec]] to [[Koniówka]].<ref name=Sygnatura>{{cite book|isbn=978-83-87873-44-8|publisher=Sygnatura|title=Dookoła Tatr. Atrakcje turystyczne}}</ref> In Slovakia, the border runs along the [[Orava (river)|Orava]] valley and the foothills of the [[Pogórze Skoruszyńskie]].
==The Orava Basin and the Nowy Targ Basin==
The entire basin is uniform in terms of landscape and of the same origin, but in terms of hydrography, it is divided into two parts:
* [[Orava Basin]] - the western part, drained by the [[Orava (river)|Orava]] River and located in the [[Black Sea]] catchment area
* [[Nowy Targ Basin]] - the eastern part, drained by the [[Dunajec]] River and located in the catchment area of the [[Baltic Sea]]
In Poland, the [[European watershed]] runs through the basin between the [[Black Sea]] basin and the [[Baltic Sea]] basin, with few distinguishing features in the terrain. This section runs from the town of [[Koniówka]] on the western side of the [[Czarny Dunajec (river)|Czarny Dunajec]] river to the north, through the peat bogs to the town of [[Piekielnik]]. The slopes of both parts of the basin are inclined in opposite directions. The slopes of the Orava Basin descend in the west to a height of about 600 m above sea level, the Nowy Targ Basin on the eastern edges to about 510 m above sea level.<ref name=Kondracki/>
==Description of the region==
The basin was formed in the [[Neogene]] as a result of the [[Fold (geology)|folding]] of the area between mountain ranges and foothills. In the basin created in this way, a lake was formed, which over time was filled with sediments of gravel and clay; their thickness in the western part reaches 300 m. Also in the [[Quaternary]], during successive [[glacial period]]s, [[alluvial cone]]s accumulated here glacial and river deposits. In the basin, and especially in the Baltic-Black Sea watershed that cuts it across, a unique complex of [[raised bog]]s has developed. These bogs, completely dependent on rainwater, began to form around 10,000 years ago, when the climate warmed after the glacial period.<ref name="Bagna">[http://bagna.pl/CMS/index.php?option=com_content&view=article&id=419 O torfowiskach orawsko-nowotarskich na stronie Bagna.pl]</ref> Today, they present a complex of raised bogs, bogs and marsh forests, unique in Poland and at the same time rare in Europe, giving a specific character to the landscape of the Basin.
The vegetation of peat bogs is particularly characteristic. In addition to sphagnum mosses, there are plants adapted to the deficiency of nutrients - insectivorous [[Drosera|sundews]] and [[Pinguicula vulgaris|common butterwort]]. A unique feature of the Orava-Nowy Targ Basin bogs is the presence of [[Pinus mugo|mountain pine]], which is usually found at higher altitudes, as well as the rare {{ill|Pinus mugo nothosubsp. rotundata|lt=mud pine|pl|Sosna błotna}} (a form of [[Pinus × rhaetica|Rhaetic pine]]), which is an introgressive hybrid of mountain pine and [[Pinus sylvestris|scots pine]].<ref name="Bagna"/> In one of the peat bogs, called [[Puścizna Wielka]], the site of [[Rubus chamaemorus|cloudberry]], a rare plant considered a [[glacial relict]], was discovered in 2002. It is the southernmost habitat of this plant in the world.<ref>{{cite book|date=2008|first=Zbigniew|first2=Halina|isbn=978-83-89648-71-6|location=Kraków|last=Mirek|last2=Piękoś-Mirkowa|publisher=Instytut Botaniki PAN|title=Czerwona księga Karpat Polskich}}</ref>
