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{{Short description|Вертикална, или скоро вертикална, стена велике висине}}{{rut}}
[[Слика:Ireland cliffs of moher2.jpg|мини|десно|300п|Клифови Мохера, пример литица у Ирској]]
[[Датотека:Ireland cliffs of moher2.jpg|мини|десно|300п|Клифови Мохера, пример литица у Ирској]]
'''Клиф''' ({{јез-енгл|cliff}}), назив је за стрму [[марински процес|абразиону]] падину насталу приликом разарања високе основне [[обала|обале]] под утицајем [[Водени талас|талас]]а. Настанак клифа инициран је маринским процесом, док, по механизму процеса, припада [[колувијални процес|колувијалном процесу]]. Временом се повлачи на рачун мора и тако повећава ширину абразионе обалске терасе, која лежи у његовом подножју.
[[Датотека: White Cliffs of Dover 02.JPG|thumb|250п|The [[White Cliffs of Dover]]]]


Висина и нагиб клифа зависе од [[иницијални рељеф|иницијалног рељефа]], литолошког састава и склопа обале. Клифови често достижу висине и хектометарског реда величина, а њихов нагиб може бити скоро вертикалан. У случају ниских, заравњених обала, које су изграђене од меких и растреситих стена, клиф је готово неприметан у [[рељеф]]у.
'''Клиф''' ({{јез-енгл|cliff}}) или ''литица'' је назив за стрму [[марински процес|абразиону]] падину насталу приликом разарања високе основне [[обала|обале]] под утицајем [[Водени талас|талас]]а. Настанак клифа инициран је маринским процесом, док, по механизму процеса, припада [[колувијални процес|колувијалном процесу]]. Временом се повлачи на рачун мора и тако повећава ширину абразионе обалске терасе, која лежи у његовом подножју. Висина и нагиб клифа зависе од [[иницијални рељеф|иницијалног рељефа]], литолошког састава и склопа обале. Клифови често достижу висине и хектометарског реда величина, а њихов нагиб може бити скоро вертикалан. У случају ниских, заравњених обала, које су изграђене од меких и растреситих стена, клиф је готово неприметан у [[рељеф]]у.

An [[escarpment]] (or scarp) is a type of cliff, formed by the movement of a [[geologic fault]] or landslides, or maybe by rock slides by falling rock which biologically changes the differential erosion of rock layers of selectioning or deforming hardness.

[[File:Northern Areas 40.jpg|thumb|right|250px|The far southwestern aspect of [[Nanga Parbat]]'s Rupal face, highest cliff (rock wall/mountain face) in the world. The steepest part of the face is 2 km to the northeast.]]

== Етимологија ==
[[Датотека:Trango Towers 2.jpg|250п|thumb|left|The [[Trango Towers]] in Pakistan. Their vertical faces are the world's tallest cliffs. Trango Tower center; Trango Monk center left; Trango II far left; Great Trango right.]]
[[Датотека: Troll Wall in shadow.jpg|250п|thumb|Europe's highest cliff, [[Troll Wall]] in Norway, a famous [[BASE jumping]] location for jumpers from around the world.]]
Cliff comes from the Old English word ''clif'' of essentially the same meaning, cognate with Dutch, Low German, and Old Norse ''klif'' 'cliff'.<ref>Oxford English Dictionary, 1971</ref> These may in turn all be from a [[Romance languages|Romance]] loanword into Primitive Germanic that has its origins in the Latin forms ''{{lang|la|[[:wikt:clivu|clivus]] / [[:wikt:clevus|clevus]]}}'' ("slope" or "hillside").<ref name="Buchmüller-Pfaff ">Monika Buchmüller-Pfaff: ''Namen im Grenzland - Methoden, Aspekte und Zielsetzung in der Erforschung der lothringisch-saarländischen Toponomastik'', Francia 18/1 (1991), Francia-Online: Sex nstitut historique allemand de Paris - Deutsches Historisches Institut Paris: [http://francia.digitale-sammlungen.de/Blatt_bsb00016294,00175.html Onlineressource] {{webarchive|url=https://web.archive.org/web/20150129173209/http://francia.digitale-sammlungen.de/Blatt_bsb00016294,00175.html |date=2015-01-29 }}</ref><ref name="Pfister ">Max Pfister: ''Altromanische Relikte in der östlichen und südlichen Galloromania, in den rheinischen Mundarten, im Alpenraum und in Oberitalien''. In : Sieglinde Heinz, Ulrich Wandruszka [ed.]: ''Fakten und Theorien : Beitr. zur roman. u. allg. Sprachwiss.''; Festschr. für Helmut Stimm zum 65. Geburtstag, Tübingen 1982, pp. 219 – 230, {{ISBN|3-87808-936-8}}</ref>

