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Coordinates: 38°19′53″N 21°6′5″E / 38.33139°N 21.10139°E / 38.33139; 21.10139
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{{for|the Achelous River in [[Bulgaria]]|Aheloy (river)}}
{{short description|River in western Greece}}
{{other uses}}

{{Infobox river
{{More footnotes|date=March 2012}}
{{Infobox River | river_name = Acheloos
| name = Acheloos
| image_name = Acheloos river narrows 02.jpg
| image = Acheloos river narrows 02.jpg
| image_caption =
| caption =
| origin = [[Pindus]] mountains
| source1_location = [[Pindus]] mountains
| source1_coordinates =
| mouth = [[Ionian Sea]]<br>{{Coord|38|19|53|N|21|6|5|E|display=inline,title}}
{{Coord|39|41|13|N|21|8|31|E|display=i}}
| basin_countries = [[Greece]]
| mouth_location = [[Ionian Sea]]
| length = {{Convert|220|km|mi|0|abbr=on}}
| mouth_coordinates = {{coord|38|19|53|N|21|6|5|E|display=inline,title}}
| elevation =
| subdivision_type1 = Country
| discharge = {{Convert|7800000000|m3|acre.ft|0|abbr=on}} (annual mean)
| subdivision_name1 = [[Greece]]
| watershed = {{Convert|5472|km2|mi2|0|abbr=on}}<ref>{{cite journal| last=TH. Fourniotis| first=Nikolaos| title=A Proposal for Impact Evaluation of the Diversion of the Acheloos River, on the Acheloos Estuary in Western Greece| journal=International Journal of Engineering Science and Technology| date=April 2012| volume=4| issue=4| pages=1793–1802| url=http://www.ijest.info/docs/IJEST12-04-04-230.pdf| accessdate=25 April 2013| location=University of Patras, Rio Campus| issn=0975-5462}}</ref>
|length_km=220
| source1_elevation =
| discharge1_avg = {{Convert|7800000000|m3|acre.ft|0|abbr=on}} (annual mean)
|basin_size_km2=5472
}}
}}
[[File:Acheloos River - Greece - marked course DE.png|thumb|300px|The Acheloos River marked on a satellite image. Labels in German.]]
[[File:Acheloos River - Greece - marked course DE.png|thumb|300px|The Acheloos River marked on a satellite image. Labels in German.]]
[[File:Acheloos river map.jpg|thumb|200px|Acheloos River map.]]


The '''Achelous''' ({{lang-el|Αχελώος}}), also '''Acheloos''', is a [[river]] in western [[Greece]]. It formed the boundary between [[Acarnania]] and [[Aetolia]] of antiquity. It empties into the [[Ionian Sea]]. In ancient times its spirit was venerated as the river god [[Achelous]].
The '''Achelous''' ({{langx|el|Αχελώος}}, {{langx|grc|Ἀχελῷος}} ''Akhelôios''), also '''Acheloos''', is a [[river]] in [[Epirus (region)|Epirus]], western [[Greece]]. It is {{Convert|220|km|mi|0|abbr=on}} long.<ref>[http://www.statistics.gr/documents/20181/1515741/GreeceInFigures_2018Q1_EN.pdf/e90e9c60-ed92-40a7-a1e0-9a58d542d596 Greece in Figures January - March 2018], p. 12</ref><ref>{{cite web|url=http://www.ypeka.gr/LinkClick.aspx?fileticket=T4DDG1hqQMY%3D&tabid=252&language=el-GR |title=Preliminary Flood Risk Assessment|archive-url=https://web.archive.org/web/20200215192049/http://www.ypeka.gr/LinkClick.aspx?fileticket=T4DDG1hqQMY%3D&tabid=252&language=el-GR|archive-date=15 February 2020|language=el|publisher=Ministry of Environment, Energy and Climate Change|page=49}}</ref> It formed the boundary between [[Acarnania]] and [[Aetolia]] of antiquity. It empties into the [[Ionian Sea]]. In ancient times its spirit was venerated as the river god [[Achelous]].


