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{{Other places}} {{Other places}}
{{Infobox settlement {{Infobox Turkey place
| type = municipality
<!-- See Template:Infobox settlement for additional fields and descriptions -->
| name = Gümüşhane | name = Gümüşhane
| other_name =
|settlement_type = ]
| image_skyline = Gümüşhane Genel.JPG | image_skyline = Gümüşhane Genel.JPG
| image_caption = Gümüşhane | image_caption = View of Gümüşhane
| image_shield = | image_shield =
| coordinates = {{coord|40|27|35|N|39|28|40|E|display=inline,title}}
| pushpin_map = Turkey
| coordinates = {{coord|40|27|35|N|39|28|40|E|display=inline,title}} | province = Gümüşhane
| subdivision_type = Country | district = Gümüşhane
| leader_party = ]
| subdivision_name = Turkey
| subdivision_type1 = ] | leader_name = Vedat Soner Başer
| area_footnotes =
| subdivision_name1 = ]
| subdivision_type2 = | area_total_km2 =
| subdivision_name2 = | elevation_m = 1153
| population_footnotes = <ref name=tuik/>
| leader_party = ]
| leader_title = Mayor | population_total = 39214
| leader_name = Ercan Çimen | population_as_of = 2022
| leader_title1 = ] | postal_code = 29830
| leader_name1 = | area_code = 0456
| area_footnotes = {{Turkey district areas|SOURCE}} | website = {{url|https://www.gumushane.bel.tr/}}
| area_blank1_title = District
| area_blank1_km2 = {{Turkey district areas|Gümüşhane|Gümüşhane}}
| elevation_m = 1153
| population_footnotes = {{Turkey district populations|SOURCE|Gümüşhane}}
| population_urban = {{Turkey district populations|Gümüşhane|Gümüşhane|şehir}}
| population_as_of = {{Turkey district populations|YEAR}}
| population_blank1_title = District
| population_blank1 = {{Turkey district populations|Gümüşhane|Gümüşhane|toplam}}
| population_density_blank1_km2 = auto
| postal_code_type =
| postal_code =
| website = {{URL| www.gumushane.bel.tr | www.gumushane.bel.tr }}
}} }}
'''Gümüşhane''' or '''Gyumushkhana''' ({{IPA-tr|ɟyˈmyʃhaːne|lang|GumushanePron.ogg}}, ''Argyrópolis'' or ''Arghyropolis'', {{lang|grc|Αργυρόπολις}} in ]) is a city and the capital district of ] in the ] region of Turkey. The city lies along the ], at an elevation of {{Convert|5000|ft|m|abbr=out}}, about {{Convert|40|mi|km|abbr=out}} southwest of Trabzon. According to the 2010 census, population of Gümüşhane urban center is 28,620.<ref name="die">{{dead link|date=October 2017 |bot=InternetArchiveBot |fix-attempted=yes }}</ref> The district covers an area of {{convert|1789|km2|sqmi|0|abbr=on}},<ref>{{cite web|url=http://www.statoids.com/ytr.html|title=Statistical information on districts of Turkey|access-date=2008-12-01|author=Statoids}}</ref> and the city lies at an elevation of {{convert|1153|m|ft|0|abbr=on}}. Coordinates on world : 40°27′35″N 39°28′40″E '''Gümüşhane''' ({{IPA|tr|ɟyˈmyʃhaːne|lang|GumushanePron.ogg}}) is a city in the ] of Turkey. It is the seat of ] and ].<ref name=il>, Turkey Civil Administration Departments Inventory. Retrieved 1 March 2023.</ref> Its population is 39,214 (2022).<ref name=tuik>{{Cite web |title=Address-based population registration system (ADNKS) results dated 31 December 2022, Favorite Reports|url=https://biruni.tuik.gov.tr/medas/?kn=95&locale=en |access-date=13 March 2023|publisher=]|language=en|format=XLS}}</ref> The city lies along the ], about {{Convert|40|mi|km|abbr=out}} southwest of Trabzon. The city lies at an elevation of {{convert|1153|m|ft|0|abbr=on}}.


==History== ==History==
It is suggested that the ancient Thia ({{lang|grc|Θεία}} in ], a settlement of ], Late Roman and ] periods) was located {{convert|4|mi|abbr=on}} west of modern Gümüşhane, in modern Beşkilise. In the Byzantine period, there was a town named ''Tzanicha'' or ''Tzantzakon'' ({{lang|grc|Τζάνιχα, Τζάντζακον}} in ]) means land of Zan / Laz people, possibly located {{Convert|2|mi|km|abbr=out}} to the west of Gümüşhane.<ref>Barrington Atlas of the Greek and Roman World: Map by Map directory, p.1237.</ref><ref>], ''Περί Κτισμάτων'', .</ref>
]
]
]
]
It is suggested that the ancient Thia ({{lang|grc|Θεία}} in ], a settlement of ], Late Roman and ] periods) was located 4 miles west of modern Gümüşhane, in modern Beşkilise. In Byzantine period, there was a town named ''Tzanicha'' or ''Tzantzakon'' ({{lang|grc|Τζάνιχα, Τζάντζακον}} in ]) means land of Zan / Laz people, possibly located {{Convert|2|mi|km|abbr=out}} to the west of Gümüşhane.<ref>Barrington Atlas of the Greek and Roman World: Map by Map directory, p.1237.</ref><ref>], ''Περί Κτισμάτων'', .</ref>


Around 840 AD, the area was included in the new Roman (Byzantine) province of Chaldia (Χαλδία).{{sfn|Kiminas|2009|pp=105}} It was later ruled by the Byzantine ]. Around 840 AD, the area was included in the new Roman (Byzantine) province of ] (Χαλδία).{{sfn|Kiminas|2009|pp=105}} It was later ruled by the Byzantine ].


During Ottoman years, the ] of Gümüşhane fell under the administration successively ], ] and Trabzon Province, and was divided into four kazas: Gümüşhane, Torul (capital city Ardassa), Şiran (Cheriana), and Kelkit (Keltik). During the Ottoman years, the ] of Gümüşhane fell under the administration successively of ], ] and Trabzon Province, and was divided into four kazas: Gümüşhane, Torul (capital city Ardassa), Şiran (Cheriana), and Kelkit (Keltik).


The sanjak in which Gümüşhane was situated at some stage comprised 37 mines of argentiferous lead and six copper mines{{citation needed|date=May 2015}}. There is no evidence that these mines were in use during Byzantine times. The sanjak in which Gümüşhane was situated at some stage comprised 37 mines of argentiferous lead and six copper mines.{{citation needed|date=May 2015}} There is no evidence that these mines were in use during Byzantine times.


As for the name of the city during the Ottoman period, Greek-speaking population was also using the name Gümüşhane (Γκιμισχανά and Κιουμουσχανά) but, in the first decades of 19th century, the hellenized form ''Argyrópolis'' (Αργυρόπολις, from ''argyros'' "silver" and ''polis'' "city") was established.<ref>Terezakis Yorgos, , Encyclopaedia of the Hellenic world, Asia Minor.</ref> As for the name of the city during the Ottoman period, Greek-speaking population was also using the name Gümüşhane (Γκιμισχανά and Κιουμουσχανά) but, in the first decades of the 19th century, the ] name '''Argiroupoli''' (Αργυρόπολις, from ''argyros'' "silver" and ''polis'' "city") was used.<ref>Terezakis Yorgos, , Encyclopaedia of the Hellenic world, Asia Minor.</ref> After the population exchange of 1923 many of the ] inhabitants moved to the ] in ], ].

