By Tanith Lee
The progeny of either god and mortal endures ceaseless conflict in a frozen hell within the moment quantity of the Lionwolf scrolls.
Lionwolf awakes on an surprising shore below a chilly blue solar, without stories store the feeling of being within the lethal womb of the ocean. Others subscribe to him, and so they too can't have in mind who they're or the place they've been. even though Lionwolf can’t keep in mind his name—and, in reality, calls himself Nameless—he sounds like he used to be a king. The twenty-three males at the shore are his military, and shortly they're known as to accountability. Eyeless blue hounds and snake-haired figures driving eight-legged horses lead the lads towards a towering urban the place a bestial mouth trumpets a terrible conflict cry. it truly is Shabatu, a spot of warfare. There, Lionwolf units eyes at the king’s lover, Chillel—the girl who used to be Lionwolf’s wife.
Are Lionwolf and his males lifeless? And is Shabatu maybe their hell?
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Additional resources for Here in Cold Hell (Lionwolf Trilogy, Book 2)
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.