Lihat sumber Gunung Erciyes

{{Infobox mountain
|name=Gunung Erciyes
|photo=Erciyes From Aktepe Goreme.JPG
|photo_caption=Pemandangan jauh dari Gunung Erciyes, yang terlihat dari [[Göreme]]
|location=[[Provinsi Kayseri]], [[Turki]]
|label_position=right
|coordinates = {{coord|38.531|N|35.447|E|type:mountain_scale:100000|format=dms|display=inline,title}}
|elevation_m=3917
|prominence_m=2419
|prominence_ref=<ref>http://www.peaklist.org/WWlists/ultras/turkey.html</ref>
|listing=[[Puncak yang sangat menonjol|Ultra]]
|range=
|topo=
|coordinates_ref=<ref name="GVP" />
|type=[[Gunung berapi kerucut]]
|age=
|last_eruption=6880 SM ± 40 tahun<ref name="GVP" />
|first_ascent=
|map_size=
}}
'''Gunung Erciyes''' ({{lang-tr|Erciyes Dağı}}), juga dikenal sebagai '''Argaeus''', adalah sebuah [[gunung berapi]] di [[Turki]]. Erciyes merupakan [[gunung berapi kerucut]] besar yang dikelilingi oleh banyak [[bidang vulkanik monogenetik]] dan [[kubah lava]], serta satu [[maar]]. Sebagian besar gunung berapi ini terbentuk oleh aliran [[lava]] yang mengandung material [[andesit]] dan [[dasit]]. Pada suatu waktu di masa lalu, bagian dari puncak gunung runtuh ke arah timur.

Gunung berapi ini mulai terbentuk pada zaman [[miosen]]. Pada awalnya, gunung berapi yang berada lebih jauh ke timur bernama ''Koç Dağ'' terbentuk dari aliran lava. Kemudian, di timur juga, letusan besar membentuk [[kaldera]]. Selama zaman [[pleistosen]], Gunung Erciyes tumbuh di dalam kaldera bersama dengan sekelompok kubah lava. Erupsi lateral Erciyes mungkin telah menghasilkan lapisan abu di [[Laut Hitam]] dan [[Laut Mediterania|Mediterania]] selama zaman [[holosen]] awal.

Letusan terakhir gunung ini terjadi selama zaman holosen awal dan mungkin telah mengendapkan abu hingga ke [[Palestina]]; terjadinya sejarah vulkanisme Erciyes tidak dapat dipastikan dengan pasti. Letusan Erciyes di masa mendatang dapat membahayakan kota-kota di utara gunung tersebut. Gunung berapi ini tertutup oleh [[gletser]] selama zaman pleistosen, dan satu gletser masih ada hingga hari ini, akan tetapi sudah mulai menghilang.

== Etimologi ==
Erciyes dahulu dikenal sebagai Argaeus, nama yang berasal dari raja [[Makedonia (kerajaan kuno)|Makedonia]], [[Argaeus I dari Makedonia|Argaeus I]] (678{{snd}}640{{nbsp}}[[Anno Domini|SM]]).{{sfn|Sarıkaya|Zreda|Çiner|2009|p=2328}} Sementara itu, gunung Argaeus yang berada di [[bulan]] dinamai dari nama lama gunung ini.<ref name="Planetarynames" />

== Geologi dan geomorfologi ==
Erciyes terletak di [[Provinsi Kayseri]], [[Turki]].<ref name="Vural2008" /> Kota [[Kayseri]] terletak {{convert|15|km}}{{sfn|Kurkcuoglu|Sen|Temel|Aydar|2001|p=510}}-{{convert|25|km}}{{sfn|Dogan|Dogan|Peate|Dogruel|2011|p=387}} sebelah utara gunung berapi Erciyes. Kota-kota lain di kawasan ini adalah [[Talas, Turki|Talas]] dan [[Hacılar|Hacilar]], juga berada di utara Erciyes tetapi lebih dekat dengan gunung berapi ini, masing-masing berjarak sekitar {{convert|19|km}} dan {{convert|12|km}}. Kota [[Develi]], juga terletak dekat dengan gunung ini, tepatnya berada di sebelah selatan gunung berapi.{{sfn|Şen|Kürkcüoğlu|Aydar|Gourgaud|2003|p=229,244}} Akses ke area puncak gunung cukup sulit.{{sfn|Dogan|Dogan|Peate|Dogruel|2011|p=388}} Para pendaki di zaman dahulu melaporkan bahwa, baik [[Laut Hitam]] dan [[Laut Mediterania|Mediterania]] dapat terlihat dari puncak gunung.<ref name="Strabo" />