The Arghyropolis belonged to the ] of Chaldie (145 communities, 77,845 inhabitants). During the ], the Turkish authorities boycott the Christians. The boycott deprived the Christians of all they possessed and reduced them to absolute poverty. The organizer of the boycott was the Djemal Azmi, Vali of Trebizonde, under whose orders were the Governor of Arghyropolis and others. In the sterile region of Argliyropolis the distress was great, because the inhabitants were entirely dependent for their existence on their local trade, and that from Russia. General mobilization was also among the causes conducive to the ruin of the Greek speaking communities, for the male inhabitants who supported their families were taken away from their homes. The Turkish officers treated the Greek speaking population in a brutal way, making many Greekophones to desert. This was the situation before the ].<ref name="Persecution_of_the_Greeks_in_Turkey_1914_1918">{{cite book| title = Persecution of the Greeks in Turkey, 1914-1918| url = https://archive.org/details/persecutionofgre00consrich| publisher = Constantinople |date=1919}}</ref>

The Russian advance gave rise to a fresh outburst of fanaticism against the Greek element, the Turks from Turkish villages plundered the Christian villages of the region. During the Turkish retreat, the Turks pillaged many Greekophone villages of the region, the inhabitants took to the mountains and their property was plundered. Later on the retreat of the Russians, the Turks
returned and the few inhabitants that remained in these villages, deprived of all resources and left to die of hunger.<ref name="Persecution_of_the_Greeks_in_Turkey_1914_1918"/>


==Geography== ==Geography==
]
]
Gümüşhane is surrounded by high mountains, Zigana-Trabzon Mountains to the north, Çimen Mountains to the south, ] Mountains to the west and Pulur, Soğanlı Mountains to the east. Trekking is popular sport is at these mountains. ] has a ski center on it and it is a well known tourist destination for winter sports. Abdal Musa Peak (3331 m.) is the highest peak within it. The main trees in the forests are Scotch pine and fir, and there are many animals and birds in the area. There are many lakes such as Karanlık Göl, Beş Göller, Artebel Gölü, Kara Göller which are at the peak of ], and are preserved as natural parks. All these mountains compose 56% of the area of Gümüşhane province. Gümüşhane is surrounded by high mountains, Zigana-Trabzon Mountains to the north, Çimen Mountains to the south, ] Mountains to the west and Pulur, Soğanlı Mountains to the east. Trekking is popular sport is at these mountains. ] has a ski center on it and it is a well known tourist destination for winter sports. Abdal Musa Peak (3331 m.) is the highest peak within it. The main trees in the forests are Scotch pine and fir, and there are many animals and birds in the area. There are many lakes such as Karanlık Göl, Beş Göller, Artebel Gölü, Kara Göller which are at the peak of ], and are preserved as natural parks. All these mountains compose 56% of the area of Gümüşhane province.


===Climate=== ===Climate===
Gümüşhane has a ] (]: ''Dsb'' on the border ''Dfb'') with cold and snowy winters and warm summers. In the height of summer; July and August, temperatures at midday usually surpass 28&nbsp;°C, summer nights tend to become very cool due to the high elevation of Gümüşhane, and in winter temperatures usually plummet to -10&nbsp;°C and even go as low as -20&nbsp;°C occasionally. Gümüşhane has a ] (]: ''Dsb,'' bordering ''Dfb,'' or ]: ''Dc'') with cold and snowy winters and warm summers. In the height of summer; July and August, temperatures at midday usually surpass 28&nbsp;°C, summer nights tend to become very cool due to the continentality of Gümüşhane, and in winter temperatures usually plummet to -10&nbsp;°C and even go as low as -20&nbsp;°C occasionally.


Highest recorded temperature:{{Convert|41.1|C|F|abbr=on}} on 2 August 2017<br>Lowest recorded temperature:{{Convert|-25.7|C|F|abbr=on}} on 22 February 1985<ref>{{Cite web |url=https://www.mgm.gov.tr/veridegerlendirme/il-ve-ilceler-istatistik.aspx?k=A&m=GUMUSHANE |access-date=28 August 2024 |title=İllerimize Ait Genel İstatistik Verileri |website=mgm.gov.tr |publisher=Meteoroloji Genel Müdürlüğü |no-pp=y |language=Turkish}}</ref>
{{Weather box |metric first= Yes |single line= Yes |location= Gümüşhane (Averages: 1961-2012, Records: 1961-2018)

