By Jane Lindskold

Initially released below the identify Legends jogging, this is the sequel to Lindskold’s award-winning novel Changer.

A few months have passed by because the occasions in Changer and instances they're a-changing.

Arthur is pressured to manage with no both of his robust correct palms. Eddie has taken off for Africa along with his pal Anson A. Kridd. Vera is experimenting with lifestyles as a mermaid in uncharted ocean realms.

Shahrazad the coyote pup―now proven as athanor, even if her final strength continues to be unknown―is taken via her father, the Changer, to Frank MacDonald’s different 3 Quarters ranch. To her father’s dismay, she indicates no signal of buying the warning she wishes if she is to survive.

Meanwhile, conscious that Arthur’s company keep watch over of the Accord has been weakened, numerous forces search to make the most. Some―like Lilith, Tommy Thunderburst and the satyrs basically desire to assert the fitting to mingle with humanity, yet others have way more ambitious―and sinister―motives.

In Nigeria, a person representing himself as Shopona, God of Smallpox, has published his scourge into town of Monamona. Confronting him is a girl who says she is Oya, an historic and robust goddess. Is Oya athanor or whatever else solely? definitely she is taking part in quickly and free with the key that's the middle of Arthur’s Accord and isn't to be solely trusted.

And what of the wind that encases Monamona in a protecting grab that also is a jail? after all, even the Changer needs to take sides―leaving Shahrazad, his wildly unpredictable daughter, to discover her strengths with no his historic knowledge to lead her.

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Additional info for Changer's Daughter (Athanor, Book 2)

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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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