== Iklim dan biologi ==
Iklim di daerah gunung ini dipengaruhi oleh topografi, hal ini dikarenakan [[Pegunungan Taurus]] dan [[Pegunungan Kaçkar|Kaçkar]] menghalangi masuknya [[kelembaban]] ke Anatolia. Musim panas di sini menghasilkan kondisi yang kering dan panas sementara musim dingin cenderung basah dan dingin; di Kayseri, suhu musim panas sekitar {{convert|19|C}} dan suhu musim dinginnya sekitar {{convert|0|C}}. Hujan di Kayseri sebagian besar terjadi di musim gugur, musim dingin, dan musim semi dan curah hujannya mencapai {{convert|383|mm}} per tahun.{{sfn|Sarıkaya|Zreda|Çiner|2009|p=2328}} Di Develi, sebelah selatan Erciyes, suhu maksimumnya sekitar {{convert|29.5|C}} dan suhu minimumnya {{convert|-5.6|C}}.{{sfn|Halici|John|Aksoy|2005|p=569,570}} Perkiraan suhu pada ketinggian 2.700 m sekitar {{convert|-0.4|C}}, dan curah hujannya {{convert|722|mm}} per tahun.{{sfn|Sarıkaya|Zreda|Çiner|2009|p=2330}} Secara keseluruhan, gunung ini memiliki [[iklim kontinental]].{{sfn|Ünaldi|2007|p=140}}

Empat sabuk [[vegetasi]] mengelilingi gunung ini, di antaranya adalah boreal, subalpine, alpine, dan subnival.{{sfn|Halici|John|Aksoy|2005|p=577}} Hingga ketinggian 1.000 – 1.100 m, vegetasi [[stepa]] mendominasi. Lebih jauh lagi, di ketinggian antara 1.100 – 2.500 m, terdapat hutan-hutan yang berisikan ''[[Juniperus]]'', ''[[Populus tremula]]'' dan ''[[Quercus]]'' di mana lingkungan tersebut belum terlalu dijamah oleh aktivitas manusia. Pada ketinggian yang lebih tinggi, terdapat padang rumput gunung.{{sfn|Ünaldi|2007|p=141}} Spesies yang ditemukan di sabuk vegetasi gunung ini sangat berbeda dari daerah yang sama di pegunungan Eropa Barat.{{sfn|Halici|John|Aksoy|2005|p=577}}

[[Flora]] yang ada di Erciyes cukup beragam. Sejumlah spesies tumbuhan [[endemik]] telah teridentifikasi, termasuk di antaranya adalah ''[[Astragalus argaeus]]'', ''[[Astragalus stenosemioides]]'', ''[[Asyneuma trichostegium]]'', ''[[Bellardiochloa argaea]]'', ''[[Dianthus crinitus]] argaeus'', ''[[Festuca cratericola]]'', ''[[Festuca woronowii]] argaea'', ''[[Hieracium argaeum]]'', ''[[Onobrychis argaea]]'', dan ''[[Vicia canescens]] argaea''.<ref name="Vural2008" /> Tanaman ''[[Silene]] erciyesdaghensis'' ditemukan di Erciyes dan dinamai berdasarkan nama gunung di mana tanaman ini ditemukan.<ref name="AksoyHamzaoglu2008" /> Ahli geografi [[Strabo]] mengklaim bahwa, pada zaman dahulu, gunung berapi ini berhutan.<ref name="Strabo" /> Sejumlah spesies hewan endemik dan relik juga dapat ditemukan di Erciyes,<ref name="Akbulut2014" /> serta kaya akan flora [[lumut kerak]].{{sfn|Halici|John|Aksoy|2005|p=567}} Aktivitas penggembalaan, pemukiman, dan pariwisata di gunung ini telah mengubah vegetasi alami gunung.{{sfn|Halici|John|Aksoy|2005|p=568}}

