Jump to content

Edit filter log

Details for log entry 32665698

06:03, 24 May 2022: Batmann (talk | contribs) triggered filter 867, performing the action "edit" on Orava-Nowy Targ Basin. Actions taken: none; Filter description: Large creations by inexperienced user (examine | diff)

Changes made in edit

[[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]]

Action parameters

VariableValue
Edit count of the user (user_editcount)
283
Name of the user account (user_name)
'Batmann'
Age of the user account (user_age)
213870698
Groups (including implicit) the user is in (user_groups)
[ 0 => '*', 1 => 'user', 2 => 'autoconfirmed' ]
Rights that the user has (user_rights)
[ 0 => 'createaccount', 1 => 'read', 2 => 'edit', 3 => 'createtalk', 4 => 'writeapi', 5 => 'viewmywatchlist', 6 => 'editmywatchlist', 7 => 'viewmyprivateinfo', 8 => 'editmyprivateinfo', 9 => 'editmyoptions', 10 => 'abusefilter-log-detail', 11 => 'urlshortener-create-url', 12 => 'centralauth-merge', 13 => 'abusefilter-view', 14 => 'abusefilter-log', 15 => 'vipsscaler-test', 16 => 'collectionsaveasuserpage', 17 => 'reupload-own', 18 => 'move-rootuserpages', 19 => 'createpage', 20 => 'minoredit', 21 => 'editmyusercss', 22 => 'editmyuserjson', 23 => 'editmyuserjs', 24 => 'purge', 25 => 'sendemail', 26 => 'applychangetags', 27 => 'spamblacklistlog', 28 => 'mwoauthmanagemygrants', 29 => 'reupload', 30 => 'upload', 31 => 'move', 32 => 'autoconfirmed', 33 => 'editsemiprotected', 34 => 'skipcaptcha', 35 => 'transcode-reset', 36 => 'transcode-status', 37 => 'createpagemainns', 38 => 'movestable', 39 => 'autoreview' ]
Whether the user is editing from mobile app (user_app)
false
Whether or not a user is editing through the mobile interface (user_mobile)
false
Page ID (page_id)
0
Page namespace (page_namespace)
0
Page title without namespace (page_title)
'Orava-Nowy Targ Basin'
Full page title (page_prefixedtitle)
'Orava-Nowy Targ Basin'
Edit protection level of the page (page_restrictions_edit)
[]
Page age in seconds (page_age)
0
Action (action)
'edit'
Edit summary/reason (summary)
'translation from Polish'
Old content model (old_content_model)
''
New content model (new_content_model)
'wikitext'
Old page wikitext, before the edit (old_wikitext)
''
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]] '
New page size (new_size)
6610
Old page size (old_size)
0
Size change in edit (edit_delta)
6610
Lines added in edit (added_lines)
[ 0 => '[[File:Kramnica i Obłazowa a1.jpg|thumb|240px|Nowy Targ Basin with Pieniny Spiskie in the background]]', 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]]' ]
Lines removed in edit (removed_lines)
[]
Whether or not the change was made through a Tor exit node (tor_exit_node)
false
Unix timestamp of change (timestamp)
1653372232