The region is moderately transformed as a result of human activity.<ref name=Kondracki/> It has two large, artificially created water reservoirs: the [[Orava (reservoir)|Orava reservoir]] and the [[Lake Czorsztyn]]. The main towns are [[Nowy Targ]] in Poland and [[Námestovo]] in Slovakia.<ref name=Sygnatura/>
The Orawa-Nowy Targ Basin covers three historical and ethnographic lands: [[Orava (region)|Orava]] in the western part (e.g. [[Jabłonka]], [[Chyżne]], and the entire area of the valley in Slovakia), [[Podhale]] in the eastern part (e.g. [[Czarny Dunajec]], [[Nowy Targ]]) and a small fragment of [[Spiš]] at the eastern end (including [[Nowa Biała]], [[Frydman]]).<ref name=Kondracki/>
==References==
{{reflist}}
{{wide image|Kotlina Orawsko-Nowotarska PSG1.jpg|1000px|The Orawa-Nowy Targ Basin and the Tatra Mountains. View from a gravel pit in [[Podczerwone]]}}
[[Category:Depressions of Europe]]
[[Category:Geography of Poland]]
[[Category:Geography of Slovakia]]' |
Unified diff of changes made by edit (edit_diff ) | '@@ -1,0 +1,40 @@
+[[File:Kramnica i Obłazowa a1.jpg|thumb|240px|Nowy Targ Basin with Pieniny Spiskie in the background]]
+[[File:514.11 Kotlina Orawsko-Nowotarska.png|thumb|240px|The area within Poland]]
+[[File:Frydman a1.jpg|thumb|240px|A fragment of the Nowy Targ basin ([[Frydman]]) and a view of the Gorce Mountains]]
+[[File:Kotlina Nowotarska BŻ3.jpg|thumb|240px|A view of [[Babia Góra]] and [[Beskid Orawsko-Podhalański]]]]
+{{commonscat|Kotlina Orawsko-Nowotarska}}
+The '''Orava-Nowy Targ Basin''' ({{lang-pl|Kotlina Orawsko-Nowotarska}}) is the northern, lowest part of the [[Podhale-Magura Area]], between the [[Western Beskids]] in the north and the [[Spisko-Gubałowski Highlands]] in the south.
+
+==Boundaries==
+
+The boundaries are as follows.<ref name=Kondracki>{{cite book|first=Jerzy|isbn=83-01-12479-2|location=Warszawa|last=Kondracki|publisher=Wyd. Naukowe PWN|year=1998|title=Geografia regionalna Polski}}</ref>
+
+* to the west, along the foothills of the Slovak [[Orava Beskids]], slightly to the west of the [[Orava (reservoir)|Orava reservoir]]
+* to the north, the basin borders on the [[Działy Orawskie]], the [[Beskid Orawsko-Podhalański]] and the [[Gorce Mountains]]. The border runs on the northern side of the Orava reservoir, through the [[Czarna Orawa]] valley, [[Piekielnik (river)|Piekielnik]] (a tributary of Czarna Orawa), along the foot of the hills of the Działy Orawskie to [[Nowy Targ]], from here through the [[Dunajec]] valley to the [[Lake Czorsztyn]], which is located within the Nowy Targ Basin.
+* eastern border: a dam on the Lake Czorsztyn
+* from the south, the valley borders with the [[Pieniny]] Mountains, [[Pogórze Bukowińskie]] and [[Pogórze Gubałowskie]]. The border runs along the southern banks of the Lake Czorsztyn to the western end of [[Zielone Skałki]], from here along the northern foothills of the [[Pieniny Spiskie]] and [[Skalice Nowotarskie]] (from [[Obłazowa]] through [[Cisowa Skała]] and [[Ranisberg]]), further up, initially along the [[Wielki Rogoźnik]] stream, then along the north-western foothills of the [[Pogórze Gubałowskie]] on eastern side of the [[Czarny Dunajec (river)|Czarny Dunajec]] to [[Koniówka]].<ref name=Sygnatura>{{cite book|isbn=978-83-87873-44-8|publisher=Sygnatura|title=Dookoła Tatr. Atrakcje turystyczne}}</ref> In Slovakia, the border runs along the [[Orava (river)|Orava]] valley and the foothills of the [[Pogórze Skoruszyńskie]].