|Jan record high C= 14.8
{{Weather box
|Feb record high C= 18.0
|metric first= Yes
|Mar record high C= 24.0
|single line= Yes
|Apr record high C= 29.0
|collapsed = y
|May record high C= 32.6
|location= Gümüşhane (1991–2020, extremes 1961–2023)
|Jun record high C= 36.2
|Jul record high C= 41.0 | Jan record high C = 15.5
|Aug record high C= 41.1 | Feb record high C = 18.0
|Sep record high C= 37.0 | Mar record high C = 24.0
|Oct record high C= 32.0 | Apr record high C = 29.0
|Nov record high C= 22.1 | May record high C = 34.4
|Dec record high C= 19.2 | Jun record high C = 36.2
|Jan high C= 2.6 | Jul record high C = 41.0
|Feb high C= 4.8 | Aug record high C = 41.1
|Mar high C= 9.6 | Sep record high C = 37.7
|Apr high C= 16.1 | Oct record high C = 32.0
|May high C= 21.1 | Nov record high C = 22.3
|Jun high C= 24.8 | Dec record high C = 19.2
|Jul high C= 28.0 | year record high C = 41.1
|Aug high C= 28.5 | Jan high C = 3.4
|Sep high C= 25.2 | Feb high C = 5.7
|Oct high C= 18.7 | Mar high C = 10.3
|Nov high C= 10.5 | Apr high C = 16.2
|Dec high C= 4.9 | May high C = 21.2
|Jan mean C = -1.8 | Jun high C = 25.4
|Feb mean C = -0.7 | Jul high C = 28.7
|Mar mean C = 3.6 | Aug high C = 29.5
|Apr mean C = 9.4 | Sep high C = 25.6
|May mean C = 13.7 | Oct high C = 19.5
|Jun mean C = 17.2 | Nov high C = 10.7
|Jul mean C = 20.2 | Dec high C = 5.2
|Aug mean C = 20.1 | year high C = 16.8
|Sep mean C = 16.6 | Jan mean C = -1.4
|Oct mean C = 11.4 | Feb mean C = -0.2
|Nov mean C = 5.0 | Mar mean C = 4.0
|Dec mean C = 0.5 | Apr mean C = 9.2
|Jan low C= -5.8 | May mean C = 13.6
|Feb low C= -5.3 | Jun mean C = 17.3
|Mar low C= -1.4 | Jul mean C = 20.3
|Apr low C= 3.7 | Aug mean C = 20.6
|May low C= 7.5 | Sep mean C = 16.8
|Jun low C= 10.6 | Oct mean C = 11.8
|Jul low C= 13.7 | Nov mean C = 4.9
|Aug low C= 13.6 | Dec mean C = 0.6
|Sep low C= 9.9 | year mean C = 9.8
|Oct low C= 5.8 | Jan low C = -5.2
|Nov low C= 0.7 | Feb low C = -4.8
|Dec low C= -3.2 | Mar low C = -0.9
|Jan record low C= -23.6 | Apr low C = 3.4
|Feb record low C= -25.7 | May low C = 7.4
|Mar record low C= -22.6 | Jun low C = 10.9
|Apr record low C= -11.0 | Jul low C = 13.8
|May record low C= -2.8 | Aug low C = 14.2
|Jun record low C= 1.8 | Sep low C = 10.3
|Jul record low C= 4.5 | Oct low C = 6.3
|Aug record low C= 4.9 | Nov low C = 0.5
|Sep record low C= -1.0 | Dec low C = -3.0
|Oct record low C= -4.8 | year low C = 4.4
|Nov record low C= -15.0 | Jan record low C = -23.6
|Dec record low C= -21.0 | Feb record low C = -25.7
| Mar record low C = -22.6
|Jan precipitation days= 11.2
| Apr record low C = -11.0
|Feb precipitation days= 10.9
| May record low C = -2.8
|Mar precipitation days= 12.5
| Jun record low C = 1.8
|Apr precipitation days= 14.1
|May precipitation days= 15.5 | Jul record low C = 4.5
| Aug record low C = 4.9
|Jun precipitation days= 10.3
| Sep record low C = -1.0
|Jul precipitation days= 4.3
| Oct record low C = -4.8
|Aug precipitation days= 3.6
| Nov record low C = -15.0
|Sep precipitation days= 5.2
| Dec record low C = -21.0
|Oct precipitation days= 9.4
| year record low C = -25.7
|Nov precipitation days= 10.3
|Dec precipitation days= 11.6 | precipitation colour = green
|Jan precipitation mm = 35.0 | Jan precipitation mm = 35.0
|Feb precipitation mm = 31.9 | Feb precipitation mm = 33.4
|Mar precipitation mm = 41.3 | Mar precipitation mm = 46.7
|Apr precipitation mm = 60.9 | Apr precipitation mm = 59.0
|May precipitation mm = 66.7 | May precipitation mm = 68.3
|Jun precipitation mm = 44.5 | Jun precipitation mm = 46.2
|Jul precipitation mm = 12.6 | Jul precipitation mm = 14.0
|Aug precipitation mm = 12.3 | Aug precipitation mm = 14.2
|Sep precipitation mm = 20.0 | Sep precipitation mm = 25.2
|Oct precipitation mm = 43.1 | Oct precipitation mm = 46.1
|Nov precipitation mm = 42.3 | Nov precipitation mm = 41.9
|Dec precipitation mm = 40.8 | Dec precipitation mm = 35.9
| year precipitation mm = 465.9
|Jan sun= 43.4
| Jan precipitation days = 11.27
|Feb sun= 103.6
| Feb precipitation days = 11.03
|Mar sun= 158.1
| Mar precipitation days = 13.67
|Apr sun= 183
| Apr precipitation days = 13.83
|May sun= 235.6
| May precipitation days = 15.9
|Jun sun= 276
| Jun precipitation days = 10.4
|Jul sun= 313.1
| Jul precipitation days = 4.13
|Aug sun= 306.9
| Aug precipitation days = 4.2
|Sep sun= 243
| Sep precipitation days = 6.07
|Oct sun= 173.6
| Oct precipitation days = 9.63
|Nov sun= 66
| Nov precipitation days = 9.23
|Dec sun= 24.8
| Dec precipitation days = 11.17
|source 1= Devlet Meteoroloji İşleri Genel Müdürlüğü <ref>{{cite web |url=http://www.dmi.gov.tr/veridegerlendirme/il-ve-ilceler-istatistik.aspx?m=GUMUSHANE |title=Archived copy |access-date=2011-03-19 |url-status=dead |archive-url=https://web.archive.org/web/20110430154809/http://dmi.gov.tr/veridegerlendirme/il-ve-ilceler-istatistik.aspx?m=GUMUSHANE |archive-date=2011-04-30 }}</ref>
| year precipitation days = 120.5
| Jan humidity =69.5
| Feb humidity =66.5
| Mar humidity =63.6
| Apr humidity =61.8
| May humidity =63.7
| Jun humidity =63.3
| Jul humidity =61.2
| Aug humidity =61.3
| Sep humidity =61.2
| Oct humidity =64.9
| Nov humidity =67.8
| Dec humidity =70.5
| year humidity =
| Jan sun = 31.0
| Feb sun = 101.7
| Mar sun = 142.6
| Apr sun = 177.0
| May sun = 223.2
| Jun sun = 261.0
| Jul sun = 300.7
| Aug sun = 285.2
| Sep sun = 225.0
| Oct sun = 161.2
| Nov sun = 63.0
| Dec sun = 31.0
| year sun =
| Jand sun = 1.0
| Febd sun = 3.6
| Mard sun = 4.6
| Aprd sun = 5.9
| Mayd sun = 7.2
| Jund sun = 8.7
| Juld sun = 9.7
| Augd sun = 9.2
| Sepd sun = 7.5
| Octd sun = 5.2
| Novd sun = 2.1
| Decd sun = 1.0
| yeard sun = 5.5
| source 1 = ]<ref>
{{cite web
| url = https://www.mgm.gov.tr/veridegerlendirme/il-ve-ilceler-istatistik.aspx?k=H&m=GUMUSHANE
| title = Resmi İstatistikler: İllerimize Ait Mevism Normalleri (1991–2020)
| publisher = Turkish State Meteorological Service
| language = tr
| access-date = 28 June 2021}}</ref>
| source 2 = ](humidity)<ref>{{Cite web |url=https://www.ncei.noaa.gov/data/oceans/archive/arc0216/0253808/4.4/data/0-data/Region-6-WMO-Normals-9120/Turkiye/CSV/Gumushane_17088.csv |title=World Meteorological Organization Climate Normals for 1991-2020: Gumushane-17088 |access-date=28 August 2024 |website=ncei.noaa.gov |publisher=] |no-pp=y |format=CSV}}</ref>
|date= March 2011 |date= March 2011
}} }}
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==Historic sites: architecture and archaeology== ==Historic sites: architecture and archaeology==
] ]
Gümüşhane has a rich historical background so there are many historical places, mosques, churches, castles. The ancient city of Satala in the modern village of ] was the most important military camp of the ancient ] in the east. This place was ruled by the ]s, ], ], ], ], ], ], and ]. Today, rests of the Sadak village is protected by the ]. In addition, Süleymaniye Mosque is in the previous Gümüşhane settlement and it was commissioned by the ] sultan ]. Küçük Mosque and Çit Village Mosque are some of other popular mosques in the city. Besides, there are numerous churches within Gümüşhane. Santa Çakallı, Santa Terzili, Kalur Rock, Samamoni, and Theodor Churches are some examples of historical churches in Gümüşhane.<ref> {{webarchive|url=https://web.archive.org/web/20120511145300/http://karalahana.com/english/archive/trabzon12.html |date=2012-05-11 }}</ref><ref> {{webarchive|url=https://web.archive.org/web/20120504012239/http://www.karalahana.com/karadeniz/gumushane.htm |date=2012-05-04 }}</ref> Gümüşhane has a rich historical background so there are many historical places, mosques, churches, castles. The ancient city of Satala in the modern village of ] was the most important military camp of the ancient ] in the east. This place was ruled by the ]s, ], ], ], ], ], ], and ]. Today, rests of the Sadak village is protected by the ]. In addition, Süleymaniye Mosque is in the previous Gümüşhane settlement and it was commissioned by the ] sultan ]. Küçük Mosque and Çit Village Mosque are some of other popular mosques in the city. Besides, there are numerous churches within Gümüşhane. Santa Çakallı, Santa Terzili, Kalur Rock, Samamoni, and Theodor Churches are some examples of historical churches in Gümüşhane.<ref> {{webarchive|url=https://web.archive.org/web/20120511145300/http://karalahana.com/english/archive/trabzon12.html |date=2012-05-11 }}</ref><ref> {{webarchive|url=https://web.archive.org/web/20120504012239/http://www.karalahana.com/karadeniz/gumushane.htm |date=2012-05-04 }}</ref>
During the medieval period one of the most important guardians of the road connecting Trabzon to Erzincan was the Byzantine fortress located about {{Convert|2|km|mi|abbr=out}} northwest of modern Gümüşhane. An archaeological and historical assessment of this site as well as a scaled plan were published in 1985. The impressive circuit walls and defenses are clearly evident at the accessible west approach to the lofty outcrop. In addition to several rooms and cisterns, the castle has two chapels; the easternmost was once covered by a dome.<ref>Robert W. Edwards, “The Garrison Forts of the Pontos: A Case for the Diffusion of the Armenian Paradigm,” Revue des Études Arméniennes 19, 1985, pp.207-211, pls.39b-42b.</ref> During the medieval period one of the most important guardians of the road connecting Trabzon to Erzincan was the Byzantine fortress located about {{Convert|2|km|mi|abbr=out}} northwest of modern Gümüşhane. An archaeological and historical assessment of this site as well as a scaled plan were published in 1985. The impressive circuit walls and defenses are clearly evident at the accessible west approach to the lofty outcrop. In addition to several rooms and cisterns, the castle has two chapels; the easternmost was once covered by a dome.<ref>Robert W. Edwards, “The Garrison Forts of the Pontos: A Case for the Diffusion of the Armenian Paradigm,” Revue des Études Arméniennes 19, 1985, pp.207-211, pls.39b-42b.</ref>


