Gallese Ryes: Difference between revisions
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[[File:Sakoneta, Deba.jpg|300px|thumb|right|Boars Beach, near the town of Helgaray, stands as the characteristical example of sea-by flysch formations across the eastern hemisphere]] | [[File:Sakoneta, Deba.jpg|300px|thumb|right|Boars Beach, near the town of Helgaray, stands as the characteristical example of sea-by flysch formations across the eastern hemisphere]] | ||
Formerly nicknamed the Giant's Road, the Gallese Ryes Geopark is an area located in the east of mainland [[Riamo]], which posesses unique geological {{wp|Flysch}}-type features created by deep water currents and avalanches during the {{wp|Cenozoic}} {{wp|Geologic time scale#Divisions of geologic time|geological era}}. | Formerly nicknamed the Giant's Road, the Gallese Ryes [[Geopark|geological features]] is an area located in the east of mainland [[Riamo]], which posesses unique [[Geology of Riamo|geological]] {{wp|Flysch}}-type features created by deep water currents and avalanches during the {{wp|Cenozoic}} {{wp|Geologic time scale#Divisions of geologic time|geological era}}. | ||
The park's characteristical image is likely to be Boars Beach: a large area where the {{wp|Flysch sediments}} | The park's characteristical image is likely to be Boars Beach: a large area where the {{wp|Flysch sediments}} form a {{wp|wave-cut platform}} and can be observed both as part of the {{wp|cliff|natural sea cliffs}} and as the main component of the bay's surface {{wp|rock}}. | ||
While several other places with such characteristics exist worldwide, the Giant's Road stands out because of its rich {{wp|fossil|fossil record}}, which is often used as the primary chronological reference to date soils and rocks throughout the [[Riamo|Riamese mainland]] and the [[Nostrian Sea|northeastern Nostrian]]. | While several other places with such characteristics exist worldwide, the Giant's Road stands out because of its rich {{wp|fossil|fossil record}}, which is often used as the primary chronological reference to date soils and rocks throughout the [[Riamo|Riamese mainland]] and the [[Nostrian Sea|northeastern Nostrian]]. | ||
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The Gallese Ryes National Park features extensive continuous {{wp|cliffed coast|cliffed coasts}} through its lenght, with minor enclosed beaches in between, most as direct consequence of the {{wp|sedimentary process}} of the uppermost layers of the cliffs. Most of the cliffs feature {{wp|Flysch}}-type features visible from the surface, which constitute the largest compilation of such formations in [[Hirethia]]. | The Gallese Ryes National Park features extensive continuous {{wp|cliffed coast|cliffed coasts}} through its lenght, with minor enclosed beaches in between, most as direct consequence of the {{wp|sedimentary process}} of the uppermost layers of the cliffs. Most of the cliffs feature {{wp|Flysch}}-type features visible from the surface, which constitute the largest compilation of such formations in [[Hirethia]]. | ||
Because of is clarity, the notably homogenous sedimentary plains, and the rich fossil record, the Gallese Ryes' flysch formations served as the base for the | Because of is clarity, the notably homogenous sedimentary plains, and the rich fossil record, the Gallese Ryes' flysch formations served as the base for some of the first [[Geology of Riamo|Riamese geology works]], as well as being one of the main reference points for the creation of several {{wp|Stratigraphic column|stratigraphic columns}} of regions across the [[Nostrian Sea]], including the [[Riamese Stratigraphic Column]]. | ||
The [[National Guri Museum of Geology]] features a permanent exhibition of the [[Riamese Stratigraphic Column]] in the way of a large collection of continuous rock cilinders which were extracted at the nearby town of Helgaray. | The [[National Guri Museum of Geology]] features a permanent exhibition of the [[Riamese Stratigraphic Column]] in the way of a large collection of continuous rock cilinders which were extracted at the nearby town of Helgaray. |
Latest revision as of 15:16, 26 January 2023
Formerly nicknamed the Giant's Road, the Gallese Ryes geological features is an area located in the east of mainland Riamo, which posesses unique geological Flysch-type features created by deep water currents and avalanches during the Cenozoic geological era.
The park's characteristical image is likely to be Boars Beach: a large area where the Flysch sediments form a wave-cut platform and can be observed both as part of the natural sea cliffs and as the main component of the bay's surface rock.
While several other places with such characteristics exist worldwide, the Giant's Road stands out because of its rich fossil record, which is often used as the primary chronological reference to date soils and rocks throughout the Riamese mainland and the northeastern Nostrian.
Flysch
The Gallese Ryes National Park features extensive continuous cliffed coasts through its lenght, with minor enclosed beaches in between, most as direct consequence of the sedimentary process of the uppermost layers of the cliffs. Most of the cliffs feature Flysch-type features visible from the surface, which constitute the largest compilation of such formations in Hirethia.
Because of is clarity, the notably homogenous sedimentary plains, and the rich fossil record, the Gallese Ryes' flysch formations served as the base for some of the first Riamese geology works, as well as being one of the main reference points for the creation of several stratigraphic columns of regions across the Nostrian Sea, including the Riamese Stratigraphic Column.
The National Guri Museum of Geology features a permanent exhibition of the Riamese Stratigraphic Column in the way of a large collection of continuous rock cilinders which were extracted at the nearby town of Helgaray.
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