Aurită Mountains: Difference between revisions

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|Introduction=The '''Cairnwall Mountains''' is a fragmented group of mountains in western [[Arezilur]], forming a rugged divide between [[Minthal]] and the shifting sands of [[Arezilur]]. The Cairnwall is a land of fractured ridges and collapsed stone formations. The desert winds carve through its exposed surfaces, grinding the stone into jagged spires and unstable slopes.

The range is uninhabited, save for a few scattered ruins and remnants of unknown origin. To the northeast, beyond the broken peaks, lies the [[Graveyard of the Fallen]], a vast expanse of toppled boulders and eroded monoliths that mark the transition toward [[~~Terasil~~]] and the [[Fractured Wedge]]. The origins of the Graveyard remain a subject of speculation, with some viewing it as a natural collapse of the mountains, while others claim its a literal graveyard of fallen [[Yairanian|Namuril]] from the [[Great Erosion|Erosion Wars]].

The range is uninhabited, save for a few scattered ruins and remnants of unknown origin. To the northeast, beyond the broken peaks, lies the [[Graveyard of the Fallen]], a vast expanse of toppled boulders and eroded monoliths that mark the transition toward [[Khamria]] and the [[Fractured Wedge]]. The origins of the Graveyard remain a subject of speculation, with some viewing it as a natural collapse of the mountains, while others claim its a literal graveyard of fallen [[Yairanian|Namuril]] from the [[Great Erosion|Erosion Wars]].

|Geography=The Cairnwall Mountains is a low, broken range, with no singular ridgeline, but instead scattered peaks, towering rock spires, and unstable boulder fields. Notable sites include [[Tor-Karoth]], is the highest intact peak in the Cairnwall Mountains, and the [[Graveyard of the Fallen]].

|Geology=The Cairnwall Mountains is composed of eroded granite and sedimentary stone, gradually being consumed by the Arezilur Desert.

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 |Introduction=The '''Cairnwall Mountains''' is a fragmented group of mountains in western [[Arezilur]], forming a rugged divide between [[Minthal]] and the shifting sands of [[Arezilur]]. The Cairnwall is a land of fractured ridges and collapsed stone formations. The desert winds carve through its exposed surfaces, grinding the stone into jagged spires and unstable slopes.
-The range is uninhabited, save for a few scattered ruins and remnants of unknown origin. To the northeast, beyond the broken peaks, lies the [[Graveyard of the Fallen]], a vast expanse of toppled boulders and eroded monoliths that mark the transition toward [[Terasil]] and the [[Fractured Wedge]]. The origins of the Graveyard remain a subject of speculation, with some viewing it as a natural collapse of the mountains, while others claim its a literal graveyard of fallen [[Yairanian|Namuril]] from the [[Great Erosion|Erosion Wars]].
+The range is uninhabited, save for a few scattered ruins and remnants of unknown origin. To the northeast, beyond the broken peaks, lies the [[Graveyard of the Fallen]], a vast expanse of toppled boulders and eroded monoliths that mark the transition toward [[Khamria]] and the [[Fractured Wedge]]. The origins of the Graveyard remain a subject of speculation, with some viewing it as a natural collapse of the mountains, while others claim its a literal graveyard of fallen [[Yairanian|Namuril]] from the [[Great Erosion|Erosion Wars]].
 |Geography=The Cairnwall Mountains is a low, broken range, with no singular ridgeline, but instead scattered peaks, towering rock spires, and unstable boulder fields. Notable sites include [[Tor-Karoth]], is the highest intact peak in the Cairnwall Mountains, and the [[Graveyard of the Fallen]].
 |Geology=The Cairnwall Mountains is composed of eroded granite and sedimentary stone, gradually being consumed by the Arezilur Desert.