By Barb Hendee, J. C. Hendee
In her quest to discover the orb of Spirit, Wynn Hygeorht is torn among males who hate every one other—her vampire protector, Chane Andraso, and the elf Osha, who has emotions for her.
Now a wierd sequence of clues leads them to a distant retain outfitted at the darkish cliffs of the coast of Witeny—where an previous enemy lurks, able to ruin her. whilst, dhampir Magiere, Leesil, and Chap proceed their determined look for the orb of Air. nonetheless hunted by means of a staff of assassins, they get away at the first on hand send, in simple terms to discover themselves below the ability of a sadistic captain.
Yet no matter if they have the capacity to live on this voyage, what waits for them on the journey’s finish is past whatever they could imagine....
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Additional resources for A Wind in the Night (The Noble Dead Saga III, Book 3)
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.