== Ancaman dan interaksi manusia ==
Gunung Erciyes yang merupakan gunung berapi dikenal karena letusannya pada zaman dahulu, tepatnya sebelum pembentukan kubah lava. Letusan semacam itu dapat membahayakan kota-kota di sekitarnya, seperti Kayseri, Hacilar, dan Talas. Mencairnya sisa es di gunung berapi dapat menghasilkan [[lahar]] yang berbahaya; pada tahun 1985, letusan gunung berapi [[Nevado del Ruiz]] di [[Kolombia]] [[Tragedi Armero|menghasilkan 20.000 korban jiwa]] setelah banjir lahar seperti itu. Bahkan tanpa letusan, curah hujan yang tinggi bisa menghasilkan banjir lahar di lereng curam gunung berapi yang padat penduduk.{{sfn|Şen|Kürkcüoğlu|Aydar|Gourgaud|2003|p=244}}

Sekitar lima hotel terdapat di gunung ini, yang merupakan situs [[olahraga musim dingin]] utama. Pada tahun 2010, 324.221 [[wisatawan]] mengunjungi gunung Erciyes dan wilayah Kayseri, sebagian besar dari mereka adalah wisatawan domestik.<ref name="Akbulut2014" />
<!--
== Catatan ==
{{notelist}}-->

