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== Geography and climate == [[File:Korea-Gyeongju-Seokguram-13.jpg|thumb|alt=A distant view of a wooden shrine surrounded by a thick forest on the slopes of a mountain in autumn.|[[Seokguram]] grotto on the slopes of [[Tohamsan]]<ref>Kang and Lee (2006), p.59</ref>]] Gyeongju lies in the southeastern corner of North Gyeongsang Province, and is bounded by the metropolitan city of [[Ulsan]] on the south. Within the province, its neighbors include [[Pohang]] on the north, [[Cheongdo County]] on the southwest, and [[Yeongcheon]] on the northwest.<ref name="EncyKorea Gyeongju 1" /> Gyeongju is located about {{convert|50|km|mi|sp=us}} north of [[Busan]].<ref name="Xinhua" /> To the east, it has no neighbor but the sea.<ref name="EncyKorea Gyeongju 1" /> Most of Gyeongju lies in the [[Gyeongsang Basin]], but a few areas of the city belong to the [[Pohang Basin]], such as Eoil-ri and Beomgok-ri in [[Yangbuk-myeon]], and part of [[Cheonbuk-myeon, Gyeongju|Cheonbuk-myeon]]. The Gyeongsang Basin areas consist of Bulguksa intrusive rock penetrating layers of [[sedimentary rock]]s, mainly [[granite]] and [[Porphyry (geology)|porphyry]]. By contrast, the Pohang Basin areas are made up of [[stratum]] that formed in the [[Tertiary]] period of the [[Cenozoic era]], which consists of [[igneous rock]], [[aqueous rock]], porphyry, [[sandstone]], and [[tuff]].<ref name="Encyber City">{{cite web |url=http://www.encyber.com/search_w/ctdetail.php?masterno=11233&contentno=11233 |title=경주시 Gyeongju-si 慶州市 |publisher=[[Doosan Encyclopedia]] |language=ko |access-date=2009-08-08 }}{{dead link|date=September 2017 |bot=InternetArchiveBot |fix-attempted=yes }}</ref> Low mountains are widespread throughout Gyeongju. The highest of these are the [[Taebaek Mountains]], which run along the city's western border. Gyeongju's highest point, [[Munboksan]] ({{Korean|hangul=문복산|labels=no}}), is {{convert|1015|m|ft|sp=us}} above [[sea level]]. This peak lies in [[Sannae-myeon, Gyeongju|Sannae-myeon]], on the border with [[Cheongdo County|Cheongdo]].<ref>{{cite web|url=http://100.nate.com/dicsearch/pentry.html?s=K&i=237482&v=43 |script-title=ko:문복산 (文福山) |trans-title=Munbok Mountain (''Munboksan'') |publisher=Nate / Encyclopedia of Korean Culture |language=ko |access-date=2009-08-05 |url-status=dead |archive-url=https://web.archive.org/web/20110610054032/http://100.nate.com/dicsearch/pentry.html?s=K&i=237482&v=43 |archive-date=2011-06-10 }}</ref> East of the Taebaek range, other western peaks such as Danseok Mountain lie within the [[Jusa Mountains|Jusa]] subrange.<ref>{{cite web|url=http://100.nate.com/dicsearch/pentry.html?i=234633 |script-title=ko:경주부산성 (慶州富山城) |trans-title=Gyeongju Busanseong |publisher=Nate / Encyclopedia of Korean Culture |language=ko |access-date=2009-08-05 |url-status=dead |archive-url=https://web.archive.org/web/20110610054221/http://100.nate.com/dicsearch/pentry.html?i=234633 |archive-date=2011-06-10 }}</ref> The city's eastern peaks, including [[Tohamsan]], belong to the Haean Mountains and [[Dongdae Mountains]].