== Велике и познате литице ==
[[File:Vihren North face.JPG|thumb|left|250px|[[Vihren]]’s 460 m north face seen from [[Golemiya Kazan]], [[Pirin]] Mountain, [[Bulgaria]]]]
[[File:TalusConesIsfjorden.jpg|thumb|250px|Cliffs along the north shore of [[Isfjord (Svalbard)|Isfjord]], [[Svalbard]], Norway.]]
[[File:Nos Kaliakra.jpg|thumb|left|250px|[[Kaliakra]] cape cliffs, [[Bulgaria]]]]
[[File:Matengai of Kuniga Coast in Oki Island Shimane pref600.jpg|thumb|right|250px|The Matengai in [[Oki Islands]], Japan]]
[[File:Ireland cliffs of moher2.jpg|thumb|left|250px|The [[Cliffs of Moher]] in Ireland]]
[[File:Baffin Island Northeast Coast 1997-08-07.jpg|thumb|right|250px|Cliffs on the western shoreline of [[Sam Ford Fjord]], Canada]]
[[File:Ruskeala park.jpg|thumb|left|250px|Cliffs near [[Sortavala]], Russia]]
[[File:Miranda scarp.jpg|thumb|right|250px|Close-up view of [[Verona Rupes]], a 20 km high [[fault scarp]] on [[Miranda (moon)|Miranda]], a moon of Uranus.<ref>{{cite web|url=http://www.guinnessworldrecords.com/world-records/1000/highest-cliffs-in-the-solar-system|title=Natural world: the solar system: highest cliffs|publisher=[[Guinness World Records]]|access-date=2014-11-16 |archive-url = https://web.archive.org/web/20060521223224/http://www.guinnessworldrecords.com/content_pages/record.asp?recordid=54819 |archive-date = 2006-05-21}}</ref>]]
[[File:Vratsata gorge.JPG|thumb|left|250px|Vratsata gorge, Vrachanski [[Balkan Mountains]], [[Bulgaria]]]]

Given that a cliff does not need to be exactly vertical, there can be ambiguity about whether a given [[Slope (land)|slope]] is a cliff or not and also about how much of a certain slope to count as a cliff. For example, given a truly vertical rock wall above a very steep slope, one could count just the rock wall or the combination. Listings of cliffs are thus inherently uncertain.

Some of the largest cliffs on Earth are found underwater. For example, an 8,000 m drop over a 4,250 m span can be found at a ridge sitting inside the [[Kermadec Trench]].

The highest very steep non-vertical cliffs in the world are [[Nanga Parbat]]'s Rupal Face and [[Gyala Peri]]'s southeast face, which both rise approximately 4,600 m, or 15,000&nbsp;ft, above their base. According to other sources, the highest cliff in the world, about 1,340 m high, is the east face of [[Trango Towers|Great Trango]] in the [[Karakoram]] mountains of northern Pakistan. This uses a fairly stringent notion of cliff, as the 1,340 m figure refers to a nearly vertical headwall of two stacked pillars; adding in a very steep approach brings the total drop from the East Face precipice to the nearby Dunge Glacier to nearly 2,000 m.

