Geography of Gondara - Revision history

Malaki59 at 07:47, 23 June 2026

2026-06-23T07:47:05Z

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			{{Breadcrumb
			\|1=Main Page\|1label=Home
			\|2=Table of Contents
			\|3=Geography of Gondara
			}}
	★ Foundational Canon		★ Foundational Canon

Malaki59: /* Major Physiographic Systems */

2026-03-26T06:48:56Z

Major Physiographic Systems

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	* [[Vidar Mountain System]] – The primary western mountain barrier, defining Gondara’s rugged western edge and controlling inland movement.		* [[Vidar Mountain System]] – The primary western mountain barrier, defining Gondara’s rugged western edge and controlling inland movement.

	* [[Murkwood ~~Highlands~~]] –A vast eastern mountain system heavily covered in dense forest, defined by continuous ridges, deep hollows, and extremely limited visibility.		* [[Murkwood Mountain System]] –A vast eastern mountain system heavily covered in dense forest, defined by continuous ridges, deep hollows, and extremely limited visibility.

	* [[Great River]] – The main continental waterway flowing from Lake Titania southeast to the ocean, forming Gondara’s primary drainage spine.		* [[Great River]] – The main continental waterway flowing from Lake Titania southeast to the ocean, forming Gondara’s primary drainage spine.

Malaki59: /* Oceanography */

2026-03-26T04:50:04Z

Oceanography

← Older revision		Revision as of 23:50, 25 March 2026
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	== Oceanography ==		== Oceanography ==

	* ~~'''~~[[Embassy Deep]]~~'''~~ – A deep abyssal basin located approximately 36 miles east of the Gondaran mainland and 61 miles southwest of Embassy Island. Reaching depths of roughly 4 miles (6,400 meters), it is one of the deepest known non-trench ocean regions in the South Pacific and defines the southeastern maritime approaches to Gondara.		* [[Embassy Deep]] – A deep abyssal basin located approximately 36 miles east of the Gondaran mainland and 61 miles southwest of Embassy Island. Reaching depths of roughly 4 miles (6,400 meters), it is one of the deepest known non-trench ocean regions in the South Pacific and defines the southeastern maritime approaches to Gondara.

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	* ~~'''~~[[Widow's Reef]]~~'''~~ – Also know as Phantom Isle. A remote reef complex located approximately 150–200 miles southwest of Gondara’s southern coastline, within a loosely defined zone centered near 35°S, 151°W. The feature is believed to consist of a submerged seamount or ridge system whose uppermost structures occasionally approach or breach the ocean surface under rare tidal and sea conditions.		* [[Widow's Reef]] – Also know as Phantom Isle. A remote reef complex located approximately 150–200 miles southwest of Gondara’s southern coastline, within a loosely defined zone centered near 35°S, 151°W. The feature is believed to consist of a submerged seamount or ridge system whose uppermost structures occasionally approach or breach the ocean surface under rare tidal and sea conditions.

	== Surrounding Island Systems ==		== Surrounding Island Systems ==

Malaki59: /* Oceanography */

2026-03-25T11:44:51Z

Oceanography

← Older revision		Revision as of 06:44, 25 March 2026
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	* '''[[~~Widows~~ Reef]]''' – Also know as Phantom Isle. A remote reef complex located approximately 150–200 miles southwest of Gondara’s southern coastline, within a loosely defined zone centered near 35°S, 151°W. The feature is believed to consist of a submerged seamount or ridge system whose uppermost structures occasionally approach or breach the ocean surface under rare tidal and sea conditions.		* '''[[Widow's Reef]]''' – Also know as Phantom Isle. A remote reef complex located approximately 150–200 miles southwest of Gondara’s southern coastline, within a loosely defined zone centered near 35°S, 151°W. The feature is believed to consist of a submerged seamount or ridge system whose uppermost structures occasionally approach or breach the ocean surface under rare tidal and sea conditions.

	== Surrounding Island Systems ==		== Surrounding Island Systems ==

Malaki59: /* Oceanography */

2026-03-25T11:07:23Z

Oceanography

← Older revision		Revision as of 06:07, 25 March 2026
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	* '''[[Widows Reef]]''' – Also know as Phantom Isle. A remote reef complex located approximately 150–200 miles southwest of Gondara’s southern coastline, within a loosely defined zone centered near 35°S, 151°W. The feature is believed to consist of a submerged seamount or ridge system whose uppermost structures occasionally approach or breach the ocean surface under rare tidal and sea conditions.		* '''[[Widows Reef]]''' – Also know as Phantom Isle. A remote reef complex located approximately 150–200 miles southwest of Gondara’s southern coastline, within a loosely defined zone centered near 35°S, 151°W. The feature is believed to consist of a submerged seamount or ridge system whose uppermost structures occasionally approach or breach the ocean surface under rare tidal and sea conditions.

	Due to inconsistent visibility, wave interaction, and historical navigation error, the reef has been associated with numerous conflicting reports, including sightings of a temporary island or landmass appearing and disappearing over time. This has led to its enduring reputation among sailors as a “moving island,” and it remains a poorly charted hazard in deep ocean waters.