<ref>{{cite web|url=http://100.nate.com/dicsearch/pentry.html?s=K&i=244809&v=44 |script-title=ko:토함산 (吐含山 ) |trans-title=Toham Mountain (''Tohamsan'') |publisher=Nate / Encyclopedia of Korean Culture |language=ko |access-date=2009-08-05 |url-status=dead |archive-url=https://web.archive.org/web/20110610054236/http://100.nate.com/dicsearch/pentry.html?s=K&i=244809&v=44 |archive-date=2011-06-10 }}</ref><ref>{{cite web |url=http://www.encyber.com/search_w/ctdetail.php?masterno=109267&contentno=109267 |script-title=ko:양북면 Yangbuk-myeon 陽北面 |publisher=[[Doosan Encyclopedia]] |language=ko |access-date=2009-08-05 }}{{dead link|date=September 2017 |bot=InternetArchiveBot |fix-attempted=yes }}</ref> [[File:Korea-Gyeongju-Map of mountains and drainage-02.png|thumb|alt=A river runs from south to north through the region, draining most of it. Half the tallest mountains are on the southern border; other mountains are mostly in the west, clustered in the northwest.|Principal mountains and drainage patterns of Gyeongju. Mountains of {{convert|500|to|700|m|ft|abbr=on}} are in green, those taller than {{convert|700|m|ft|abbr=on}} in violet. The rest three in gray are under {{convert|500|m|ft|abbr=on}}.]] Gyeongju's drainage patterns are shaped by these lines of mountains.<ref name="EncyKorea Nature" /> The Dongdae Mountains divide a narrow foothills area on their east, and various internal river systems to the west. Most of the city's interior is drained by the small [[Hyeongsan River]], which flows north from Ulsan and meets the sea at Pohang Harbor. The Hyeongsan's chief tributaries include the Bukcheon and Namcheon, which join it in [[Gyeongju Basin]].<ref name="EncyKorea Nature" /> The southwestern corner of Gyeongju, on the far side of the Taebaek range, drains into the [[Geumho River]], which then flows into the [[Nakdong River|Nakdong]]. A small area of the south, just west of the Dongdae range, drains into the [[Taehwa River]], which flows into the Bay of Ulsan.<ref>{{cite web|url=http://100.nate.com/dicsearch/pentry.html?i=244800 |script-title=ko:태화강 (太和江) |trans-title=Taehwa River |publisher=Nate / Encyclopedia of Korean Culture |language=ko |access-date=2009-08-05 |url-status=dead |archive-url=https://web.archive.org/web/20110610054300/http://100.nate.com/dicsearch/pentry.html?i=244800 |archive-date=2011-06-10 }}</ref><ref>{{cite web|url=http://100.nate.com/dicsearch/pentry.html?i=247864 |script-title=ko:형산강지구대 (兄山江地溝帶) |trans-title=Hyeongsan River Rift Valley |publisher=Nate / Encyclopedia of Korean Culture |language=ko |access-date=2009-08-05 |url-status=dead |archive-url=https://web.archive.org/web/20110610054318/http://100.nate.com/dicsearch/pentry.html?i=247864 |archive-date=2011-06-10 }}</ref> The Gyeongju coastline runs for {{convert|36.1|km|mi|sp=us}} between [[Pohang]] in the north and [[Ulsan]] in the south.<ref name="2008 Tonggye 2">{{cite web |url=http://gyeongju.go.kr/administrative/administrative/tonggye2008/2.pdf |archive-url=https://www.webcitation.org/5iEKQTnlY?url=http://gyeongju.go.kr/administrative/administrative/tonggye2008/2.pdf |url-status=dead |archive-date=2009-07-13 |script-title=ko:2008년도 경주시 통계연보 : 2.토지 및 기후 |trans-title=Statistical yearbook of Gyeongju 2008 : 2. Land and weather |publisher=Gyeongju City |date=August 2008 |access-date=2009-07-13 }}</ref> There are no islands or large bays, only the small [[Alcove (architecture)|indentations]] made by the small streams flowing off the Dongdae ridgeline. Because of this, the city has no significant ports, though there are 12 small harbors.<ref name="gyeongju1">{{cite web|url=http://www.gyeongju.go.kr/industry/agriculture/info.asp?main=5&sub=1&cor=5|archive-url=https://web.archive.org/web/20110613162052/http://www.gyeongju.go.kr/industry/agriculture/info.asp?main=5&sub=1&cor=5|url-status=dead|archive-date=2011-06-13|work=Gyeongju City website|script-title=ko:농축수산 |trans-title=Agriculture, Livestock industry, and Fisheries |access-date=2009-07-07 |language=ko}}</ref> One such harbor in Gyeongju's southeast corner is home to the Ulsan base of the National Maritime Police. This base is responsible for security over a wide area of South Korea's east-central coast.