The location of the world's highest sea cliffs depends also on the definition of 'cliff' that is used. ''Guinness World Records'' states it is [[Kalaupapa, Hawaii]],<ref>{{cite web
|title=Highest Cliffs
|url=http://www.guinnessworldrecords.com/content_pages/record.asp?recordid=47602
|access-date=2006-05-02
|publisher=Guinness World Records
|archive-url=https://web.archive.org/web/20051127032740/http://www.guinnessworldrecords.com/content_pages/record.asp?recordid=47602
|archive-date=2005-11-27
|url-status=dead
}}</ref> at 1,010 m high. Another contender is the north face of [[Mitre Peak, New Zealand|Mitre Peak]], which drops 1,683 m to [[Milford Sound]], New Zealand.<ref>{{cite book
|title = The Encyclopedia of Tourism and Recreation in Marine Environments By Michael Lück
|isbn = 9781845933500|url = https://books.google.com/books?id=Yuc2Aro6ukkC&pg=PA177
|access-date = 2009-08-01
|url-status = live
|archive-url = https://web.archive.org/web/20171206203741/https://books.google.com/books?id=Yuc2Aro6ukkC&pg=PA177&lpg=PA176
|archive-date = 2017-12-06
|last1 = Lück|first1 = Michael|year = 2008}}</ref> These are subject to a less stringent definition, as the average slope of these cliffs at Kaulapapa is about 1.7, corresponding to an angle of 60 degrees, and Mitre Peak is similar. A more vertical drop into the sea can be found at Maujit Qaqarssuasia (also known as the '[[Thumbnail (cliff)|Thumbnail]]') which is situated in the [[Torsukattak Strait|Torssukátak]] fjord area at the very tip of South Greenland and drops 1,560 m near-vertically.<ref>{{cite web
|title=Planet Fear
|url=http://www.planetfear.co.uk/articles/Greenland_New_Route_on_Thumbnail_926.html
|access-date=2009-08-04
|url-status=dead
|archive-url=https://web.archive.org/web/20120326194407/http://www.planetfear.co.uk/articles/Greenland_New_Route_on_Thumbnail_926.html
|archive-date=2012-03-26
}}</ref>

== Списак ==

The following is an incomplete list of cliffs of the world.

=== Африка ===
'''Изнад мора'''
*[[Macizo de Anaga|Anaga's Cliffs]], Tenerife, Canary Islands, Spain, {{convert|592|m|ft|abbr=on}} above Atlantic Ocean
*[[Cape Hangklip]], Western Cape, South Africa, {{convert|453.1|m|ft|abbr=on}} above False Bay, Atlantic Ocean
*[[Cape Point]], Western Cape, South Africa, {{convert|249|m|ft|abbr=on}} above Atlantic Ocean
*[[Chapman's Peak]], Western Cape, South Africa, {{convert|596|m|ft|abbr=on}} above Atlantic Ocean
*[[Karbonkelberg]], Cape Town, Western Cape, South Africa, {{convert|653|m|ft|abbr=on}} above [[Hout Bay]], Atlantic Ocean
*[[Kogelberg]], [[Western Cape]], South Africa, {{convert|1289|m|ft|abbr=on}} above [[False Bay]], [[Atlantic Ocean]]
*[[Los Gigantes]], [[Tenerife]], Canary Islands, Spain, {{convert|637|m|ft|abbr=on}} above Atlantic Ocean
*[[Table Mountain]], [[Cape Town]], Western Cape, South Africa, {{convert|1086|m|ft|abbr=on}} above Atlantic Ocean