== Referensi ==
{{Reflist|30em|refs=
<!--<ref name="Neugebauer2017">{{cite journal|last1=Neugebauer|first1=Ina|last2=Wulf|first2=Sabine|last3=Schwab|first3=Markus J.|last4=Serb|first4=Johanna|last5=Plessen|first5=Birgit|last6=Appelt|first6=Oona|last7=Brauer|first7=Achim|title=Implications of S1 tephra findings in Dead Sea and Tayma palaeolake sediments for marine reservoir age estimation and palaeoclimate synchronisation|journal=Quaternary Science Reviews|date=August 2017|volume=170|page=274|doi=10.1016/j.quascirev.2017.06.020|url=https://www.sciencedirect.com/science/article/pii/S0277379117300744|language=en|issn=0277-3791}}</ref>
<ref name="ReberAkcar2014">{{Cite journal|last=Reber|first=Regina|last2=Akçar|first2=Naki|last3=Yesilyurt|first3=Serdar|last4=Yavuz|first4=Vural|last5=Tikhomirov|first5=Dmitry|last6=Kubik|first6=Peter W.|last7=Schlüchter|first7=Christian|date=2014-10-01|title=Glacier advances in northeastern Turkey before and during the global Last Glacial Maximum|url=http://www.sciencedirect.com/science/article/pii/S0277379114002893|journal=Quaternary Science Reviews|volume=101|page=191|doi=10.1016/j.quascirev.2014.07.014}}</ref>-->
<ref name="AksoyHamzaoglu2008">{{Cite journal|last=Aksoy|first=Ahmet|last2=Hamzaoğlu|first2=Ergin|last3=Kiliç|first3=Semra|date=2008-12-01|title=A new species of Silene L. (Caryophyllaceae) from Turkey|url=http://onlinelibrary.wiley.com/doi/10.1111/j.1095-8339.2008.00922.x/abstract|journal=Botanical Journal of the Linnean Society|language=en|volume=158|issue=4|page=731|doi=10.1111/j.1095-8339.2008.00922.x|issn=1095-8339}}</ref><!--
<ref name="Pinar-Erdem1977">{{Cite book|url=https://link.springer.com/chapter/10.1007/978-1-4684-3036-3_7|title=The Ocean Basins and Margins|last=Pinar-Erdem|first=Nuriye|last2=Ilhan|first2=Emin|date=1977-01-01|publisher=Springer US|isbn=9781468430387|editor-last=Nairn|editor-first=Alan E. M.|page=297|chapter=Outlines of the Stratigraphy and Tectonics of Turkey, with Notes on the Geology of Cyprus|doi=10.1007/978-1-4684-3036-3_7|editor-last2=Kanes|editor-first2=William H.|editor-last3=Stehli|editor-first3=Francis G.}}</ref>
<ref name="Aksu2003">{{Cite journal|last=Aksu|first=Ibrahim|date=2003-12-01|title=The Sultan's Journey and other Turkish Placename Stories|url=https://dx.doi.org/10.1179/nam.2003.51.3-4.163|journal=Names|volume=51|issue=3–4|page=185|doi=10.1179/nam.2003.51.3-4.163|issn=0027-7738}}</ref>
<ref name="Schumacher1996">{{cite journal|last1=Schumacher|first1=R.|last2=Mues-Schumacher|first2=U.|title=The Kizilkaya ignimbrite — an unusual low-aspect-ratio ignimbrite from Cappadocia, central Turkey|journal=Journal of Volcanology and Geothermal Research|date=January 1996|volume=70|issue=1–2|page=107|doi=10.1016/0377-0273(95)00046-1}}</ref>
<ref name="Ciner2017">{{Cite journal|last=Çiner|first=Attila|last2=Sarıkaya|first2=Mehmet Akif|date=2017-01-01|title=Cosmogenic 36Cl geochronology of late Quaternary glaciers in the Bolkar Mountains, south central Turkey|url=http://sp.lyellcollection.org/content/433/1/271|journal=Geological Society, London, Special Publications|language=en|volume=433|issue=1|page=271|doi=10.1144/SP433.3|issn=0305-8719}}</ref>