[[Herodotus]], taking notice of the shoreline-transforming power of the Acheloos River, even compared it to the [[Nile]] in this respect:
[[Herodotus]], taking notice of the shoreline-transforming power of the Acheloos River, even compared it to the [[Nile]] in this respect:
:'There are other rivers as well which, though not as large as the Nile, have had substantial results. In particular (although I could name others), there is the Achelous, which flows through [[Acarnania]] into the sea and has already turned half the Echinades islands into mainland.' (2.10, trans. Waterfield)
:'There are other rivers as well which, though not as large as the Nile, have had substantial results. In particular (although I could name others), there is the Achelous, which flows through [[Acarnania]] into the sea and has already turned half the Echinades islands into mainland.' (2.10, trans. Waterfield)


It is said to have been called more anciently ''Thoas'', ''Axenus'' and ''Thestius''.<ref>William Smith, [https://www.perseus.tufts.edu/hopper/text?doc=Perseus:text:1999.04.0064:id=achelous-geo ACHELO´US], in his ''Dictionary of Greek and Roman Geography'' (1854)</ref>
The previous name was '''Thoas'''. It is rarely known as '''Thestios''' and '''Axenos'''.{{Citation needed|date=August 2009}}


==Course==
==Course==
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On exiting the Kremasta reservoir, the river flows southwest into Aetolia-Acarnania, feeding the [[Kastraki (lake)|Kastraki]] reservoir, west of the [[Panaitoliko]] range. {{convert|10|to|15|km}} downstream from this lake, it flows into the [[Stratos (lake)|Stratos]] reservoir. Further downstream, it runs through the lowlands west of [[Agrinio]]. It finally empties into the [[Ionian Sea]], {{convert|29|km|abbr=on}} west of [[Missolonghi]].
On exiting the Kremasta reservoir, the river flows southwest into Aetolia-Acarnania, feeding the [[Kastraki (lake)|Kastraki]] reservoir, west of the [[Panaitoliko]] range. {{convert|10|to|15|km}} downstream from this lake, it flows into the [[Stratos (lake)|Stratos]] reservoir. Further downstream, it runs through the lowlands west of [[Agrinio]]. It finally empties into the [[Ionian Sea]], {{convert|29|km|abbr=on}} west of [[Missolonghi]].


===Settlements===
== Settlements ==
In order from upstream to downstream:
In order from upstream to downstream:
* [[Aspropotamos, Trikala|Katafyto]]
* [[Aspropotamos, Trikala|Katafyto]]
* [[Gardiki, Trikala|Gardiki]]
* [[Gardiki, Trikala|Gardiki]]
* [[Mesochora]]
* [[Mesochora]]
* [[Neraida|Koryfi]]
* [[Koryfi, Trikala|Koryfi]]
* [[Myrofyllo]]
* [[Myrofyllo]]
* [[Argithea|Petroto]]
* [[Argithea|Petroto]]
Line 47: Line 52:
* [[Oiniades|Gouria]]
* [[Oiniades|Gouria]]
* [[Oiniades|Neochori]]
* [[Oiniades|Neochori]]

===Dams===
There are five dams on the river. From upstream to downstream there is the [[Mesochora Dam]] which was completed in 2001 but has not impounded its reservoir. Below that is the [[Sykia Dam]] which is partly constructed. Further down is the [[Kremasta Dam|Kremasta]] (1965), [[Kastraki Dam|Kastraki]] (1969) and [[Stratos Dam]]s (1989).


==Acheloos River in mythology==
==Acheloos River in mythology==
:''Main article [[Achelous]]''
{{main article|Achelous}}
[[File:Hall of the Augustals.jpg|thumb|A Roman fresco from [[Herculaneum]] depicting [[Hercules]] (from Etruscan ''[[Hercle]]'' and ultimately Greek ''[[Herakles]]'') and [[Achelous]] (patron deity of the Achelous River in Greece) from [[Greek mythology|Greco]]-[[Roman mythology]], 1st century AD]]