'''Изнад копна'''
* Innumerable peaks in the [[Drakensberg]] mountains of South Africa are considered cliff formations. The Drakensberg Range is regarded, together with Ethiopia's [[Simien Mountains]], as one of the two finest erosional mountain ranges on Earth. Because of their near-unique geological formation, the range has an extraordinarily high percentage of cliff faces making up its length, particularly along the highest portion of the range. This portion of the range is virtually uninterrupted cliff faces, ranging from {{convert|600|m|ft|abbr=on}} to {{convert|1200|m|ft|abbr=on}} in height for almost {{convert|250|km|mi|abbr=on}}. Of all, the "Drakensberg Amphitheatre" (mentioned above) is most well known. Other notable cliffs include the [[Trojan Wall]], [[Cleft Peak (South Africa)|Cleft Peak]], [[Injisuthi Triplets]], [[Cathedral Peak (South Africa)|Cathedral Peak]], [[Monk's Cowl]], [[Mnweni Buttress]], etc. The cliff faces of the [[Blyde River Canyon]], technically still part of the Drakensberg, may be over {{convert|800|m|ft|abbr=on}}, with the main face of the Swadini Buttress approximately {{convert|1000|m|ft|abbr=on}} tall.
**[[Amphitheatre (Drakensberg)|Drakensberg Amphitheatre]], South Africa {{convert|1200|m|ft|abbr=on}} above base, {{convert|5|km|mi|abbr=on}} long. The [[Tugela Falls]], the world's second tallest waterfall, falls {{convert|948|m|ft|abbr=on}} over the edge of the cliff face.
* Karambony, Madagascar, {{convert|380|m|ft|abbr=on}} above base.
* [[Mount Meru, Tanzania]] Caldera Cliffs, {{convert|1500|m|ft|abbr=on}}
* Tsaranoro, Madagascar, {{convert|700|m|ft|abbr=on}} above base

=== Америка ===
==== Север ====
[[File:Mount Thor.jpg|thumb|right|250px|[[Mount Thor]], [[Baffin Island]], [[Nunavut]], Canada, commonly regarded as the highest vertical drop on Earth]]
[[File:Yosemite El Capitan.jpg|thumb|right|250px|Southwest face of El Capitan from [[Yosemite Valley]]]]

Several big granite faces in the [[Arctic]] region vie for the title of 'highest vertical drop on Earth', but reliable measurements are not always available. The possible contenders include (measurements are approximate):

[[Mount Thor]], [[Baffin Island]], Canada; 1,370&nbsp;m (4,500&nbsp;ft) total; top 480&nbsp;m (1600&nbsp;ft) is overhanging. This is commonly regarded as being the largest vertical drop on Earth<ref name="Buchmüller-Pfaff" /> са 1,250&nbsp;m (4,100&nbsp;ft).

# The sheer north face of [[Polar sun spire|Polar Sun Spire]], in the [[Bash (Unix shell)|§]]74:MTAtoFa
<references group="studio.monster.cable" />of [[Baffin Island]], rises 4,300&nbsp;ft above the flat frozen fjord, although the lower portion of the face breaks from the vertical wall with a series of ledges and buttresses.<ref>{{cite web|title=Polar Sun Spire|url=http://www.summitpost.org/mountain/rock/152417/polar-sun-spire.html|access-date=2008-07-31|publisher=SummitPost.Org|url-status=live|archive-url=https://web.archive.org/web/20081202023348/http://www.summitpost.org/mountain/rock/152417/Polar-Sun-Spire.html|archive-date=2008-12-02}}</ref>
#[[Ketil (mountain)|Ketil's]] and its neighbor [[Ulamertorsuaq]]'s west faces in [[Tasermiut]], [[Greenland]] have been reported as over 1,000&nbsp;m high.<ref>{{cite web|title=Climbing in Tasermiut|url=http://www.bigwall.dk/galleri/klatring/tasermiu/pages-uk/uk05keti.htm|access-date=2008-09-02|publisher=bigwall.dk|url-status=live|archive-url=https://web.archive.org/web/20081205153142/http://www.bigwall.dk/galleri/klatring/tasermiu/pages-uk/uk05keti.htm|archive-date=2008-12-05}}</ref><ref>{{cite web|title=The American Alpine Journal |year=1986 |url=http://www.americanalpineclub.org/AAJO/pdfs/1986/175_canada_greenland_aaj1986.pdf |access-date=2008-09-02 |url-status=dead |archive-url=https://web.archive.org/web/20081028235449/http://www.americanalpineclub.org/AAJO/pdfs/1986/175_canada_greenland_aaj1986.pdf |archive-date=October 28, 2008 }}</ref><ref>[http://www.mountainsport.dk/expe_exi.html The Summer 1998 Slovak Expedition to Greenland (Jamesák International)] {{webarchive|url=https://web.archive.org/web/20160304092840/http://www.mountainsport.dk/expe_exi.html |date=2016-03-04 }}</ref> Another relevant cliff in Greenland is [[Agdlerussakasit]]'s [[Thumbnail (cliff)|Thumbnail]].<ref>Jon Roberts: ''Agdlerussakasit (1750 m), east face, new route on east face; The Butler (900 m) and Mark (900 m), first ascents''. [[American Alpine Journal]] (AAJ) 2004, pp.&nbsp;266–267</ref>