<ref>{{cite web|url=http://coast.kcg.go.kr/english/intro/greet.asp |title=Greeting |publisher=The National Maritime Police |access-date=2009-08-05 |url-status=dead |archive-url=https://web.archive.org/web/20090328044837/http://coast.kcg.go.kr/english/intro/greet.asp |archive-date=March 28, 2009 }}</ref><ref>{{cite web|author=Lee, Gil-Beom |date=2009-03-09|url=http://coast.kcg.go.kr/english/sea/diff_send.asp |title=Main Operations |publisher=The National Maritime Police|access-date=2009-08-05|archive-url=https://web.archive.org/web/20090621224746/http://coast.kcg.go.kr/english/sea/diff_send.asp <!--Added by H3llBot-->|archive-date=2009-06-21}}</ref><ref>{{cite web|url=http://ulsan.kcg.go.kr/intro/intro.asp |script-title=ko:경찰서소개 |trans-title=Introduction of the police |publisher=Ulsan Coast Guard, Korea |access-date=2009-08-05 |quote={{lang|ko|울산광역시 북구 신명동으로부터 부산광역시 기장군 공수리까지 해안선과 어업자원보호선을 연결한 해역}} |language=ko |url-status=dead |archive-url=https://web.archive.org/web/20050207121709/http://ulsan.kcg.go.kr/intro/intro.asp |archive-date=February 7, 2005 }}</ref> ===Climate=== Gyeongju has a cooler version of a [[humid subtropical climate]] ([[Köppen climate classification|Köppen]]: ''Cfa''). Due to its coastal location, Gyeongju has a slightly milder climate than the more inland regions of Korea. In general, however, the city's climate is typical of South Korea. It has hot summers and cool winters, with a [[monsoon]] season between late June and early August. As on the rest of Korea's east coast, autumn [[typhoon]]s are not uncommon. The average annual rainfall is {{convert|1091|mm|in|sp=us|1}}, and the average annual high temperatures range from {{convert|8.6|-|31.1|°C|°F|0}}.<ref>{{cite web|url=http://www.gyeongju.go.kr/inFrame.asp?how_chk=&hdnPage=&Kwa01Code=&s_sy=&s_sm=&s_ey=&s_em=&SearchType=&SearchString=&reqNum=&vDiscrNo=&name=&result=&discrHash=&PCODE=A0105&main=1&sub=5 |archive-url=https://web.archive.org/web/20110613162102/http://www.gyeongju.go.kr/inFrame.asp?how_chk=&hdnPage=&Kwa01Code=&s_sy=&s_sm=&s_ey=&s_em=&SearchType=&SearchString=&reqNum=&vDiscrNo=&name=&result=&discrHash=&PCODE=A0105&main=1&sub=5 |url-status=dead |archive-date=2011-06-13 |publisher=Gyeongju City website|script-title=ko:위치와 자연지리 |trans-title=Location and geography |access-date=2009-07-13 |language=ko}}</ref> Gyeongju's historic city center lies on the banks of the Hyeongsan in Gyeongju Basin. This low-lying area has been subject to repeated [[flood]]ing throughout recorded history, often as a result of typhoons. On average, chronicles report a major flood every 27.9 years, beginning in the 1st century.<ref>Kang (2002), p. 6.</ref> Modern flood control mechanisms brought about a dramatic reduction in flooding in the later 20th century. The last major flood occurred in 1991, when the Deokdong Lake reservoir overflowed due to [[1991 Pacific typhoon season#Typhoon Gladys|Typhoon Gladys]].<ref>Kang (2002), p. 5.