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] ]
] ]
There are numerous large and small ]s which owe their formation to the geology - particularly the ]s - of Gümüşhane, including Alicli Agil Cave, Arili Cave, Altınbaşı Cave, Asarönü Ören Cave, Kartalkaya Cave, Ayiini Cave, K.Ardiçli Cave, Karçukuru Cave, Ardiçli Cave, Tepekli Cave, Uçbacalı Cave, Buz Cave and Ikisu Cave.<ref>http://www.visiontours.com.au/index.php/tourism-and-travel/activities/caves/ Retrieved 25 April 2017.</ref> There are numerous large and small ]s which owe their formation to the geology - particularly the ]s - of Gümüşhane, including Alicli Agil Cave, Arili Cave, Altınbaşı Cave, Asarönü Ören Cave, Kartalkaya Cave, Ayiini Cave, K.Ardiçli Cave, Karçukuru Cave, Ardiçli Cave, Tepekli Cave, Uçbacalı Cave, Buz Cave and Ikisu Cave.<ref>{{cite web |url=http://www.visiontours.com.au/index.php/tourism-and-travel/activities/caves/ |title=Vision Tours » Caves |website=www.visiontours.com.au |access-date=25 April 2017}}</ref>


A distinctive local ], bearing purple blossoms in Spring and frequently to be found growing in rock crevices around the mouths of Gümüşhane's many caves, is a member of the ] genus ] : ] - a plant rich in medicinally valuable ] of the type found also in ].<ref>''Flora of Turkey and the East Aegean Islands'' ed. Davis,P.H., pub. University of Edinburgh Press 1978, reprinted 1997, 2001 and 2008. {{ISBN|0 85224 336 7}}</ref> A distinctive local ], bearing purple blossoms in Spring and frequently to be found growing in rock crevices around the mouths of Gümüşhane's many caves, is a member of the ] genus ] : ] - a plant rich in medicinally valuable ] of the type found also in ].<ref>''Flora of Turkey and the East Aegean Islands'' ed. Davis,P.H., pub. University of Edinburgh Press 1978, reprinted 1997, 2001 and 2008. {{ISBN|0 85224 336 7}}</ref>
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] ]


Many native tourists participate in these festivals - not only for entertainment's sake, but also to shop for regional delicacies. ''Pestil'' and ''köme'' are renowned desserts of Gümüşhane, made from ], ], ]s, ]s and milk. In addition to köme and pestil, ]s, ]s, and walnuts are notable local foods put to use in the many different desserts which are numbered among the regional specialities of Gümüşhane. Nor is the town's rich food culture restricted to sweetmeats : '']'', ''lemis'', ''erişte'', '']'', ''kuymak'', ''evelek, ]sı'' and '']'' feature among the savoury dishes local to Gümüşhane.<ref> {{webarchive|url=https://web.archive.org/web/20120511150313/http://www.karalahana.com/english/archive/food.html |date=2012-05-11 }}</ref> Many native tourists participate in these festivals - not only for entertainment's sake, but also to shop for regional delicacies. ''Pestil'' and ''köme'' are renowned desserts of Gümüşhane, made from ], ], ]s, ]s and milk. In addition to köme and pestil, ]s, ]s, and walnuts are notable local foods put to use in the many different desserts which are numbered among the regional specialities of Gümüşhane. Nor is the town's rich food culture restricted to sweetmeats : '']'', ''lemis'', ''erişte'', '']'', ''kuymak'', ''evelek, ]sı'' and ''siron'' feature among the savoury dishes local to Gümüşhane.<ref> {{webarchive|url=https://web.archive.org/web/20120511150313/http://www.karalahana.com/english/archive/food.html |date=2012-05-11 }}</ref>


==Ethnic groups== ==Ethnic groups==
Line 188: Line 217:
{{More citations needed section|date=April 2011}} {{More citations needed section|date=April 2011}}


The local residents of Gümüşhane region were ] also called Chan (Tzan; by Georgians) i.e. ] (Halt; by themselves). Just after the ] (1461) and the town soon became a home for miners. Sultan Murad ΙΙΙ (1574–1595) appears to have granted extra privileges to the chief miners and the town prospered and soon became a centre of Hellenism. At the time, it had 60,000 residents. Its trade was increasing and the whole province of Chaldia was on the rise. Another example of its development was that they minted coins with the name Kioumous-hane on them. Another example was the settlement of chief mining families there such as the Sarasites, the Karatsades, the Stavracoglous, the Kalimachidises, the Grigorantons and others. There were also more jewellery shops opening, as well as more hagiography and other arts in the region.


The rise in wealth and abundance soon brought positive changes to the communities. From the beginning of the 18th century new schools were opening, and from 1723 the Frontistirion (Greek Tuition Centre) of Argyropolis was in full operation. The tuition centre became an educational institution and spiritual centre of the region. In 1650 the diocese was elevated to archdiocese status, and hundreds of churches and temples were built.
New mines rich in minerals were discovered in Ak-dag Maden and Argoni, which resulted in a large exodus of miners from Argyropolis to the new mines. The further dramatic fall in population followed the Russo-Turkish War of 1829–30, when many Greek speaking Pontians of the area collaborated with or welcomed the Russian army that occupied the area. So as to escape likely Turkish reprisals, the majority of the Greekophone Pontic population followed the Russian army as it withdrew back into ] and Southern Russia, many settling there and joining preexisting communities of ] that had moved eastwards between the fall of the ] in 1461 and the 1801 Russian annexation of Georgia, including another community of Pontic Greekophone miners who had settled in Lore, then ] of Georgia in 1778 invited by the king ]. Some of the Pontic Greekophone mining families of Gumuşhane also settled in ], Mesopotamia and other mining regions, from Tiflis (]) to as far as Ak-Dağ and the Taurus. During those years tension between the Christian Greekophones and Muslim population was also growing due to the Greek Revolution and the public reversion to Greek Orthodoxy of many of the ], Pontic Greekophones who had superficially adopted Turkish Islam in the early Ottoman period but who had remained crypto-Christian in private.<ref> {{webarchive|url=https://web.archive.org/web/20120511150856/http://karalahana.com/english/Crypto-Christians-of-the-Trabzon.html |date=2012-05-11 }}</ref>