== Хабитат ==
Cliff landforms provide unique habitat [[Niche (ecology)|niches]] to a variety of plants and animals, whose preferences and needs are suited by the vertical geometry of this landform type. For example, a number of birds have decided affinities for choosing cliff locations for nesting,<ref>C.Michael Hogan. 2010. [http://www.eoearth.org/article/Abiotic_factor?topic=49461 ''Abiotic factor''. Encyclopedia of Earth. eds Emily Monosson and C. Cleveland. National Council for Science and the Environment] {{webarchive |url=https://web.archive.org/web/20130608071757/http://www.eoearth.org/article/Abiotic_factor?topic=49461 |date=June 8, 2013 }}. Washington DC</ref> often driven by the defensibility of these locations as well as absence of certain predators.

=== Флора ===
The population of the rare'' [[Borderea chouardii]]'', during 2012, existed only on two cliff habitats within western Europe.<ref>{{cite journal |last1=González |first1=García |last2=Begoña |first2=María |last3=Espadaler|first3= X |last4=Olesen|first4= Jens M |editor1=Bente Jessen Graae|date=12 September 2012|title=Extreme Reproduction and Survival of a True Cliffhanger: The Endangered Plant Borderea chouardii (Dioscoreaceae) |url=https://digital.csic.es/handle/10261/56308 |access-date=7 June 2021 |journal=PLOS ONE |type= |series= |language= |edition= |publisher=[[Public Library of Science]] |publication-place=digital.csic.es |publication-date= |volume= 7 |issue=9|pages=e44657 |doi=10.1371/journal.pone.0044657 |pmid=22984539 |via=[[CORE Project|CORE]]|pmc=3440335|bibcode=2012PLoSO...744657G |doi-access=free }}</ref>


== Види још ==
== Види још ==
* [[Таласна поткапина]]
* [[Таласна поткапина]]
* [[Марински процес]]
* [[Марински процес]]

== Референце ==
{{reflist}}


== Литература ==
== Литература ==
{{refbegin}}
{{Commonscat|Cliffs}}
* Марковић М., Павловић Р., Чупковић Т. 2003. ''Геоморфологија''. Београд: Завод за уџбенике и наставна средства
* Марковић М., Павловић Р., Чупковић Т. 2003. ''Геоморфологија''. Београд: Завод за уџбенике и наставна средства
* Мастило, Наталија (2005): ''Речник савремене српске географске терминологије'', Географски факултете, Београд
* Мастило, Наталија (2005): ''Речник савремене српске географске терминологије'', Географски факултете, Београд
* {{cite web | title = Catalogue of place names in northern East Greenland | publisher = Geological Survey of Denmark | url = https://data.geus.dk/geusmap/?mapname=stednavnedb#baslay=baseMapGl&optlay=&extent=549832.8357720698,8582739.868248867,622444.3190166993,8680765.370629115&layers=grl_geus_north_east_higgins_map,grl_ne_higgins_placenames,grl_ne_placenames&filter_1=txt_search.part%3D%26placename%3D&filter_2=txt_search.part%3D%26placename%3D | access-date = 20 September 2019}}
* {{cite web|title=Backpacking - Kootenay National Park|url=https://www.pc.gc.ca/en/pn-np/bc/kootenay/activ/arrierepays-backcountry|access-date=2020-09-23|publisher=National Park Service|url-status=live|archive-url=https://web.archive.org/web/20190929020835/https://www.pc.gc.ca/en/pn-np/bc/kootenay/activ/arrierepays-backcountry|archive-date=2019-09-29}}
* {{cite web|title=Geology Fieldnotes|url=http://www.nature.nps.gov/geology/parks/zion/index.cfm|access-date=2010-11-28|publisher=National Park Service|url-status=live|archive-url=https://web.archive.org/web/20130522020351/http://www.nature.nps.gov/geology/parks/zion/index.cfm|archive-date=2013-05-22}}
{{refend}}