<ref name="BartonLane2015">{{Cite journal|last=Barton|first=R. N. E.|last2=Lane|first2=C. S.|last3=Albert|first3=P. G.|last4=White|first4=D.|last5=Collcutt|first5=S. N.|last6=Bouzouggar|first6=A.|last7=Ditchfield|first7=P.|last8=Farr|first8=L.|last9=Oh|first9=A.|date=2015-06-15|title=The role of cryptotephra in refining the chronology of Late Pleistocene human evolution and cultural change in North Africa|url=http://www.sciencedirect.com/science/article/pii/S0277379114003497|journal=Quaternary Science Reviews|series=Synchronising Environmental and Archaeological Records using Volcanic Ash Isochrons|volume=118|page=163|doi=10.1016/j.quascirev.2014.09.008}}</ref>
<ref name="AydarCubukcu2010">{{Cite journal|last=Aydar|first=Erkan|last2=Cubukcu|first2=H. Evren|last3=Sen|first3=Erdal|last4=Ersoy|first4=Orkun|last5=Duncan|first5=Robert A.|last6=Ciner|first6=Attila|date=2010-05-01|title=Timing of Cappadocian volcanic events and its significance on the development of Central Anatolian Orogenic Plateau|volume=12|page=10147|bibcode=2010EGUGA..1210147A}}</ref>-->
<ref name="Akbulut2014">{{Cite book|url=https://link.springer.com/chapter/10.1007/978-3-642-16191-9_6|title=Volcanic Tourist Destinations|last=Akbulut|first=Gülpınar|date=2014-01-01|publisher=Springer Berlin Heidelberg|isbn=9783642161902|editor-last=Erfurt-Cooper|editor-first=Patricia|series=Geoheritage, Geoparks and Geotourism|page=96|chapter=Volcano Tourism in Turkey|doi=10.1007/978-3-642-16191-9_6}}</ref><!--
<ref name="Aydemir2009">{{Cite journal|last=Aydemir|first=Attila|date=2009-07-01|title=Tectonic investigation of Central Anatolia, Turkey, using geophysical data|url=http://www.sciencedirect.com/science/article/pii/S0926985109000214|journal=Journal of Applied Geophysics|volume=68|issue=3|page=324|doi=10.1016/j.jappgeo.2009.02.002}}</ref>-->
<ref name="GVP">{{Cite GVP|vn=213010|name=Erciyes Dagi}}</ref>
<ref name="Strabo">{{cite book|author1=Strabo|authorlink1=Strabo|title=Geographica, book 2|trans-title=Geography|orig-year=23|date=1924|edition=2|url=http://www.perseus.tufts.edu/hopper/text?doc=urn:cts:greekLit:tlg0099.tlg001.perseus-eng2:12.2.7|accessdate=28 January 2017|chapter=7}}</ref><!--
<ref name="Sarp2005">{{Cite journal|last=Sarp|first=Halil|last2=ČernÝ|first2=Radovan|date=2005-04-01|title=Yazganite, NaFe3+ 2(Mg,Mn)(AsO4)3·H2O, a new mineral: its description and crystal structure|url=http://www.ingentaconnect.com/content/schweiz/ejm/2005/00000017/00000002/art00019|journal=European Journal of Mineralogy|volume=17|issue=2|page=367|doi=10.1127/0935-1221/2005/0017-0367}}</ref>-->
<ref name="Vural2008">{{Cite journal|last=Vural|first=Cem|date=2008-09-01|title=A new species of Dianthus (Caryophyllaceae) from Mount Erciyes, central Anatolia, Turkey|url=http://onlinelibrary.wiley.com/doi/10.1111/j.1095-8339.2008.00843.x/abstract|journal=Botanical Journal of the Linnean Society|language=en|volume=158|issue=1|pages=55–61|doi=10.1111/j.1095-8339.2008.00843.x|issn=1095-8339}}</ref><!--
<ref name="Bayari2006">{{Cite book|url=https://link.springer.com/chapter/10.1007/1-4020-4738-X_3|title=Groundwater and Ecosystems|last=Bayari|first=Sardar|last2=Ozyurt|first2=N. N.|last3=Hatipoglu|first3=Z.|last4=Kilani|first4=S.|date=2006-01-01|publisher=Springer Netherlands|isbn=9781402047367|editor-last=Baba|editor-first=Alper|language=en|doi=10.1007/1-4020-4738-x_3|editor-last2=Howard|editor-first2=Ken W. F.|editor-last3=Gunduz|editor-first3=Orhan|page=40}}</ref>-->
<ref name="Planetarynames">{{cite web|url=https://planetarynames.wr.usgs.gov/Feature/3974|title=Planetary Names: Mons, montes: Mons Argaeus on Moon|website=planetarynames.wr.usgs.gov|language=en|access-date=2017-01-26}}</ref>
}}