	== Surrounding Island Systems ==		== Surrounding Island Systems ==

Malaki59: /* Oceanography */

2026-03-25T11:06:56Z

Oceanography

← Older revision		Revision as of 06:06, 25 March 2026
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	* '''[[~~Moving Island~~ Reef]]''' – A remote reef complex located approximately 150–200 miles southwest of Gondara’s southern coastline, within a loosely defined zone centered near 35°S, 151°W. The feature is believed to consist of a submerged seamount or ridge system whose uppermost structures occasionally approach or breach the ocean surface under rare tidal and sea conditions.		* '''[[Widows Reef]]''' – Also know as Phantom Isle. A remote reef complex located approximately 150–200 miles southwest of Gondara’s southern coastline, within a loosely defined zone centered near 35°S, 151°W. The feature is believed to consist of a submerged seamount or ridge system whose uppermost structures occasionally approach or breach the ocean surface under rare tidal and sea conditions.

	Due to inconsistent visibility, wave interaction, and historical navigation error, the reef has been associated with numerous conflicting reports, including sightings of a temporary island or landmass appearing and disappearing over time. This has led to its enduring reputation among sailors as a “moving island,” and it remains a poorly charted hazard in deep ocean waters.		Due to inconsistent visibility, wave interaction, and historical navigation error, the reef has been associated with numerous conflicting reports, including sightings of a temporary island or landmass appearing and disappearing over time. This has led to its enduring reputation among sailors as a “moving island,” and it remains a poorly charted hazard in deep ocean waters.

Malaki59: /* Oceanography */

2026-03-25T11:05:02Z

Oceanography

← Older revision		Revision as of 06:05, 25 March 2026
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	== Oceanography ==		== Oceanography ==

	* '''Embassy Deep''' – A deep abyssal basin located approximately 36 miles east of the Gondaran mainland and 61 miles southwest of Embassy Island. Reaching depths of roughly 4 miles (6,400 meters), it is one of the deepest known non-trench ocean regions in the South Pacific and defines the southeastern maritime approaches to Gondara.		* '''[[Embassy Deep]]''' – A deep abyssal basin located approximately 36 miles east of the Gondaran mainland and 61 miles southwest of Embassy Island. Reaching depths of roughly 4 miles (6,400 meters), it is one of the deepest known non-trench ocean regions in the South Pacific and defines the southeastern maritime approaches to Gondara.

	----		----
			* '''[[Moving Island Reef]]''' – A remote reef complex located approximately 150–200 miles southwest of Gondara’s southern coastline, within a loosely defined zone centered near 35°S, 151°W. The feature is believed to consist of a submerged seamount or ridge system whose uppermost structures occasionally approach or breach the ocean surface under rare tidal and sea conditions.

			Due to inconsistent visibility, wave interaction, and historical navigation error, the reef has been associated with numerous conflicting reports, including sightings of a temporary island or landmass appearing and disappearing over time. This has led to its enduring reputation among sailors as a “moving island,” and it remains a poorly charted hazard in deep ocean waters.

	== Surrounding Island Systems ==		== Surrounding Island Systems ==

Malaki59 at 06:01, 24 March 2026

2026-03-24T06:01:17Z

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 == Surrounding Island Systems ==
-Gondara exists within a densely populated oceanic environment defined by multiple surrounding island systems extending from its immediate coastal waters to several hundred miles offshore. These systems vary significantly in scale, composition, and habitability, forming distinct maritime zones that influence navigation, contact, and the limits of external access.
+* '''Northern Atoll Field''' – A dense field of low coral atolls extending from approximately 15 to over 150 miles north of Gondara. These formations are numerous, closely spaced, and largely unsuitable for sustained settlement, forming a natural barrier to northern approach.
-=== Northern Atoll Field ===
+* '''Northwestern Island Chain''' – A series of larger volcanic islands to the northwest, representing the primary outer interface between Gondaran maritime activity and the wider Pacific island network. These islands vary in size and influence, with outer portions marking the limits of consistent Gondaran reach.
-North of Gondara lies an extensive field of low coral atolls beginning within approximately 15 miles of the mainland and extending outward beyond 150 miles. These formations are numerous and closely spaced in places, often separated by distances of less than 50 miles, creating a fragmented but continuous maritime environment.
+* '''Northeastern and Eastern Islands''' – Scattered islands and atolls distributed across Gondara’s eastern approaches. These formations are more widely spaced and less dense, reducing their effectiveness as continuous navigation routes toward the mainland.
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Malaki59 at 05:58, 24 March 2026

2026-03-24T05:58:37Z

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 * [[Titanwood Cathedral]] – The largest Titanwood forest valley, known for its immense tree growth and enclosed terrain.
 * [[Talakar Forest]] – A western coastal Titanwood region with dense canopy and high biomass.
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-== Mountain Passes and Corridors ==
+== Surrounding Island Systems ==
-* [[Tamaron Gap]] – A major inland passage through the Vidar system, allowing controlled east–west movement.
+This structure reinforces Gondara’s position not as an isolated landmass in empty ocean, but as a dominant continental presence embedded within a complex and stratified Pacific environment.
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Malaki59: /* Continental Overview */

2026-03-24T05:47:11Z

Continental Overview

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	Gondara is structured by opposing mountain systems, a central inland basin, and a dominant river network that shapes the continent’s climate, movement, and settlement.		Gondara is structured by opposing mountain systems, a central inland basin, and a dominant river network that shapes the continent’s climate, movement, and settlement.
	From the enclosed forests of the east to the open plains and descending steppe of the interior, each region reflects a distinct geographic identity.		From the enclosed forests of the east to the open plains and descending steppe of the interior, each region reflects a distinct geographic identity.

			Gondara’s continental margin is broadest along its northern approaches, where West Vantage and East Vantage occupy the outer edges of the wider shelf system. Southward, the shelf narrows progressively along both coasts until the southern mainland transitions to a steep-margin profile, with deep ocean lying relatively close offshore near South Point and the southeastern approaches.

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