== Спољашње везе ==
{{Commonscat|Cliffs}}
* {{Cite Americana|wstitle=Cliff |short=x}}

{{Authority control}}


[[Категорија:Марински процес]]
[[Категорија:Марински процес]]

Верзија на датум 26. новембар 2021. у 23:14

Клифови Мохера, пример литица у Ирској
The White Cliffs of Dover

Клиф (енгл. cliff) или литица је назив за стрму абразиону падину насталу приликом разарања високе основне обале под утицајем таласа. Настанак клифа инициран је маринским процесом, док, по механизму процеса, припада колувијалном процесу. Временом се повлачи на рачун мора и тако повећава ширину абразионе обалске терасе, која лежи у његовом подножју. Висина и нагиб клифа зависе од иницијалног рељефа, литолошког састава и склопа обале. Клифови често достижу висине и хектометарског реда величина, а њихов нагиб може бити скоро вертикалан. У случају ниских, заравњених обала, које су изграђене од меких и растреситих стена, клиф је готово неприметан у рељефу.

An escarpment (or scarp) is a type of cliff, formed by the movement of a geologic fault or landslides, or maybe by rock slides by falling rock which biologically changes the differential erosion of rock layers of selectioning or deforming hardness.

The far southwestern aspect of Nanga Parbat's Rupal face, highest cliff (rock wall/mountain face) in the world. The steepest part of the face is 2 km to the northeast.

Етимологија

The Trango Towers in Pakistan. Their vertical faces are the world's tallest cliffs. Trango Tower center; Trango Monk center left; Trango II far left; Great Trango right.
Europe's highest cliff, Troll Wall in Norway, a famous BASE jumping location for jumpers from around the world.

Cliff comes from the Old English word clif of essentially the same meaning, cognate with Dutch, Low German, and Old Norse klif 'cliff'.[1] These may in turn all be from a Romance loanword into Primitive Germanic that has its origins in the Latin forms clivus / clevus ("slope" or "hillside").[2][3]

Велике и познате литице

Vihren’s 460 m north face seen from Golemiya Kazan, Pirin Mountain, Bulgaria
Cliffs along the north shore of Isfjord, Svalbard, Norway.
Kaliakra cape cliffs, Bulgaria
The Matengai in Oki Islands, Japan
The Cliffs of Moher in Ireland
Cliffs on the western shoreline of Sam Ford Fjord, Canada
Cliffs near Sortavala, Russia
Close-up view of Verona Rupes, a 20 km high fault scarp on Miranda, a moon of Uranus.[4]
Vratsata gorge, Vrachanski Balkan Mountains, Bulgaria

Given that a cliff does not need to be exactly vertical, there can be ambiguity about whether a given slope is a cliff or not and also about how much of a certain slope to count as a cliff. For example, given a truly vertical rock wall above a very steep slope, one could count just the rock wall or the combination. Listings of cliffs are thus inherently uncertain.

Some of the largest cliffs on Earth are found underwater. For example, an 8,000 m drop over a 4,250 m span can be found at a ridge sitting inside the Kermadec Trench.

The highest very steep non-vertical cliffs in the world are Nanga Parbat's Rupal Face and Gyala Peri's southeast face, which both rise approximately 4,600 m, or 15,000 ft, above their base. According to other sources, the highest cliff in the world, about 1,340 m high, is the east face of Great Trango in the Karakoram mountains of northern Pakistan. This uses a fairly stringent notion of cliff, as the 1,340 m figure refers to a nearly vertical headwall of two stacked pillars; adding in a very steep approach brings the total drop from the East Face precipice to the nearby Dunge Glacier to nearly 2,000 m.