=== Sumber ===
{{refbegin}}
* {{Cite journal|last=Cullen|first=Victoria L.|last2=Smith|first2=Victoria C.|last3=Helge|first3= Arz W.|date=2014-10-01|title=The detailed tephrostratigraphy of a core from the south‐east Black Sea spanning the last ∼60 ka|url=http://onlinelibrary.wiley.com/doi/10.1002/jqs.2739/abstract|journal=Journal of Quaternary Science|volume=29|issue=7|doi=10.1002/jqs.2739|issn=1099-1417|ref=harv}}
* {{Cite journal|last=Develle|first=A-L.|last2=Williamson|first2=D.|last3=Gasse|first3=F.|last4=Walter-Simonnet|first4=A-V.|date=2009-10-10|title=Early Holocene volcanic ash fallout in the Yammoûneh lacustrine basin (Lebanon): Tephrochronological implications for the Near East|url=http://www.sciencedirect.com/science/article/pii/S0377027309003084|journal=Journal of Volcanology and Geothermal Research|volume=186|issue=3–4|pages=416–425|doi=10.1016/j.jvolgeores.2009.07.016|ref=harv}}
* {{Cite journal|last=Dogan|first=A. Umran|last2=Dogan|first2=Meral|last3=Peate|first3=David W.|last4=Dogruel|first4=Zafer|date=2011-12-01|title=Textural and mineralogical diversity of compositionally homogeneous dacites from the summit of Mt. Erciyes, Central Anatolia, Turkey|url=http://www.sciencedirect.com/science/article/pii/S0024493711002556|journal=[[Lithos (journal)|Lithos]]|volume=127|issue=3–4|pages=387–400|doi=10.1016/j.lithos.2011.09.003|ref=harv}}
* {{Cite journal|last=Erol|first=O.|date=1999-04-01|title=A geomorphological study of the Sultansazliǧi lake, central Anatolia|url=http://www.sciencedirect.com/science/article/pii/S0277379198001024|journal=Quaternary Science Reviews|volume=18|issue=4–5|pages=647–657|doi=10.1016/S0277-3791(98)00102-4|ref=harv}}
* {{Cite journal|last=Gencalioglu-Kuscu|first=Gonca|date=2010-12-05|title=Geochemical characterization of a Quaternary monogenetic volcano in Erciyes Volcanic Complex: Cora Maar (Central Anatolian Volcanic Province, Turkey)|url=https://link.springer.com/article/10.1007/s00531-010-0620-4|journal=International Journal of Earth Sciences|language=en|volume=100|issue=8|pages=1967–1985|doi=10.1007/s00531-010-0620-4|issn=1437-3254|ref=harv}}
* {{Cite journal|last=Gençalioğlu-Kuşcu|first=Gonca|last2=Atilla|first2=Cüneyt|last3=Cas|first3=Ray A. F.|last4=Kuşcu|first4=İlkay|date=2007-01-01|title=Base surge deposits, eruption history, and depositional processes of a wet phreatomagmatic volcano in Central Anatolia (Cora Maar)|url=http://www.sciencedirect.com/science/article/pii/S0377027306003118|journal=Journal of Volcanology and Geothermal Research|series=Maar-diatreme volcanism and associated processes|volume=159|issue=1–3|pages=198–209|doi=10.1016/j.jvolgeores.2006.06.013|ref=harv}}
* {{Cite journal|last=GÜÇTEKİN|first=AYKUT|last2=KÖPRÜBAŞI|first2=NEZİHİ|date=2009-03-06|title=Geochemical Characteristics of Mafic and Intermediate Volcanic Rocks from the Hasandağ and Erciyes Volcanoes (Central Anatolia, Turkey)|url=http://journals.tubitak.gov.tr/earth/abstract.htm?id=9891|journal=Turkish Journal of Earth Sciences|volume=18|issue=1|issn=1300-0985|ref=harv}}
* {{cite journal|last1=Halici|first1=M. G.|last2=John|first2=V.|last3=Aksoy|first3=A.|title=Lichens of Erciyes Mountain (Kayseri, Turkey)|journal=Flora Mediterranea|date=2005|issue=15|pages=567–580|url=http://www1.unipa.it/herbmed/flora/15-567.pdf|accessdate=29 January 2017|ref=harv|issn=1120-4052}}
* {{Cite journal|last=Hamann|first=Y.|last2=Wulf|first2=S.|last3=Ersoy|first3=O.|last4=Ehrmann|first4=W.|last5=Aydar|first5=E.|last6=Schmiedl|first6=G.|date=2010-05-01|title=First evidence of a distal early Holocene ash layer in Eastern Mediterranean deep-sea sediments derived from the Anatolian volcanic province|url=http://www.sciencedirect.com/science/article/pii/S003358940900163X|journal=Quaternary Research|volume=73|issue=3|pages=497–506|doi=10.1016/j.yqres.2009.12.004|ref=harv}}
* {{cite journal|last1=Hayakawa|first1=Y. S.|last2=Yoshida|first2=H.|last3=Obanawa|first3=H.|last4=Naruhashi|first4=R.|last5=Okumura|first5=K.|last6=Zaiki|first6=M.|last7=Kontani|first7=R.|title=Characteristics of debris avalanche deposits inferred from source volume estimate and hummock morphology around Mt. Erciyes, central Turkey|journal=Nat. Hazards Earth Syst. Sci.|date=7 February 2018|volume=18|issue=2|pages=429–444|doi=10.5194/nhess-18-429-2018|url=https://www.nat-hazards-earth-syst-sci.net/18/429/2018/|ref=harv|issn=1684-9981}}