==History==
==History==
In antiquity, the Achelous was the largest and most celebrated river in Greece, rising in [[Mount Pindus]], and after flowing through the mountainous country of the [[Dolopia]]ns and [[Agraeans]], entered the plain of [[Acarnania]] and [[Aetolia]] near [[Stratos, Greece|Stratus]], and discharged itself into the [[Ionian Sea]], near the Acarnanian town of [[Oeniadae]]. It subsequently formed the boundary between Acarnania and Aetolia, but in the time of [[Thucydides]] the territory of Oeniadae extended east of the river. It is usually called a river of Acarnania, but it is sometimes assigned to Aetolia. Its general direction is from north to south. Its waters are of a whitish yellow or cream colour, whence it derives a later name of ''Aspropotamo'' or the White river, and to which [[Dionysius Periegetes]] probably alludes in the epithet ἀργυροδίνης.<ref>[[Dionysius Periegetes]], ''Description of the World'', 432.</ref> Periegetes places the sources of the river near a place called [[Chalcis (Epirus)|Chalcis]].<ref>[[Dionysius Periegetes]], ''Description of the World'', 496.</ref> It is said to have been called more anciently '''Thoas''', '''Axenus''' and '''Thestius'''.<ref>{{Cite Thucydides|2.102}}</ref><ref>{{Cite Strabo|pp. 449, 450, 458}}</ref><ref>[[Plutarch]], ''de Fluv.'' 22</ref><ref>{{Cite Stephanus|''s.v.'' Ἀχελῷος}}</ref> In the lower part of its course, the plain through which it flows was called in antiquity '''Paracheloitis''' after the river. This plain was celebrated for its fertility, though covered in great part with marshes, several of which were formed by the overflowings of the Achelous.<ref>{{Cite DGRG|title=Acheolous}}</ref>
In 1359 the [[Battle of Achelous (1359)|Battle of Achelous]] between [[Albanians|Albanian]] forces under [[Peter Losha]] and the [[Despotate of Epirus]] under [[Nikephoros II Orsini]] took place near the river Achelous. Nikephoros II was defeated and killed during the battle, and two new states were established in the area, the [[Despotate of Arta]] and the [[Despotate of Angelokastron and Lepanto]].<ref name="mb">{{cite book| last=Van Antwerp| first=John| title=The Late Medieval Balkans: A Critical Survey from the Late Twelfth Century to the Ottoman Conquest| url=http://books.google.com/books?id=QDFVUDmAIqIC&pg=PA350&dq=Aetolia+1359&cd=1#v=onepage&q=Aetolia%201359&f=false| year=1994| publisher=[[University of Michigan Press]]| isbn=978-0-472-08260-5| pages=348–51}} </ref>

In 1359 the [[Battle of Achelous (1359)|Battle of Achelous]] between [[Albanians|Albanian]] forces under [[Peter Losha]] and the [[Despotate of Epirus]] under [[Nikephoros II Orsini]] took place near the river Achelous. Nikephoros II was defeated and killed during the battle, and two new states were established in the area, the [[Despotate of Arta]] and the [[Despotate of Angelokastron and Lepanto]].<ref name="mb">{{cite book| last=Van Antwerp| first=John| title=The Late Medieval Balkans: A Critical Survey from the Late Twelfth Century to the Ottoman Conquest| url=https://books.google.com/books?id=QDFVUDmAIqIC&q=Aetolia+1359&pg=PA350| year=1994| publisher=[[University of Michigan Press]]| isbn=978-0-472-08260-5| pages=348â 51}}</ref>