Just after the ] (1461) and the town soon became a home for miners. Sultan ] (1574–1595) appears to have granted extra privileges to the chief miners and the town prospered and soon became a centre of ]. At the time, it had 60,000 residents. Its trade was increasing and the whole province of ] was on the rise. Another example of its development was that they minted coins with the name Kioumous-hane on them. Another example was the settlement of chief mining families there such as the Sarasites, the Karatsades, the Stavracoglous, the Kalimachidises, the Grigorantons and others. There were also more jewellery shops opening, as well as more hagiography and other arts in the region.
During those confusing and troubling times many people became benefactors of Argyropolis, such as the Sarasite family and the influential teacher Georgios Kyriakidis. Kyriakidis identified the need to extract large sums of money from the churches of Saint George, Saint Theodore, Τίμιου Σταυρού and Παναγίας for the educational needs of the town. Sale of church property as well as donations and consecrations resulted in the erection of a new school at the Frontistirion of Argyropolis, a school which was to operate until the Exchange (1923). The Frontistirion comprised a three-grade high school, a seven-grade primary school including scholarship classes, and a six-grade girls' school, as well as a carpet-making technical school.


The rise in wealth and abundance soon brought positive changes to the communities. From the beginning of the 18th century new schools were opening, and from 1723 the Greek Tuition Centre '']'' was in full operation. The tuition centre became an educational institution and spiritual centre of the region. In 1650 the diocese was elevated to archdiocese status, and hundreds of churches and temples were built. New mines rich in minerals were discovered in Ak-dag Maden and Argoni, which resulted in a large exodus of miners from Argyropolis to the new mines. The further dramatic fall in population followed the Russo-Turkish War of 1829–30, when many Greek Pontians of the area collaborated with or welcomed the Russian army that occupied the area. So as to escape likely Turkish reprisals, the majority of the Pontic Greek population followed the Russian army as it withdrew back into ] and ], many settling there and joining preexisting communities of ] that had moved eastwards between the fall of the ] in 1461 and the 1801 Russian annexation of Georgia, including another community of Pontic Greekophone miners who had settled in Lore, then ] of Georgia in 1778 invited by the king ]. Some of the ] mining families of Gumuşhane also settled in ], Mesopotamia and other mining regions, from Tiflis (]) to as far as Ak-Dağ and the Taurus. During those years tension between the Christian Greeks (Rum) and Muslim population was also growing due to the ] and the public reversion to Greek Orthodoxy of many of the ], ] who had superficially adopted Turkish Islam in the early Ottoman period but who had remained ] in private.<ref> {{webarchive|url=https://web.archive.org/web/20120511150856/http://karalahana.com/english/Crypto-Christians-of-the-Trabzon.html |date=2012-05-11 }}</ref>
Another public building was the library, the Educational Society Kyriakidis, as well as the Metropolis of Chaldia. The Argyropolitans therefore are very much regarded as having some of the best resources in education, due mainly to their economic rise as a result of mining.<ref>], Pontus: Antik Çağ’dan Günümüze Karadeniz’in Etnik ve Siyasi Tarihi Genesis Publishing. Ankara, 2011 pp. 695-701</ref>


During those confusing and troubling times many people became benefactors of Argyropolis, such as the Sarasite family and the influential teacher Georgios Kyriakidis. Kyriakidis identified the need to extract large sums of money from the churches of Saint George, Saint Theodore, Τίμιου Σταυρού and Παναγίας for the educational needs of the town. Sale of church property as well as donations and consecrations resulted in the erection of a new school at the ], a school which was to operate until the ] (1923). The Frontistirion comprised a three-grade high school, a seven-grade primary school including scholarship classes, and a six-grade girls' school, as well as a carpet-making technical school.
After the turmoil and ethnic strife (1914–1923), a few ethnic Pontic Greeks managed to flee to Greece. They settled in the Macedonia region of Northern Greece. A small group which settled in Naousa brought precious items with them from their churches in town, as well as items from the library of the Frontistirion, including rare manuscripts and books. This collection is still in use today and is considered{{By whom|date=January 2011}} a prized asset of Naousa.

Another public building was the library, the Educational Society Kyriakidis, as well as the ]. The Argyropolitans therefore are very much regarded as having some of the best resources in education, due mainly to their economic rise as a result of mining.<ref>], Pontus: Antik Çağ’dan Günümüze Karadeniz’in Etnik ve Siyasi Tarihi Genesis Publishing. Ankara, 2011 pp. 695-701</ref>

After the ] (1914–1923), a few ethnic ] managed to flee to ]. They settled in ], region of ]. A small group which settled in ] brought precious items with them from their churches in town, as well as items from the library of the Frontistirion, including rare manuscripts and books. This collection is still in use today by Euxenus Association of Pontians of Naoussa - National Library of Argyroupolis 'Kiriakidis' and is considered a prized asset of Naousa.


The town was occupied by the Russian army on July 20, 1916, but the Russians withdrew on February 15, 1918, after the fall of the czar. After the exchange (1923) no Orthodox remained in the region. The town was occupied by the Russian army on July 20, 1916, but the Russians withdrew on February 15, 1918, after the fall of the czar. After the exchange (1923) no Orthodox remained in the region.
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Historically, Gümüşhane had ] plantations for ].<ref name=Prothero64>{{cite book|last=Prothero|first=W.G.|title=Armenia and Kurdistan|year=1920|publisher=H.M. Stationery Office|location=London|page=64|url=http://www.wdl.org/en/item/11768/view/1/64/}}</ref> Historically, Gümüşhane had ] plantations for ].<ref name=Prothero64>{{cite book|last=Prothero|first=W.G.|title=Armenia and Kurdistan|year=1920|publisher=H.M. Stationery Office|location=London|page=64|url=http://www.wdl.org/en/item/11768/view/1/64/}}</ref>

==Gallery==
<gallery>
File:Tasoba@Torul-Gumushane-Turkey.JPG|]
File:Santa_Harabeleri_-_panoramio.jpg|left|] Ruins in Gümüşhane
File:Gümüşhane_Yolu..._-_panoramio_(1).jpg|Highway to Gümüşhane city center
</gallery>
==Mayors of Gümüşhane==
* ]-] Yalçın Kurt ]
* ]-] Naim Ağaç ]
* ]-] Mustafa Canlı ]
* ]-] Ercan Çimen ]
* ]-] Vedat Soner Başer ]