</ref> {{Weather box | location = Gyeongju (2011–2020 normals, extremes 2010–present) | metric first = Y | single line = Y | Jan record high C = 16.8 | Feb record high C = 24.2 | Mar record high C = 26.6 | Apr record high C = 32.5 | May record high C = 36.2 | Jun record high C = 36.5 | Jul record high C = 39.7 | Aug record high C = 39.8 | Sep record high C = 35.1 | Oct record high C = 31.5 | Nov record high C = 29.4 | Dec record high C = 19.3 | year record high C = 39.8 | Jan high C = 5.9 | Feb high C = 8.4 | Mar high C = 14.4 | Apr high C = 19.7 | May high C = 25.7 | Jun high C = 27.7 | Jul high C = 30.6 | Aug high C = 31.4 | Sep high C = 26.2 | Oct high C = 21.6 | Nov high C = 15.3 | Dec high C = 7.7 | year high C = 19.6 | Jan mean C = 0.3 | Feb mean C = 2.3 | Mar mean C = 7.4 | Apr mean C = 12.7 | May mean C = 18.4 | Jun mean C = 21.9 | Jul mean C = 25.4 | Aug mean C = 25.9 | Sep mean C = 20.5 | Oct mean C = 14.8 | Nov mean C = 8.7 | Dec mean C = 1.9 | year mean C = 13.4 | Jan low C = -4.7 | Feb low C = -3.1 | Mar low C = 1.0 | Apr low C = 6.0 | May low C = 11.7 | Jun low C = 17.0 | Jul low C = 21.4 | Aug low C = 21.9 | Sep low C = 16.2 | Oct low C = 9.3 | Nov low C = 3.0 | Dec low C = -3.2 | year low C = 8.0 | Jan record low C = -14.7 | Feb record low C = -13.4 | Mar record low C = -6.6 | Apr record low C = -3.0 | May record low C = 1.9 | Jun record low C = 10.2 | Jul record low C = 14.9 | Aug record low C = 14.0 | Sep record low C = 7.0 | Oct record low C = -0.6 | Nov record low C = -6.6 | Dec record low C = -11.7 | year record low C = -14.7 | precipitation colour = green | Jan precipitation mm = 32.2 | Feb precipitation mm = 30.8 | Mar precipitation mm = 59.7 | Apr precipitation mm = 96.1 | May precipitation mm = 55.3 | Jun precipitation mm = 100.6 | Jul precipitation mm = 190.1 | Aug precipitation mm = 191.9 | Sep precipitation mm = 194.1 | Oct precipitation mm = 108.2 | Nov precipitation mm = 37.8 | Dec precipitation mm = 24.4 | year precipitation mm = 1121.2 | unit precipitation days = 0.1 mm | Jan precipitation days = 5.1 | Feb precipitation days = 6.8 | Mar precipitation days = 7.6 | Apr precipitation days = 9.8 | May precipitation days = 7.7 | Jun precipitation days = 9.6 | Jul precipitation days = 12.8 | Aug precipitation days = 13.7 | Sep precipitation days = 12.2 | Oct precipitation days = 6.7 | Nov precipitation days = 6.8 | Dec precipitation days = 5.4 | year precipitation days = | Jan humidity = 52.6 | Feb humidity = 56.7 | Mar humidity = 58.3 | Apr humidity = 60.3 | May humidity = 63.5 | Jun humidity = 72.6 | Jul humidity = 78.4 | Aug humidity = 79.8 | Sep humidity = 81.3 | Oct humidity = 75.1 | Nov humidity = 67.5 | Dec humidity = 56.3 | year humidity = 66.9 | Jan sun = 197.2 | Feb sun = 179.1 | Mar sun = 226.7 | Apr sun = 218.8 | May sun = 240.0 | Jun sun = 182.1 | Jul sun = 162.9 | Aug sun = 180.9 | Sep sun = 147.5 | Oct sun = 178.5 | Nov sun = 161.8 | Dec sun = 186.2 | year sun = 2261.7 | source = [[Korea Meteorological Administration]]<ref name= KMA> {{cite web | archive-url = https://web.archive.org/web/20220129211110/https://data.kma.go.kr/resources/normals/pdf_data/korea_pdf_0106_v2.pdf | archive-date = 29 January 2022 | url = https://data.kma.go.kr/resources/normals/pdf_data/korea_pdf_0106_v2.pdf | title = Climatological Normals of Korea (1991 ~ 2020) | publisher = Korea Meteorological Administration | access-date = 7 June 2023 | language = ko}}</ref><ref name= KMAextremes> {{cite web | url = https://data.kma.go.kr/climate/extremum/selectExtremumList.do?pgmNo=103 | publisher = Korea Meteorological Administration | access-date = 4 April 2022 | script-title = ko:순위값 - 구역별조회 | language = ko}}</ref> }}
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