In the 1960s, the [[Kremasta Dam]] in the Aitoloacarnania-Evrytania boundary was under construction. The area is not forested. The dam, made of concrete, took years to complete, eventually flooding a portion of the western part of the prefecture of Eurytania. The dam includes a power station with transformer lines in the east. The dam powers electricity for the western part of Greece and the central part. It caused some soil erosion in some flooded valleys. The [[Kastraki Dam]] is downstream and was completed in 1969. Downstream of Katsiki, the [[Stratos Dam]] was completed in 1989. The arch bridges includes the [[Karafilio]] and the [[Ardanovo]].
In the 1960s, the [[Kremasta Dam]] in the Aitoloacarnania-Evrytania boundary was under construction. The area is not forested. The dam, made of concrete, took years to complete, eventually flooding a portion of the western part of the prefecture of Eurytania. The dam includes a power station with transformer lines in the east. The dam powers electricity for the western part of Greece and the central part. It caused some soil erosion in some flooded valleys. The [[Kastraki Dam]] is downstream and was completed in 1969. Downstream of Katsiki, the [[Stratos Dam]] was completed in 1989. The arch bridges includes the [[Karafilio]] and the [[Ardanovo]].
Line 58: Line 69:
The Acheloos River Diversion project has been the center of debate since the 1980s. It calls for four large dams, the [[Sykia Dam|Sykia]], [[Mesochora Dam|Mesochora]], [[Mouzaki Dam|Mouzaki]] and [[Pyli Dam|Pyli]], along with a {{Convert|17.4|km|mi|abbr=on|adj=mid|-long}} channel. The goal of the project is to divert {{Convert|600000000|m3|acre.ft|abbr=on}} annually from the river west towards the [[Thessaly]] plains in order to help irrigate {{Convert|240000|-|380000|ha|acre|abbr=on}} of mostly cotton crops. Construction on the project has been stalled several times, the latest in 2005, because of environmental and social concerns.
The Acheloos River Diversion project has been the center of debate since the 1980s. It calls for four large dams, the [[Sykia Dam|Sykia]], [[Mesochora Dam|Mesochora]], [[Mouzaki Dam|Mouzaki]] and [[Pyli Dam|Pyli]], along with a {{Convert|17.4|km|mi|abbr=on|adj=mid|-long}} channel. The goal of the project is to divert {{Convert|600000000|m3|acre.ft|abbr=on}} annually from the river west towards the [[Thessaly]] plains in order to help irrigate {{Convert|240000|-|380000|ha|acre|abbr=on}} of mostly cotton crops. Construction on the project has been stalled several times, the latest in 2005, because of environmental and social concerns.


==Sources==
==References==
{{Commons category|Acheloos River}}
{{reflist}}
{{reflist}}

==Sources==
* {{DGRG|title=Acheolous}}


==External links==
==External links==
{{Commons category|Acheloos River}}
* [http://www.beazley.ox.ac.uk/dictionary/Dict/ASP/dictionarybody.asp?name=Acheloos Acheloos] Ancient Greece Iconography at [[John Beazley|Beazley]] Archive ([[Oxford University]])
* [http://www.beazley.ox.ac.uk/dictionary/Dict/ASP/dictionarybody.asp?name=Acheloos Acheloos] Ancient Greece Iconography at [[John Beazley|Beazley]] Archive ([[Oxford University]])
* [https://web.archive.org/web/20041215165032/http://www.ecoguide.gr/en/road/show_road.php3?Id=9 Ecoguides on Achelous]
* [http://encarta.msn.com/encyclopedia_761580324/Akheloos.html] ([http://www.webcitation.org/query?id=1257001490879032 Archived] 2009-10-31) - MSN [[Encarta]]
* [http://www.ecoguide.gr/en/road/show_road.php3?Id=9 Ecoguides on Achelous]
* [https://web.archive.org/web/20050221070823/http://www.aheloos.tv2.gr/ TV2 Travel Channel on Achelous]
* [https://web.archive.org/web/20050207121820/http://aspropotamos.com/english-version.htm Aspropotamos River]
* [http://www.aheloos.tv2.gr/ TV2 Travel Channel on Achelous]
* [http://www.aspropotamos.com/english-version.htm Aspropotamos River]
* [http://www.vourgarelinet.gr/axioth/aheloos/aheloos.htm] (in Greek)
* [http://www.vourgarelinet.gr/axioth/aheloos/aheloos.htm] (in Greek)
* [http://www.evrytan.gr/up0/Ta_Potamia_mas1.htm] (in Greek)
* [https://web.archive.org/web/20041209204802/http://www.evrytan.gr/up0/Ta_Potamia_mas1.htm] (in Greek)
* [http://www.tee.gr/online/epikaira/2000/2123/pg026.shtml] (in Greek)
* [https://web.archive.org/web/20050214112129/http://www.tee.gr/online/epikaira/2000/2123/pg026.shtml] (in Greek)
* [http://www.aspropotamos.com/aspros-history.htm] (in Greek)
* [https://web.archive.org/web/20050211231650/http://aspropotamos.com/aspros-history.htm] (in Greek)
* [http://www.trikalasport.gr/exormisis/prin2003/axeloos.html] (in Greek) - Trikalasport.gr
* [https://web.archive.org/web/20060308200223/http://www.trikalasport.gr/exormisis/prin2003/axeloos.html] (in Greek) - Trikalasport.gr
* [http://www.kliafas.com/aspros0.htm] (in Greek)
* [http://www.kliafas.com/aspros0.htm] (in Greek)
* [http://books.google.com/books?id=03fC3lCOGlsC&pg=PA328&dq=Stratos+Hydroelectric+Dam&hl=en&ei=DlvxS5r4NcL88AbIp7H-Cg&sa=X&oi=book_result&ct=book-thumbnail&resnum=1&ved=0CC0Q6wEwAA#v=onepage&q=Stratos%20Hydroelectric%20Dam&f=false]
* [https://books.google.com/books?id=03fC3lCOGlsC&dq=Stratos+Hydroelectric+Dam&pg=PA328]