+
+==The Orava Basin and the Nowy Targ Basin==
+The entire basin is uniform in terms of landscape and of the same origin, but in terms of hydrography, it is divided into two parts:
+* [[Orava Basin]] - the western part, drained by the [[Orava (river)|Orava]] River and located in the [[Black Sea]] catchment area
+* [[Nowy Targ Basin]] - the eastern part, drained by the [[Dunajec]] River and located in the catchment area of the [[Baltic Sea]]
+
+In Poland, the [[European watershed]] runs through the basin between the [[Black Sea]] basin and the [[Baltic Sea]] basin, with few distinguishing features in the terrain. This section runs from the town of [[Koniówka]] on the western side of the [[Czarny Dunajec (river)|Czarny Dunajec]] river to the north, through the peat bogs to the town of [[Piekielnik]]. The slopes of both parts of the basin are inclined in opposite directions. The slopes of the Orava Basin descend in the west to a height of about 600 m above sea level, the Nowy Targ Basin on the eastern edges to about 510 m above sea level.<ref name=Kondracki/>
+
+==Description of the region==
+The basin was formed in the [[Neogene]] as a result of the [[Fold (geology)|folding]] of the area between mountain ranges and foothills. In the basin created in this way, a lake was formed, which over time was filled with sediments of gravel and clay; their thickness in the western part reaches 300 m. Also in the [[Quaternary]], during successive [[glacial period]]s, [[alluvial cone]]s accumulated here glacial and river deposits. In the basin, and especially in the Baltic-Black Sea watershed that cuts it across, a unique complex of [[raised bog]]s has developed. These bogs, completely dependent on rainwater, began to form around 10,000 years ago, when the climate warmed after the glacial period.<ref name="Bagna">[http://bagna.pl/CMS/index.php?option=com_content&view=article&id=419 O torfowiskach orawsko-nowotarskich na stronie Bagna.pl]</ref> Today, they present a complex of raised bogs, bogs and marsh forests, unique in Poland and at the same time rare in Europe, giving a specific character to the landscape of the Basin.
+
+The vegetation of peat bogs is particularly characteristic. In addition to sphagnum mosses, there are plants adapted to the deficiency of nutrients - insectivorous [[Drosera|sundews]] and [[Pinguicula vulgaris|common butterwort]]. A unique feature of the Orava-Nowy Targ Basin bogs is the presence of [[Pinus mugo|mountain pine]], which is usually found at higher altitudes, as well as the rare {{ill|Pinus mugo nothosubsp. rotundata|lt=mud pine|pl|Sosna błotna}} (a form of [[Pinus × rhaetica|Rhaetic pine]]), which is an introgressive hybrid of mountain pine and [[Pinus sylvestris|scots pine]].<ref name="Bagna"/> In one of the peat bogs, called [[Puścizna Wielka]], the site of [[Rubus chamaemorus|cloudberry]], a rare plant considered a [[glacial relict]], was discovered in 2002. It is the southernmost habitat of this plant in the world.<ref>{{cite book|date=2008|first=Zbigniew|first2=Halina|isbn=978-83-89648-71-6|location=Kraków|last=Mirek|last2=Piękoś-Mirkowa|publisher=Instytut Botaniki PAN|title=Czerwona księga Karpat Polskich}}</ref>
+
+The region is moderately transformed as a result of human activity.<ref name=Kondracki/> It has two large, artificially created water reservoirs: the [[Orava (reservoir)|Orava reservoir]] and the [[Lake Czorsztyn]]. The main towns are [[Nowy Targ]] in Poland and [[Námestovo]] in Slovakia.<ref name=Sygnatura/>
+
+The Orawa-Nowy Targ Basin covers three historical and ethnographic lands: [[Orava (region)|Orava]] in the western part (e.g. [[Jabłonka]], [[Chyżne]], and the entire area of the valley in Slovakia), [[Podhale]] in the eastern part (e.g. [[Czarny Dunajec]], [[Nowy Targ]]) and a small fragment of [[Spiš]] at the eastern end (including [[Nowa Biała]], [[Frydman]]).<ref name=Kondracki/>