==Notable natives== ==Notable natives==
* ] (1879, Gümüşhane - 1961), Deputy during the Ottoman Empire and after declaration of republic first Minister of Agriculture and Minister of Finance of Turkey * ] (1879, Gümüşhane - 1961), Deputy during the Ottoman Empire and after declaration of republic first Minister of Agriculture and Minister of Finance of Turkey
* ] (1905, İstanbul - 1975), Prominent Turkish nationalist writer, born into a family from Gümüşhane * ] (1905, İstanbul - 1975), Prominent Turkish nationalist writer, born into a family from Gümüşhane
* ] (1919, Trabzon - 1990), Turkish academic of theology, left-wing politician and writer, born into Ataç family of Gümüşhane * ] (1919, Trabzon - 1990), Turkish academic of theology, left-wing politician and writer, born into Ataç family of Gümüşhane
Line 217: Line 260:
* ] (1984, Trabzon - ), Turkish singer, born into a family from ] * ] (1984, Trabzon - ), Turkish singer, born into a family from ]
* ] (1966, İstanbul - ), Turkish television producer and lawyer, born into a family from Gümüşhane on his maternal side. * ] (1966, İstanbul - ), Turkish television producer and lawyer, born into a family from Gümüşhane on his maternal side.
* ] (1901, Tsalka - 1959) Greek Elder * ] (1901, Tsalka - 1959) Greek Elder
* ] (1881, Gümüşhane - 1971), Greek scholar, journalist, teacher and writer * ] (1881, Gümüşhane - 1971), Greek scholar, journalist, teacher and writer
* ] (1969, Zonguldak - ), Turkish football manager and former player, born into a family from ] * ] (1969, Zonguldak - ), Turkish football manager and former player, born into a family from ]
Line 231: Line 274:
*The Encyclopedia of Pontian Hellenism. Malliaris Pedia. *The Encyclopedia of Pontian Hellenism. Malliaris Pedia.
*The Byzantine Monuments and Topography of the Pontos . Anthony Bryer, David Winfield. Dumbarton Oaks p.&nbsp;3 *The Byzantine Monuments and Topography of the Pontos . Anthony Bryer, David Winfield. Dumbarton Oaks p.&nbsp;3
* {{Cite book|last=Kiminas|first=Demetrius|title=The Ecumenical Patriarchate: A History of Its Metropolitanates with Annotated Hierarch Catalogs|year=2009|url=https://books.google.com/books?id=QLWqXrW2X-8C|publisher=Wildside Press LLC}} * {{Cite book|last=Kiminas|first=Demetrius|title=The Ecumenical Patriarchate: A History of Its Metropolitanates with Annotated Hierarch Catalogs|year=2009|url=https://books.google.com/books?id=QLWqXrW2X-8C|publisher=Wildside Press LLC|isbn=9781434458766 }}
* {{cite web|url=http://www.kulturturizm.gov.tr/EN/BelgeGoster.aspx?17A16AE30572D31395FB1C5180B6EBD6B0B3F062CA1037C7|archive-url=https://archive.today/20121221195938/http://www.kulturturizm.gov.tr/EN/BelgeGoster.aspx?17A16AE30572D31395FB1C5180B6EBD6B0B3F062CA1037C7|url-status=dead|archive-date=2012-12-21|title=Mosques, Mausoleums and Churches in Gümüşhane|access-date=2009-03-05|author=Turkish Ministry of Culture and Tourism}}
* {{cite web|url=http://www.fallingrain.com/world/TU/0/Gumushane.html|title=Geographical information on Gümüşhane, Turkey|access-date=2008-12-01|author=Falling Rain Genomics, Inc}}
* {{cite web|url=http://www.kulturturizm.gov.tr/EN/BelgeGoster.aspx?17A16AE30572D31395FB1C5180B6EBD6B0B3F062CA1037C7|archive-url=https://archive.is/20121221195938/http://www.kulturturizm.gov.tr/EN/BelgeGoster.aspx?17A16AE30572D31395FB1C5180B6EBD6B0B3F062CA1037C7|url-status=dead|archive-date=2012-12-21|title=Mosques, Mausoleums and Churches in Gümüşhane|access-date=2009-03-05|author=Turkish Ministry of Culture and Tourism}}


==External links== ==External links==
{{Commons category-inline|Gümüşhane}} {{Commons category-inline|Gümüşhane}}
* {{in lang|tr}}
* {{in lang|tr}} * {{in lang|tr}}
* *
* *


{{Gümüşhane District}}
{{Districts of Turkey|provname=Gümüşhane|image=Gumushane|sortkey=Gumushane}}
{{Authority control}} {{Authority control}}


{{DEFAULTSORT:Gumushane}} {{DEFAULTSORT:Gumushane}}
] ]
] ]
] ]
] ]

Latest revision as of 19:10, 8 November 2024

For other places with the same name, see Gümüşhane (disambiguation). Municipality in Turkey
Gümüşhane
Municipality
View of GümüşhaneView of Gümüşhane
Gümüşhane is located in TurkeyGümüşhaneGümüşhaneLocation in Turkey
Coordinates: 40°27′35″N 39°28′40″E / 40.45972°N 39.47778°E / 40.45972; 39.47778
CountryTurkey
ProvinceGümüşhane
DistrictGümüşhane
Government
 • MayorVedat Soner Başer (MHP)
Elevation1,153 m (3,783 ft)
Population39,214
Time zoneUTC+3 (TRT)
Postal code29830
Area code0456
Websitewww.gumushane.bel.tr

Gümüşhane (Turkish: [ɟyˈmyʃhaːne] ) is a city in the Black Sea Region of Turkey. It is the seat of Gümüşhane Province and Gümüşhane District. Its population is 39,214 (2022). The city lies along the Harşit River, about 40 miles (64 km) southwest of Trabzon. The city lies at an elevation of 1,153 m (3,783 ft).

History

It is suggested that the ancient Thia (Θεία in Greek, a settlement of Roman, Late Roman and Byzantine periods) was located 4 mi (6.4 km) west of modern Gümüşhane, in modern Beşkilise. In the Byzantine period, there was a town named Tzanicha or Tzantzakon (Τζάνιχα, Τζάντζακον in Byzantine Greek) means land of Zan / Laz people, possibly located 2 miles (3.2 km) to the west of Gümüşhane.

Around 840 AD, the area was included in the new Roman (Byzantine) province of Chaldia (Χαλδία). It was later ruled by the Byzantine Empire of Trebizond.

During the Ottoman years, the sanjak of Gümüşhane fell under the administration successively of Rum Province, Erzurum Province and Trabzon Province, and was divided into four kazas: Gümüşhane, Torul (capital city Ardassa), Şiran (Cheriana), and Kelkit (Keltik).

The sanjak in which Gümüşhane was situated at some stage comprised 37 mines of argentiferous lead and six copper mines. There is no evidence that these mines were in use during Byzantine times.

As for the name of the city during the Ottoman period, Greek-speaking population was also using the name Gümüşhane (Γκιμισχανά and Κιουμουσχανά) but, in the first decades of the 19th century, the Greek name Argiroupoli (Αργυρόπολις, from argyros "silver" and polis "city") was used. After the population exchange of 1923 many of the Greek inhabitants moved to the synonymous town in Attica, Greece.

Geography

Örümcek Forest in Gümüşhane
Zigana Torul in Gümüşhane

Gümüşhane is surrounded by high mountains, Zigana-Trabzon Mountains to the north, Çimen Mountains to the south, Giresun Mountains to the west and Pulur, Soğanlı Mountains to the east. Trekking is popular sport is at these mountains. Mount Zigana has a ski center on it and it is a well known tourist destination for winter sports. Abdal Musa Peak (3331 m.) is the highest peak within it. The main trees in the forests are Scotch pine and fir, and there are many animals and birds in the area. There are many lakes such as Karanlık Göl, Beş Göller, Artebel Gölü, Kara Göller which are at the peak of Gavurdağı Mountain, and are preserved as natural parks. All these mountains compose 56% of the area of Gümüşhane province.

Climate

Gümüşhane has a humid continental climate (Köppen climate classification: Dsb, bordering Dfb, or Trewartha climate classification: Dc) with cold and snowy winters and warm summers. In the height of summer; July and August, temperatures at midday usually surpass 28 °C, summer nights tend to become very cool due to the continentality of Gümüşhane, and in winter temperatures usually plummet to -10 °C and even go as low as -20 °C occasionally.