{{Authority control}}


[[Category:Achelous River| ]]
[[Category:Achelous basin| ]]
[[Category:Landforms of Aetolia-Acarnania]]
[[Category:Landforms of Arta (regional unit)]]
[[Category:Landforms of Evrytania]]
[[Category:Landforms of Karditsa (regional unit)]]
[[Category:Landforms of Kastoria (regional unit)]]
[[Category:Landforms of Trikala (regional unit)]]
[[Category:Rivers of Greece]]
[[Category:Rivers of Greece]]
[[Category:Rivers of Central Greece]]
[[Category:Rivers of Epirus (region)]]
[[Category:Rivers of Thessaly]]
[[Category:Rivers of Western Greece]]

Latest revision as of 16:58, 9 November 2024

Acheloos
Map
Location
CountryGreece
Physical characteristics
Source 
 • locationPindus mountains
 • coordinates39°41′13″N 21°8′31″E / 39.68694°N 21.14194°E / 39.68694; 21.14194
Mouth 
 • location
Ionian Sea
 • coordinates
38°19′53″N 21°6′5″E / 38.33139°N 21.10139°E / 38.33139; 21.10139
Length220 km (140 mi)
Basin size5,472 km2 (2,113 sq mi)
Discharge 
 • average7,800,000,000 m3 (6,323,563 acre⋅ft) (annual mean)
The Acheloos River marked on a satellite image. Labels in German.
Acheloos River map.

The Achelous (Greek: Αχελώος, Ancient Greek: Ἀχελῷος Akhelôios), also Acheloos, is a river in Epirus, western Greece. It is 220 km (137 mi) long.[1][2] It formed the boundary between Acarnania and Aetolia of antiquity. It empties into the Ionian Sea. In ancient times its spirit was venerated as the river god Achelous.

Herodotus, taking notice of the shoreline-transforming power of the Acheloos River, even compared it to the Nile in this respect:

'There are other rivers as well which, though not as large as the Nile, have had substantial results. In particular (although I could name others), there is the Achelous, which flows through Acarnania into the sea and has already turned half the Echinades islands into mainland.' (2.10, trans. Waterfield)

It is said to have been called more anciently Thoas, Axenus and Thestius.[3]

Course

[edit]

The river Achelous begins at about 2,000 metres (6,600 ft) elevation on the eastern slope of Lakmos mountain in the Pindus range, near the village Anthousa in the westernmost part of the Trikala regional unit. One of its first tributaries is the Aspropotamos, meaning the white river.

The river flows generally southwards, and forms part of the boundary between the regional units of Arta and Trikala, which is also the boundary between Epirus and Thessaly. Further downstream, it forms the boundary of Arta and Karditsa, and further of Aetolia-Acarnania and Evrytania. The river runs into the Kremasta reservoir, which is also fed by the rivers Agrafiotis and Megdovas.

On exiting the Kremasta reservoir, the river flows southwest into Aetolia-Acarnania, feeding the Kastraki reservoir, west of the Panaitoliko range. 10 to 15 kilometres (6.2 to 9.3 mi) downstream from this lake, it flows into the Stratos reservoir. Further downstream, it runs through the lowlands west of Agrinio. It finally empties into the Ionian Sea, 29 km (18 mi) west of Missolonghi.

Settlements

[edit]

In order from upstream to downstream:

Dams

[edit]

There are five dams on the river. From upstream to downstream there is the Mesochora Dam which was completed in 2001 but has not impounded its reservoir. Below that is the Sykia Dam which is partly constructed. Further down is the Kremasta (1965), Kastraki (1969) and Stratos Dams (1989).