+
+==References==
+{{reflist}}
+
+{{wide image|Kotlina Orawsko-Nowotarska PSG1.jpg|1000px|The Orawa-Nowy Targ Basin and the Tatra Mountains. View from a gravel pit in [[Podczerwone]]}}
+
+[[Category:Depressions of Europe]]
+[[Category:Geography of Poland]]
+[[Category:Geography of Slovakia]]
' |
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1 => '[[File:514.11 Kotlina Orawsko-Nowotarska.png|thumb|240px|The area within Poland]]',
2 => '[[File:Frydman a1.jpg|thumb|240px|A fragment of the Nowy Targ basin ([[Frydman]]) and a view of the Gorce Mountains]]',
3 => '[[File:Kotlina Nowotarska BŻ3.jpg|thumb|240px|A view of [[Babia Góra]] and [[Beskid Orawsko-Podhalański]]]]',
4 => '{{commonscat|Kotlina Orawsko-Nowotarska}}',
5 => 'The '''Orava-Nowy Targ Basin''' ({{lang-pl|Kotlina Orawsko-Nowotarska}}) is the northern, lowest part of the [[Podhale-Magura Area]], between the [[Western Beskids]] in the north and the [[Spisko-Gubałowski Highlands]] in the south.',
6 => '',
7 => '==Boundaries==',
8 => '',
9 => 'The boundaries are as follows.<ref name=Kondracki>{{cite book|first=Jerzy|isbn=83-01-12479-2|location=Warszawa|last=Kondracki|publisher=Wyd. Naukowe PWN|year=1998|title=Geografia regionalna Polski}}</ref>',
10 => '',
11 => '* to the west, along the foothills of the Slovak [[Orava Beskids]], slightly to the west of the [[Orava (reservoir)|Orava reservoir]]',
12 => '* to the north, the basin borders on the [[Działy Orawskie]], the [[Beskid Orawsko-Podhalański]] and the [[Gorce Mountains]]. The border runs on the northern side of the Orava reservoir, through the [[Czarna Orawa]] valley, [[Piekielnik (river)|Piekielnik]] (a tributary of Czarna Orawa), along the foot of the hills of the Działy Orawskie to [[Nowy Targ]], from here through the [[Dunajec]] valley to the [[Lake Czorsztyn]], which is located within the Nowy Targ Basin.',
13 => '* eastern border: a dam on the Lake Czorsztyn',
14 => '* from the south, the valley borders with the [[Pieniny]] Mountains, [[Pogórze Bukowińskie]] and [[Pogórze Gubałowskie]]. The border runs along the southern banks of the Lake Czorsztyn to the western end of [[Zielone Skałki]], from here along the northern foothills of the [[Pieniny Spiskie]] and [[Skalice Nowotarskie]] (from [[Obłazowa]] through [[Cisowa Skała]] and [[Ranisberg]]), further up, initially along the [[Wielki Rogoźnik]] stream, then along the north-western foothills of the [[Pogórze Gubałowskie]] on eastern side of the [[Czarny Dunajec (river)|Czarny Dunajec]] to [[Koniówka]].<ref name=Sygnatura>{{cite book|isbn=978-83-87873-44-8|publisher=Sygnatura|title=Dookoła Tatr. Atrakcje turystyczne}}</ref> In Slovakia, the border runs along the [[Orava (river)|Orava]] valley and the foothills of the [[Pogórze Skoruszyńskie]].',
15 => '',
16 => '==The Orava Basin and the Nowy Targ Basin==',
17 => 'The entire basin is uniform in terms of landscape and of the same origin, but in terms of hydrography, it is divided into two parts:',
18 => '* [[Orava Basin]] - the western part, drained by the [[Orava (river)|Orava]] River and located in the [[Black Sea]] catchment area',
19 => '* [[Nowy Targ Basin]] - the eastern part, drained by the [[Dunajec]] River and located in the catchment area of the [[Baltic Sea]]',
20 => '',