Highest recorded temperature:41.1 °C (106.0 °F) on 2 August 2017
Lowest recorded temperature:−25.7 °C (−14.3 °F) on 22 February 1985

Climate data for Gümüşhane (1991–2020, extremes 1961–2023)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 15.5
(59.9)
18.0
(64.4)
24.0
(75.2)
29.0
(84.2)
34.4
(93.9)
36.2
(97.2)
41.0
(105.8)
41.1
(106.0)
37.7
(99.9)
32.0
(89.6)
22.3
(72.1)
19.2
(66.6)
41.1
(106.0)
Mean daily maximum °C (°F) 3.4
(38.1)
5.7
(42.3)
10.3
(50.5)
16.2
(61.2)
21.2
(70.2)
25.4
(77.7)
28.7
(83.7)
29.5
(85.1)
25.6
(78.1)
19.5
(67.1)
10.7
(51.3)
5.2
(41.4)
16.8
(62.2)
Daily mean °C (°F) −1.4
(29.5)
−0.2
(31.6)
4.0
(39.2)
9.2
(48.6)
13.6
(56.5)
17.3
(63.1)
20.3
(68.5)
20.6
(69.1)
16.8
(62.2)
11.8
(53.2)
4.9
(40.8)
0.6
(33.1)
9.8
(49.6)
Mean daily minimum °C (°F) −5.2
(22.6)
−4.8
(23.4)
−0.9
(30.4)
3.4
(38.1)
7.4
(45.3)
10.9
(51.6)
13.8
(56.8)
14.2
(57.6)
10.3
(50.5)
6.3
(43.3)
0.5
(32.9)
−3.0
(26.6)
4.4
(39.9)
Record low °C (°F) −23.6
(−10.5)
−25.7
(−14.3)
−22.6
(−8.7)
−11.0
(12.2)
−2.8
(27.0)
1.8
(35.2)
4.5
(40.1)
4.9
(40.8)
−1.0
(30.2)
−4.8
(23.4)
−15.0
(5.0)
−21.0
(−5.8)
−25.7
(−14.3)
Average precipitation mm (inches) 35.0
(1.38)
33.4
(1.31)
46.7
(1.84)
59.0
(2.32)
68.3
(2.69)
46.2
(1.82)
14.0
(0.55)
14.2
(0.56)
25.2
(0.99)
46.1
(1.81)
41.9
(1.65)
35.9
(1.41)
465.9
(18.34)
Average precipitation days 11.27 11.03 13.67 13.83 15.9 10.4 4.13 4.2 6.07 9.63 9.23 11.17 120.5
Average relative humidity (%) 69.5 66.5 63.6 61.8 63.7 63.3 61.2 61.3 61.2 64.9 67.8 70.5 64.6
Mean monthly sunshine hours 31.0 101.7 142.6 177.0 223.2 261.0 300.7 285.2 225.0 161.2 63.0 31.0 2,002.6
Mean daily sunshine hours 1.0 3.6 4.6 5.9 7.2 8.7 9.7 9.2 7.5 5.2 2.1 1.0 5.5
Source 1: Turkish State Meteorological Service
Source 2: NCEI(humidity)

Historic sites: architecture and archaeology

Old Gümüşhane city, 1910s Ottoman era postcard

Gümüşhane has a rich historical background so there are many historical places, mosques, churches, castles. The ancient city of Satala in the modern village of Sadak was the most important military camp of the ancient Roman Empire in the east. This place was ruled by the Colchians, Hittites, Assyrians, Urartu, Persians, Pontic Greeks, Romans, and Byzantines. Today, rests of the Sadak village is protected by the Ministry of Culture and Tourism. In addition, Süleymaniye Mosque is in the previous Gümüşhane settlement and it was commissioned by the Ottoman sultan Süleyman the Magnificent. Küçük Mosque and Çit Village Mosque are some of other popular mosques in the city. Besides, there are numerous churches within Gümüşhane. Santa Çakallı, Santa Terzili, Kalur Rock, Samamoni, and Theodor Churches are some examples of historical churches in Gümüşhane. During the medieval period one of the most important guardians of the road connecting Trabzon to Erzincan was the Byzantine fortress located about 2 kilometres (1.2 mi) northwest of modern Gümüşhane. An archaeological and historical assessment of this site as well as a scaled plan were published in 1985. The impressive circuit walls and defenses are clearly evident at the accessible west approach to the lofty outcrop. In addition to several rooms and cisterns, the castle has two chapels; the easternmost was once covered by a dome.

Natural environment

Ecel Rocks in Gümüşhane
Kürtün village in Gümüşhane
Mountains of Gümüşhane

There are numerous large and small caves which owe their formation to the geology - particularly the limestones - of Gümüşhane, including Alicli Agil Cave, Arili Cave, Altınbaşı Cave, Asarönü Ören Cave, Kartalkaya Cave, Ayiini Cave, K.Ardiçli Cave, Karçukuru Cave, Ardiçli Cave, Tepekli Cave, Uçbacalı Cave, Buz Cave and Ikisu Cave.

A distinctive local wildflower, bearing purple blossoms in Spring and frequently to be found growing in rock crevices around the mouths of Gümüşhane's many caves, is a member of the nightshade genus Physochlaina : Physochlaina orientalis - a plant rich in medicinally valuable tropane alkaloids of the type found also in belladonna.

The cave in Gümüşhane most visited by tourists is the 150 metres (490 ft) long Karaca Cave, popular because of its speleothems (= dripstone formations), including stalagmites, stalactites, columns and travertine pools. It is a fossil cave located between Torul and Gümüşhane, in which the lime-rich water percolating through fissures in the roof has slowly built up calcite structures of remarkable complexity. Other geological features of Gümüşhane include the numerous plateaux commanding views of the forested areas which surround them. These include the Zigana, Taşköprü, Artabel, Şiran and Kalis plateaux, which form fitting sites for the Summer festivals which are held there annually.

Cuisine

Siron is a traditional dish in Gümüşhane

Many native tourists participate in these festivals - not only for entertainment's sake, but also to shop for regional delicacies. Pestil and köme are renowned desserts of Gümüşhane, made from mulberries, honey, hazel nuts, walnuts and milk. In addition to köme and pestil, rosehips, apples, and walnuts are notable local foods put to use in the many different desserts which are numbered among the regional specialities of Gümüşhane. Nor is the town's rich food culture restricted to sweetmeats : mantı, lemis, erişte, borani, kuymak, evelek, dolması and siron feature among the savoury dishes local to Gümüşhane.

Ethnic groups

Pontic Greek influence

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Just after the fall of Trebizond (1461) and the town soon became a home for miners. Sultan Murad ΙΙΙ (1574–1595) appears to have granted extra privileges to the chief miners and the town prospered and soon became a centre of Hellenism. At the time, it had 60,000 residents. Its trade was increasing and the whole province of Chaldia was on the rise. Another example of its development was that they minted coins with the name Kioumous-hane on them. Another example was the settlement of chief mining families there such as the Sarasites, the Karatsades, the Stavracoglous, the Kalimachidises, the Grigorantons and others. There were also more jewellery shops opening, as well as more hagiography and other arts in the region.