The location of the world's highest sea cliffs depends also on the definition of 'cliff' that is used. Guinness World Records states it is Kalaupapa, Hawaii,[5] at 1,010 m high. Another contender is the north face of Mitre Peak, which drops 1,683 m to Milford Sound, New Zealand.[6] These are subject to a less stringent definition, as the average slope of these cliffs at Kaulapapa is about 1.7, corresponding to an angle of 60 degrees, and Mitre Peak is similar. A more vertical drop into the sea can be found at Maujit Qaqarssuasia (also known as the 'Thumbnail') which is situated in the Torssukátak fjord area at the very tip of South Greenland and drops 1,560 m near-vertically.[7]

Списак

The following is an incomplete list of cliffs of the world.

Африка

Изнад мора

Изнад копна

  • Innumerable peaks in the Drakensberg mountains of South Africa are considered cliff formations. The Drakensberg Range is regarded, together with Ethiopia's Simien Mountains, as one of the two finest erosional mountain ranges on Earth. Because of their near-unique geological formation, the range has an extraordinarily high percentage of cliff faces making up its length, particularly along the highest portion of the range. This portion of the range is virtually uninterrupted cliff faces, ranging from 600 m (2.000 ft) to 1.200 m (3.900 ft) in height for almost 250 km (160 mi). Of all, the "Drakensberg Amphitheatre" (mentioned above) is most well known. Other notable cliffs include the Trojan Wall, Cleft Peak, Injisuthi Triplets, Cathedral Peak, Monk's Cowl, Mnweni Buttress, etc. The cliff faces of the Blyde River Canyon, technically still part of the Drakensberg, may be over 800 m (2.600 ft), with the main face of the Swadini Buttress approximately 1.000 m (3.300 ft) tall.
    • Drakensberg Amphitheatre, South Africa 1.200 m (3.900 ft) above base, 5 km (3,1 mi) long. The Tugela Falls, the world's second tallest waterfall, falls 948 m (3.110 ft) over the edge of the cliff face.
  • Karambony, Madagascar, 380 m (1.250 ft) above base.
  • Mount Meru, Tanzania Caldera Cliffs, 1.500 m (4.900 ft)
  • Tsaranoro, Madagascar, 700 m (2.300 ft) above base

Америка

Север

Mount Thor, Baffin Island, Nunavut, Canada, commonly regarded as the highest vertical drop on Earth
Southwest face of El Capitan from Yosemite Valley

Several big granite faces in the Arctic region vie for the title of 'highest vertical drop on Earth', but reliable measurements are not always available. The possible contenders include (measurements are approximate):

Mount Thor, Baffin Island, Canada; 1,370 m (4,500 ft) total; top 480 m (1600 ft) is overhanging. This is commonly regarded as being the largest vertical drop on Earth[2] са 1,250 m (4,100 ft).

  1. The sheer north face of Polar Sun Spire, in the §74:MTAtoFa

of Baffin Island, rises 4,300 ft above the flat frozen fjord, although the lower portion of the face breaks from the vertical wall with a series of ledges and buttresses.[8]

  1. Ketil's and its neighbor Ulamertorsuaq's west faces in Tasermiut, Greenland have been reported as over 1,000 m high.[9][10][11] Another relevant cliff in Greenland is Agdlerussakasit's Thumbnail.[12]

Хабитат

Cliff landforms provide unique habitat niches to a variety of plants and animals, whose preferences and needs are suited by the vertical geometry of this landform type. For example, a number of birds have decided affinities for choosing cliff locations for nesting,[13] often driven by the defensibility of these locations as well as absence of certain predators.

