By Jennifer A. Nielsen
The fake Prince is the exciting first publication in a brand-new trilogy full of probability and deceit and hidden identities that might have readers speeding breathlessly to the end.
In a discontent state, civil battle is brewing. To unify the divided humans, Conner, a nobleman of the court docket, devises a crafty plan to discover an impersonator of the king's long-lost son and set up him as a puppet prince. 4 orphans are recruited to compete for the position, together with a defiant boy named Sage. Sage is aware that Conner's causes are greater than questionable, but his existence balances on a sword's element -- he has to be selected to play the prince or he'll definitely be killed. yet Sage's opponents have their very own agendas as well.
As Sage strikes from a rundown orphanage to Conner's luxurious palace, layer upon layer of treachery and deceit spread, till eventually, a fact is published that, finally, may actually end up extra harmful than all the lies taken together.
An amazing experience packed with possibility and motion, lies and lethal truths that may have readers clinging to the sting in their seats.
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Extra resources for The False Prince (Ascendance Trilogy, 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.