By Stephen R. Donaldson

The long-awaited sequel to The Runes of the Earth returns readers to the Land-and opens with the reunion of Linden Avery and Thomas Covenant!

Linden Avery, who enjoyed Thomas Covenant and watched him die, has again to the Land looking for her abducted son, Jeremiah. As Fatal Revenant starts off, Linden watches from the battlements of Revelstone whilst the most unlikely occurs- driving prior to the hordes attacking Revelstone are Jeremiah and Covenant himself, it appears greatly alive.

the following within the Land, Jeremiah is healed of the psychological situation that had saved him mute and unresponsive for thus decades. he's energetic, and dedicated to Covenant. yet Covenant is unusually replaced. Sarcastic and bragging, he not sounds like the guy whom Linden cherished. And but he says he has a plan: he'll take her and Jeremiah to a spot the place they could discover a natural resource of Earthpower and, after he has completed his personal reasons, Linden can be unfastened to take advantage of that groovy energy to move domestic, to take Jeremiah domestic, or to do anything she sees healthy. even if she distrusts the likely assorted guy he has now develop into, how can she make any selection other than to stick to him?

Their trip will hide unbelievable distances during the Land-even via time itself-and will try Linden's braveness many times. in spite of everything, enjoyable her future will demand a bad jump of religion: Can she quit every thing she proposal have been restored to her, for the sake of the Land?

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Extra info for Fatal Revenant (The Last Chronicles of Thomas Covenant, 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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