The rise in wealth and abundance soon brought positive changes to the communities. From the beginning of the 18th century new schools were opening, and from 1723 the Greek Tuition Centre Frontistirion of Argyropolis was in full operation. The tuition centre became an educational institution and spiritual centre of the region. In 1650 the diocese was elevated to archdiocese status, and hundreds of churches and temples were built. New mines rich in minerals were discovered in Ak-dag Maden and Argoni, which resulted in a large exodus of miners from Argyropolis to the new mines. The further dramatic fall in population followed the Russo-Turkish War of 1829–30, when many Greek Pontians of the area collaborated with or welcomed the Russian army that occupied the area. So as to escape likely Turkish reprisals, the majority of the Pontic Greek population followed the Russian army as it withdrew back into Georgia and Southern Russia, many settling there and joining preexisting communities of Caucasus Greeks that had moved eastwards between the fall of the Empire of Trebizond in 1461 and the 1801 Russian annexation of Georgia, including another community of Pontic Greekophone miners who had settled in Lore, then Kingdom of Kartli of Georgia in 1778 invited by the king Heraclius II of Georgia. Some of the Pontic Greek mining families of Gumuşhane also settled in Nicomedia, Mesopotamia and other mining regions, from Tiflis (Tbilisi) to as far as Ak-Dağ and the Taurus. During those years tension between the Christian Greeks (Rum) and Muslim population was also growing due to the Greek Revolution and the public reversion to Greek Orthodoxy of many of the Stavriotes, Pontic Greeks who had superficially adopted Turkish Islam in the early Ottoman period but who had remained crypto-Christian in private.

During those confusing and troubling times many people became benefactors of Argyropolis, such as the Sarasite family and the influential teacher Georgios Kyriakidis. Kyriakidis identified the need to extract large sums of money from the churches of Saint George, Saint Theodore, Τίμιου Σταυρού and Παναγίας for the educational needs of the town. Sale of church property as well as donations and consecrations resulted in the erection of a new school at the Frontistirion of Argyropolis, a school which was to operate until the population exchange (1923). The Frontistirion comprised a three-grade high school, a seven-grade primary school including scholarship classes, and a six-grade girls' school, as well as a carpet-making technical school.

Another public building was the library, the Educational Society Kyriakidis, as well as the Metropolis of Chaldia. The Argyropolitans therefore are very much regarded as having some of the best resources in education, due mainly to their economic rise as a result of mining.

After the Pontic Greek Genocide (1914–1923), a few ethnic Pontic Greeks managed to flee to Greece. They settled in Macedonia, region of Northern Greece. A small group which settled in Naousa brought precious items with them from their churches in town, as well as items from the library of the Frontistirion, including rare manuscripts and books. This collection is still in use today by Euxenus Association of Pontians of Naoussa - National Library of Argyroupolis 'Kiriakidis' and is considered a prized asset of Naousa.

The town was occupied by the Russian army on July 20, 1916, but the Russians withdrew on February 15, 1918, after the fall of the czar. After the exchange (1923) no Orthodox remained in the region.

Economy

Historically, Gümüşhane had mulberry tree plantations for sericulture.

Gallery

  • Torul Torul
  • Santa Ruins in Gümüşhane Santa Ruins in Gümüşhane
  • Highway to Gümüşhane city center Highway to Gümüşhane city center

Mayors of Gümüşhane

Notable natives

  • Hasan Fehmi Ataç (1879, Gümüşhane - 1961), Deputy during the Ottoman Empire and after declaration of republic first Minister of Agriculture and Minister of Finance of Turkey
  • Nihal Atsız (1905, İstanbul - 1975), Prominent Turkish nationalist writer, born into a family from Gümüşhane
  • Bahriye Üçok (1919, Trabzon - 1990), Turkish academic of theology, left-wing politician and writer, born into Ataç family of Gümüşhane
  • Tarık Akan (1949, İstanbul - 2016), Turkish film actor and producer, born into a family from Gümüşhane
  • Beren Saat (1984, Ankara - ), Turkish actress, born into a family from Gümüşhane
  • Turgay Erdener (1957, Gümüşhane - ), Composer and teacher
  • Aydın Doğan (1936, Kelkit - ), Entrepreneur and businessmen
  • Mehmet Scholl (1970, Karlsruhe - ), German football manager and former player, born into a family from Torul
  • Hikmet Temel Akarsu (1960, Gümüşhane - ), Turkish novelist, short-story writer, satirist and playwright
  • Yusuf Güney (1984, Trabzon - ), Turkish singer, born into a family from Kelkit
  • Armağan Çağlayan (1966, İstanbul - ), Turkish television producer and lawyer, born into a family from Gümüşhane on his maternal side.
  • Saint George Karslidis (1901, Tsalka - 1959) Greek Elder
  • Georgios Kandilaptis (1881, Gümüşhane - 1971), Greek scholar, journalist, teacher and writer
  • Ertuğrul Sağlam (1969, Zonguldak - ), Turkish football manager and former player, born into a family from Torul
  • Ziya Doğan (1961, Köse - ), Turkish football manager
  • Tolga Zengin (1983, Hopa - ), Turkish football goalkeeper, born into a family from Torul
  • Yunus Mallı (1992, Kaseel - ), Turkish footballer, born into a family from Şiran
  • Mithat Demirel (1978, Berlin - ), German former professional basketball player of Turkish descent.

References

  1. ^ "Address-based population registration system (ADNKS) results dated 31 December 2022, Favorite Reports" (XLS). TÜİK. Retrieved 13 March 2023.
  2. İl Belediyesi, Turkey Civil Administration Departments Inventory. Retrieved 1 March 2023.
  3. Barrington Atlas of the Greek and Roman World: Map by Map directory, p.1237.
  4. Procopius of Caesarea, Περί Κτισμάτων, book C, 7.
  5. Kiminas 2009, pp. 105.
  6. Terezakis Yorgos, Diocese of Chaldia (Ottoman Period), Encyclopaedia of the Hellenic world, Asia Minor.
  7. "İllerimize Ait Genel İstatistik Verileri". mgm.gov.tr (in Turkish). Meteoroloji Genel Müdürlüğü. Retrieved 28 August 2024.
  8. "Resmi İstatistikler: İllerimize Ait Mevism Normalleri (1991–2020)" (in Turkish). Turkish State Meteorological Service. Retrieved 28 June 2021.
  9. "World Meteorological Organization Climate Normals for 1991-2020: Gumushane-17088" (CSV). ncei.noaa.gov. National Oceanic and Atmosoheric Administration. Retrieved 28 August 2024.
  10. Gümüşhane (en) Archived 2012-05-11 at the Wayback Machine
  11. Gümüşhane historical places (tr) Archived 2012-05-04 at the Wayback Machine
  12. Robert W. Edwards, “The Garrison Forts of the Pontos: A Case for the Diffusion of the Armenian Paradigm,” Revue des Études Arméniennes 19, 1985, pp.207-211, pls.39b-42b.
  13. "Vision Tours » Caves". www.visiontours.com.au. Retrieved 25 April 2017.
  14. Flora of Turkey and the East Aegean Islands ed. Davis,P.H., pub. University of Edinburgh Press 1978, reprinted 1997, 2001 and 2008. ISBN 0 85224 336 7
  15. Traditional food Archived 2012-05-11 at the Wayback Machine
  16. Who were the crypto-Christians?, Crypto-Christians of the Trabzon Region of Pontos Archived 2012-05-11 at the Wayback Machine
  17. Özhan Öztürk, Pontus: Antik Çağ’dan Günümüze Karadeniz’in Etnik ve Siyasi Tarihi Genesis Publishing. Ankara, 2011 pp. 695-701
  18. Prothero, W.G. (1920). Armenia and Kurdistan. London: H.M. Stationery Office. p. 64.

Literature

External links

Media related to Gümüşhane at Wikimedia Commons

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