* {{Cite journal|last=Innocenti|first=F.|last2=Mazzuoli|first2=R.|last3=Pasquarè|first3=G.|last4=Brozolo|first4=F. Radicati Di|last5=Villari|first5=L.|date=1975-07-01|title=The Neogene calcalkaline volcanism of Central Anatolia: geochronological data on Kayseri—Nigde area|url=https://www.cambridge.org/core/journals/geological-magazine/article/div-classtitlethe-neogene-calcalkaline-volcanism-of-central-anatolia-geochronological-data-on-kayserinigde-areadiv/DC0268AB5A112F9BA847040133494D40|journal=Geological Magazine|volume=112|issue=4|pages=349–360|doi=10.1017/S0016756800046744|issn=1469-5081|ref=harv}}
* {{Cite journal|last=Koçyiğit|first=Ali|last2=Erol|first2=Oğuz|date=2001-01-01|title=A tectonic escape structure: Erciyes pull-apart basin, Kayseri, central Anatolia, Turkey|url=https://dx.doi.org/10.1080/09853111.2001.11432439|journal=Geodinamica Acta|volume=14|issue=1–3|pages=133–145|doi=10.1080/09853111.2001.11432439|issn=0985-3111|ref=harv}}
* {{Cite journal|last=Kürkçüoglu|first=Biltan|last2=Sen|first2=Erdal|last3=Aydar|first3=Erkan|last4=Gourgaud|first4=Alain|last5=Gündogdu|first5=Niyazi|date=1998-10-01|title=Geochemical approach to magmatic evolution of Mt. Erciyes stratovolcano Central Anatolia, Turkey|url=http://www.sciencedirect.com/science/article/pii/S0377027398000675|journal=Journal of Volcanology and Geothermal Research|volume=85|issue=1–4|pages=473–494|doi=10.1016/S0377-0273(98)00067-5|ref=harv}}
* {{Cite journal|last=Kurkcuoglu|first=B.|last2=Sen|first2=E.|last3=Temel|first3=A.|last4=Aydar|first4=E.|last5=Gourgaud|first5=A.|date=2001-06-01|title=Trace-Element Modeling and Source Constraints for Tholeiitic and Cale-alkaline Basalts from a Depleted Asthenospheric Mantle Source, Mt. Erciyes Stratovolcano, Turkey|url=https://dx.doi.org/10.1080/00206810109465029|journal=International Geology Review|volume=43|issue=6|pages=508–522|doi=10.1080/00206810109465029|issn=0020-6814|ref=harv}}
* {{Cite journal|last=Kürkcüoglu|first=Biltan|last2=sen|first2=Erdal|last3=Temel|first3=Abidin|last4=Aydar|first4=Erkan|last5=Gourgaud|first5=Alain|date=2004-03-01|title=Interaction of Asthenospheric and Lithospheric Mantle: The Genesis of Calc-alkaline Volcanism at Erciyes Volcano, Central Anatolia, Turkey|url=https://dx.doi.org/10.2747/0020-6814.46.3.243|journal=International Geology Review|volume=46|issue=3|pages=243–258|doi=10.2747/0020-6814.46.3.243|issn=0020-6814|ref=harv}}
* {{cite journal|last1=Notsu|first1=K.|last2=Fujitani|first2=T.|last3=Ui|first3=T.|last4=Matsuda|first4=J.|last5=Ercan|first5=T.|title=Geochemical features of collision-related volcanic rocks in central and eastern Anatolia, Turkey|journal=Journal of Volcanology and Geothermal Research|volume=64|issue=3–4|year=1995|pages=171–191|issn=0377-0273|doi=10.1016/0377-0273(94)00077-T|ref=harv}}
* {{Cite journal|last=Sarıkaya|first=Mehmet Akif|last2=Zreda|first2=Marek|last3=Çiner|first3=Attila|date=2009-11-01|title=Glaciations and paleoclimate of Mount Erciyes, central Turkey, since the Last Glacial Maximum, inferred from 36Cl cosmogenic dating and glacier modeling|url=http://www.sciencedirect.com/science/article/pii/S0277379109001425|journal=Quaternary Science Reviews|volume=28|issue=23–24|pages=2326–2341|doi=10.1016/j.quascirev.2009.04.015|ref=harv}}
* {{Cite journal|date=2002|last=Sen|first=Erdal|last2=Aydar|first2=Erkan|last3=Gourgaud|first3=Alain|last4=Kurkcuoglu|first4=Biltan|title=La phase explosive précédant l'extrusion des dômes volcaniques : exemple du dôme rhyodacitique de Dikkartin Dag, Erciyes, Anatolie centrale, Turquie|url=https://dx.doi.org/10.1016/S1631-0713(02)01698-X|journal=Comptes Rendus Geoscience|volume=334|issue=1|pages=27–33|doi=10.1016/s1631-0713(02)01698-x|ref=harv}}
* {{cite journal|last1=Şen|first1=Erdal|last2=Kürkcüoğlu|first2=Biltan|last3=Aydar|first3=Erkan|last4=Gourgaud|first4=Alain|last5=Vincent|first5=Pierre M.|title=Volcanological evolution of Mount Erciyes stratovolcano and origin of the Valibaba Tepe ignimbrite (Central Anatolia, Turkey)|journal=Journal of Volcanology and Geothermal Research|volume=125|issue=3–4|year=2003|pages=225–246|issn=0377-0273|doi=10.1016/S0377-0273(03)00110-0|ref=harv}}
* {{cite journal|last1=Ünaldi|first1=Ülkü Eser|title=A Negative Example Area In Human - Natural Environment Relationship: Erciyes Mountain (Turkiye)|journal=Humanity & Social Sciences Journ|date=2007|volume=2|issue=2|pages=139–147|url=http://citeseerx.ist.psu.edu/viewdoc/download?doi=10.1.1.494.7318&rep=rep1&type=pdf|accessdate=29 January 2017|ref=harv|issn=1818-4960|citeseerx=10.1.1.494.7318}}
{{refend}}

== Pranala luar ==
{{Commons category-inline}}
* [http://www.erciyeskayakmerkezi.com/ Ski Resort]
* [http://volcano.si.edu/volcano.cfm?vn=213010 Global Volcanism Program page about Mount Erciyes]

{{DEFAULTSORT:Erciyes}}
{{Authority control}}
[[Kategori:Gunung di Turki]]