Флора

The population of the rare Borderea chouardii, during 2012, existed only on two cliff habitats within western Europe.[14]

Види још

Референце

  1. ^ Oxford English Dictionary, 1971
  2. ^ а б Monika Buchmüller-Pfaff: Namen im Grenzland - Methoden, Aspekte und Zielsetzung in der Erforschung der lothringisch-saarländischen Toponomastik, Francia 18/1 (1991), Francia-Online: Sex nstitut historique allemand de Paris - Deutsches Historisches Institut Paris: Onlineressource Архивирано 2015-01-29 на сајту Wayback Machine
  3. ^ Max Pfister: Altromanische Relikte in der östlichen und südlichen Galloromania, in den rheinischen Mundarten, im Alpenraum und in Oberitalien. In : Sieglinde Heinz, Ulrich Wandruszka [ed.]: Fakten und Theorien : Beitr. zur roman. u. allg. Sprachwiss.; Festschr. für Helmut Stimm zum 65. Geburtstag, Tübingen 1982, pp. 219 – 230, ISBN 3-87808-936-8
  4. ^ „Natural world: the solar system: highest cliffs”. Guinness World Records. Архивирано из оригинала 2006-05-21. г. Приступљено 2014-11-16. 
  5. ^ „Highest Cliffs”. Guinness World Records. Архивирано из оригинала 2005-11-27. г. Приступљено 2006-05-02. 
  6. ^ Lück, Michael (2008). The Encyclopedia of Tourism and Recreation in Marine Environments By Michael Lück. ISBN 9781845933500. Архивирано из оригинала 2017-12-06. г. Приступљено 2009-08-01. 
  7. ^ „Planet Fear”. Архивирано из оригинала 2012-03-26. г. Приступљено 2009-08-04. 
  8. ^ „Polar Sun Spire”. SummitPost.Org. Архивирано из оригинала 2008-12-02. г. Приступљено 2008-07-31. 
  9. ^ „Climbing in Tasermiut”. bigwall.dk. Архивирано из оригинала 2008-12-05. г. Приступљено 2008-09-02. 
  10. ^ „The American Alpine Journal” (PDF). 1986. Архивирано из оригинала (PDF) 28. 10. 2008. г. Приступљено 2008-09-02. 
  11. ^ The Summer 1998 Slovak Expedition to Greenland (Jamesák International) Архивирано 2016-03-04 на сајту Wayback Machine
  12. ^ Jon Roberts: Agdlerussakasit (1750 m), east face, new route on east face; The Butler (900 m) and Mark (900 m), first ascents. American Alpine Journal (AAJ) 2004, pp. 266–267
  13. ^ C.Michael Hogan. 2010. Abiotic factor. Encyclopedia of Earth. eds Emily Monosson and C. Cleveland. National Council for Science and the Environment Архивирано јун 8, 2013 на сајту Wayback Machine. Washington DC
  14. ^ González, García; Begoña, María; Espadaler, X; Olesen, Jens M (12. 9. 2012). Bente Jessen Graae, ур. „Extreme Reproduction and Survival of a True Cliffhanger: The Endangered Plant Borderea chouardii (Dioscoreaceae)”. PLOS ONE. digital.csic.es: Public Library of Science. 7 (9): e44657. Bibcode:2012PLoSO...744657G. PMC 3440335Слободан приступ. PMID 22984539. doi:10.1371/journal.pone.0044657Слободан приступ. Приступљено 7. 6. 2021 — преко CORE. 

Литература

  • Марковић М., Павловић Р., Чупковић Т. 2003. Геоморфологија. Београд: Завод за уџбенике и наставна средства
  • Мастило, Наталија (2005): Речник савремене српске географске терминологије, Географски факултете, Београд
  • „Catalogue of place names in northern East Greenland”. Geological Survey of Denmark. Приступљено 20. 9. 2019. 
  • „Backpacking - Kootenay National Park”. National Park Service. Архивирано из оригинала 2019-09-29. г. Приступљено 2020-09-23. 
  • „Geology Fieldnotes”. National Park Service. Архивирано из оригинала 2013-05-22. г. Приступљено 2010-11-28. 

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