By Anna Carey
The place do you move while nowhere is safe?
Sixteen years after a perilous virus burnt up such a lot of Earth's inhabitants, the realm is a deadly position. Eighteen-year-old Eve hasn't ever been past the seriously guarded perimeter of her university, the place she and 2 hundred different orphaned women were promised a destiny because the academics and artists of the hot the USA. however the evening earlier than commencement, Eve learns the stunning fact approximately her school's actual purpose-and the scary destiny that awaits her.
Fleeing the single domestic she's ever identified, Eve units off on an extended, treacherous trip, looking for a spot she will be able to live to tell the tale. alongside the way in which she encounters Arden, her former rival from institution, and Caleb, a coarse, rebellious boy residing within the wild. Separated from males her complete lifestyles, Eve has been taught to worry them, yet Caleb slowly wins her belief . . . and her center. He gives you to guard her, but if squaddies start searching them, Eve needs to choose from real love and her life.
In this epic new sequence, Anna Carey imagines a destiny that's either appealing and terrifying. Readers will experience Eve's undying tale of forbidden love and remarkable event.
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Extra resources for Eve (Eve, Book 1)
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.