Acheloos River in mythology

[edit]
A Roman fresco from Herculaneum depicting Hercules (from Etruscan Hercle and ultimately Greek Herakles) and Achelous (patron deity of the Achelous River in Greece) from Greco-Roman mythology, 1st century AD

History

[edit]

In antiquity, the Achelous was the largest and most celebrated river in Greece, rising in Mount Pindus, and after flowing through the mountainous country of the Dolopians and Agraeans, entered the plain of Acarnania and Aetolia near Stratus, and discharged itself into the Ionian Sea, near the Acarnanian town of Oeniadae. It subsequently formed the boundary between Acarnania and Aetolia, but in the time of Thucydides the territory of Oeniadae extended east of the river. It is usually called a river of Acarnania, but it is sometimes assigned to Aetolia. Its general direction is from north to south. Its waters are of a whitish yellow or cream colour, whence it derives a later name of Aspropotamo or the White river, and to which Dionysius Periegetes probably alludes in the epithet ἀργυροδίνης.[4] Periegetes places the sources of the river near a place called Chalcis.[5] It is said to have been called more anciently Thoas, Axenus and Thestius.[6][7][8][9] In the lower part of its course, the plain through which it flows was called in antiquity Paracheloitis after the river. This plain was celebrated for its fertility, though covered in great part with marshes, several of which were formed by the overflowings of the Achelous.[10]

In 1359 the Battle of Achelous between Albanian forces under Peter Losha and the Despotate of Epirus under Nikephoros II Orsini took place near the river Achelous. Nikephoros II was defeated and killed during the battle, and two new states were established in the area, the Despotate of Arta and the Despotate of Angelokastron and Lepanto.[11]

In the 1960s, the Kremasta Dam in the Aitoloacarnania-Evrytania boundary was under construction. The area is not forested. The dam, made of concrete, took years to complete, eventually flooding a portion of the western part of the prefecture of Eurytania. The dam includes a power station with transformer lines in the east. The dam powers electricity for the western part of Greece and the central part. It caused some soil erosion in some flooded valleys. The Kastraki Dam is downstream and was completed in 1969. Downstream of Katsiki, the Stratos Dam was completed in 1989. The arch bridges includes the Karafilio and the Ardanovo.

The Acheloos River Diversion project has been the center of debate since the 1980s. It calls for four large dams, the Sykia, Mesochora, Mouzaki and Pyli, along with a 17.4 km-long (10.8 mi) channel. The goal of the project is to divert 600,000,000 m3 (490,000 acre⋅ft) annually from the river west towards the Thessaly plains in order to help irrigate 240,000–380,000 ha (590,000–940,000 acres) of mostly cotton crops. Construction on the project has been stalled several times, the latest in 2005, because of environmental and social concerns.

References

[edit]
  1. ^ Greece in Figures January - March 2018, p. 12
  2. ^ "Preliminary Flood Risk Assessment" (in Greek). Ministry of Environment, Energy and Climate Change. p. 49. Archived from the original on 15 February 2020.
  3. ^ William Smith, ACHELO´US, in his Dictionary of Greek and Roman Geography (1854)
  4. ^ Dionysius Periegetes, Description of the World, 432.
  5. ^ Dionysius Periegetes, Description of the World, 496.
  6. ^ Thucydides. History of the Peloponnesian War. Vol. 2.102.
  7. ^ Strabo. Geographica. Vol. pp. 449, 450, 458. Page numbers refer to those of Isaac Casaubon's edition.
  8. ^ Plutarch, de Fluv. 22
  9. ^ Stephanus of Byzantium. Ethnica. Vol. s.v. Ἀχελῷος.
  10. ^ Public Domain Smith, William, ed. (1854–1857). "Acheolous". Dictionary of Greek and Roman Geography. London: John Murray.
  11. ^ Van Antwerp, John (1994). The Late Medieval Balkans: A Critical Survey from the Late Twelfth Century to the Ottoman Conquest. University of Michigan Press. pp. 348â 51. ISBN 978-0-472-08260-5.

Sources

[edit]
[edit]