By Jeff Mariotte

The younger Pictish warrior Kral, aided through his dependable cadre of pals, sails to the sinister and unsafe realm of Stygia, at the path of the stolen holy relic that can shop his people—the tooth of the Ice undergo. but even after enduring perils past their darkest goals, they locate that a part of their prize is missing—stolen by means of the duplicitous warrior-thief, Conor.

Journeying into the guts of the Cimmerian wasteland within the useless of wintry weather, Kral and his partners look for their traitorous former comrade while the enraged Picts salary a determined, doomed battle opposed to the nice King Conan himself.

Beset through enemies on all fronts, Kral needs to struggle for ownership of enamel of the Ice endure if he's to avoid wasting his humans from utter annihilation, and declare a future he by no means can have dreamed of…

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Extra resources for Age of Conan: Dawn of the Ice Bear: Dawn of the Ice Bear

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Fig. 3. Nilotic and Levant margins. I, coastal and lacustrine plain (arrow: retreating coast line); 2, continental shelf (SB: shelfbreak); 3, escarpment; 4, marginal plateau (a) and seamount (b); 5, submarine canyon and sea valley; 6, continental rise and deepsea fan (a); 7, erosional moat; 8, basin plain; 10, halokinetic features, dome (a) and low diapir (b); 11, Levant Platform; 14, subduction trench; 16, submarine passage; 17, fracture, fault (a), shear zone (b), buried structure (c); 18, spreading axis (Red Sea).

The most striking characteristic of this sector is the subangular arrangement (northwest-southeast and southwest-northeast) imposed by frontal (westward) and oblique (eastward) subduction. The mounts and ridges are buttelike uplifted features (examples: Matapan and Strabo mounts, respectively 2496 and 711 m) of different size and shape. They may represent outward overturned folds, probably modified by halokinesis. Trenches are deep (to 5 km), irregularly shaped depressions. Their structural and sedimentary discontinuity is attributed to partial blocking by island flanks.

Chart of the Quaternary prodelta of the Var River (Provence), kindly provided by Decca-Survey France. Location shown in Figs. 7. The block-diagram has been computer generated from a digital data bank. The original contour map (at a scale of 1 : 10,000) was prepared from a dense bathymetric line survey (50 m apart), using a narrow beam (6°) echosounder. The chart depicts the narrow deltaic shelf, deep and intense dissection by a radial ravine system, fiat bottom of the Var Canyon (on the left of the diagram) contrasting with the sharp and crenulate crests, and the near-continuity between the subaerial and submerged segments of the Var Valley.

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