Difference between revisions of "Besokan river"
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The native [[Proto-Besokian language|Besokian]] term was '''*Kô-Nôwis''' or '''*Kô-Nôwisten''' ‘Great Mother’, hence [[Soskish languages|Soskish]] '''Kônovec''', thought to refer to the river’ significance to early [[Besokian peoples|Besokian culture]]. The [[Besokian languages]] were in turn named after the Besokan. | The native [[Proto-Besokian language|Besokian]] term was '''*Kô-Nôwis''' or '''*Kô-Nôwisten''' ‘Great Mother’, hence [[Soskish languages|Soskish]] '''Kônovec''', thought to refer to the river’ significance to early [[Besokian peoples|Besokian culture]]. The [[Besokian languages]] were in turn named after the Besokan. | ||
==Course and Hydrology== | ==Course and Hydrology== | ||
[[File:Loire in Amboise.jpg|thumb|The Besokan is shallow for most of its upper course, passing fields of sand and gravel, comparable to the Loire in central France.]] | |||
The source of the Besokan is located in the Erkenmian Mountains north of Kernogori. It has no major tributary on its course through the [[Kernogori|Dark Valley]] but is said to be ‘fed by a thousand streams’ as it passes through the fertile landscape, and reaching Dom the river has already grown to a major body of water. From there, it turns south, passing the southeastern end of the Reknayan Wall and entering a narrower valley, the '''Besokan Valley''' proper, between the Herna mountains and the Párian Ridge. For most of its upper course, passing large beds of gravel and sand, and despite its renowned width, the Besokan does not achieve a great depth, remaining relatively shallow until it enters the plain of Tár. The river proceeds in a trough close to the Herna mountains, again fed by countless small streams and growing in sizeuntil it forms Lake Marin immediately north of the gorge of the same name, the southern entrance of Tár. Exiting the gorge and passing Nishûnâc, the remainder of its course is hemmed by rolling hills and dense woodland, the Forests of the Besokan. It mouths into the Gulf of Seligon forming a bar-built estuary between the islands of Golim and Kirospel. | The source of the Besokan is located in the Erkenmian Mountains north of Kernogori. It has no major tributary on its course through the [[Kernogori|Dark Valley]] but is said to be ‘fed by a thousand streams’ as it passes through the fertile landscape, and reaching Dom the river has already grown to a major body of water. From there, it turns south, passing the southeastern end of the Reknayan Wall and entering a narrower valley, the '''Besokan Valley''' proper, between the Herna mountains and the Párian Ridge. For most of its upper course, passing large beds of gravel and sand, and despite its renowned width, the Besokan does not achieve a great depth, remaining relatively shallow until it enters the plain of Tár. The river proceeds in a trough close to the Herna mountains, again fed by countless small streams and growing in sizeuntil it forms Lake Marin immediately north of the gorge of the same name, the southern entrance of Tár. Exiting the gorge and passing Nishûnâc, the remainder of its course is hemmed by rolling hills and dense woodland, the Forests of the Besokan. It mouths into the Gulf of Seligon forming a bar-built estuary between the islands of Golim and Kirospel. | ||
==Cultural Significance== | ==Cultural Significance== | ||
Revision as of 16:49, 13 April 2023
The Besokan is a major river of the eastern Reknaya and the traditional dividing line between Belkondíl and Old Seligon. With a maximal width of over 300 elôrini, it is considered Elondor’s widest river.
Etymology and Names
The name Besokan is of Olgish origin, most likely related to Besok, an ethnonym for to the inhabitants of the Besokan Valley and possibly the lands to its west (largely Soskish and Reknayan populations). The term means ‘gift people’ or ‘fee people’, referring either to valuable gifts brought to Belkdondíl by Soskish merchants or to their function as merceraries, notably as hired cavalrists, in the Olgish kingdoms. The ending -an is a commonly found Olgish nominalizer, or could be a related to the root *an- ‘to proceed, progress’, referring either to the river itself or demarking the area the Besok came from. The term is found denoting the border, or possibly a country, between Belkondíl and (Old) Seligon in the earlier Olgish writings (c. 700 B.E.B.) and by the end Olgish Expansion had been established as the general name for the river.
The native Besokian term was *Kô-Nôwis or *Kô-Nôwisten ‘Great Mother’, hence Soskish Kônovec, thought to refer to the river’ significance to early Besokian culture. The Besokian languages were in turn named after the Besokan.
Course and Hydrology
The source of the Besokan is located in the Erkenmian Mountains north of Kernogori. It has no major tributary on its course through the Dark Valley but is said to be ‘fed by a thousand streams’ as it passes through the fertile landscape, and reaching Dom the river has already grown to a major body of water. From there, it turns south, passing the southeastern end of the Reknayan Wall and entering a narrower valley, the Besokan Valley proper, between the Herna mountains and the Párian Ridge. For most of its upper course, passing large beds of gravel and sand, and despite its renowned width, the Besokan does not achieve a great depth, remaining relatively shallow until it enters the plain of Tár. The river proceeds in a trough close to the Herna mountains, again fed by countless small streams and growing in sizeuntil it forms Lake Marin immediately north of the gorge of the same name, the southern entrance of Tár. Exiting the gorge and passing Nishûnâc, the remainder of its course is hemmed by rolling hills and dense woodland, the Forests of the Besokan. It mouths into the Gulf of Seligon forming a bar-built estuary between the islands of Golim and Kirospel.