21 => 'In Poland, the [[European watershed]] runs through the basin between the [[Black Sea]] basin and the [[Baltic Sea]] basin, with few distinguishing features in the terrain. This section runs from the town of [[Koniówka]] on the western side of the [[Czarny Dunajec (river)|Czarny Dunajec]] river to the north, through the peat bogs to the town of [[Piekielnik]]. The slopes of both parts of the basin are inclined in opposite directions. The slopes of the Orava Basin descend in the west to a height of about 600 m above sea level, the Nowy Targ Basin on the eastern edges to about 510 m above sea level.<ref name=Kondracki/>',
22 => '',
23 => '==Description of the region==',
24 => 'The basin was formed in the [[Neogene]] as a result of the [[Fold (geology)|folding]] of the area between mountain ranges and foothills. In the basin created in this way, a lake was formed, which over time was filled with sediments of gravel and clay; their thickness in the western part reaches 300 m. Also in the [[Quaternary]], during successive [[glacial period]]s, [[alluvial cone]]s accumulated here glacial and river deposits. In the basin, and especially in the Baltic-Black Sea watershed that cuts it across, a unique complex of [[raised bog]]s has developed. These bogs, completely dependent on rainwater, began to form around 10,000 years ago, when the climate warmed after the glacial period.<ref name="Bagna">[http://bagna.pl/CMS/index.php?option=com_content&view=article&id=419 O torfowiskach orawsko-nowotarskich na stronie Bagna.pl]</ref> Today, they present a complex of raised bogs, bogs and marsh forests, unique in Poland and at the same time rare in Europe, giving a specific character to the landscape of the Basin.',
25 => '',
26 => 'The vegetation of peat bogs is particularly characteristic. In addition to sphagnum mosses, there are plants adapted to the deficiency of nutrients - insectivorous [[Drosera|sundews]] and [[Pinguicula vulgaris|common butterwort]]. A unique feature of the Orava-Nowy Targ Basin bogs is the presence of [[Pinus mugo|mountain pine]], which is usually found at higher altitudes, as well as the rare {{ill|Pinus mugo nothosubsp. rotundata|lt=mud pine|pl|Sosna błotna}} (a form of [[Pinus × rhaetica|Rhaetic pine]]), which is an introgressive hybrid of mountain pine and [[Pinus sylvestris|scots pine]].<ref name="Bagna"/> In one of the peat bogs, called [[Puścizna Wielka]], the site of [[Rubus chamaemorus|cloudberry]], a rare plant considered a [[glacial relict]], was discovered in 2002. It is the southernmost habitat of this plant in the world.<ref>{{cite book|date=2008|first=Zbigniew|first2=Halina|isbn=978-83-89648-71-6|location=Kraków|last=Mirek|last2=Piękoś-Mirkowa|publisher=Instytut Botaniki PAN|title=Czerwona księga Karpat Polskich}}</ref>',
27 => '',
28 => 'The region is moderately transformed as a result of human activity.<ref name=Kondracki/> It has two large, artificially created water reservoirs: the [[Orava (reservoir)|Orava reservoir]] and the [[Lake Czorsztyn]]. The main towns are [[Nowy Targ]] in Poland and [[Námestovo]] in Slovakia.<ref name=Sygnatura/>',
29 => '',
30 => 'The Orawa-Nowy Targ Basin covers three historical and ethnographic lands: [[Orava (region)|Orava]] in the western part (e.g. [[Jabłonka]], [[Chyżne]], and the entire area of the valley in Slovakia), [[Podhale]] in the eastern part (e.g. [[Czarny Dunajec]], [[Nowy Targ]]) and a small fragment of [[Spiš]] at the eastern end (including [[Nowa Biała]], [[Frydman]]).<ref name=Kondracki/>',
31 => '',
32 => '==References==',
33 => '{{reflist}}',
34 => '',
35 => '{{wide image|Kotlina Orawsko-Nowotarska PSG1.jpg|1000px|The Orawa-Nowy Targ Basin and the Tatra Mountains. View from a gravel pit in [[Podczerwone]]}}',
36 => '',
37 => '[[Category:Depressions of Europe]]',
38 => '[[Category:Geography of Poland]]',
39 => '[[Category:Geography of Slovakia]]'
] |
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Unix timestamp of change (timestamp ) | 1653372232 |