By Jeffrey Lord

Richard Blade is an grownup myth pulp novel sequence produced via top Books among 1969 and 1984. The 37 books within the sequence have been written through Roland J. eco-friendly, Ray Nelson, and Manning Lee Stokes below the pseudonym "Jeffrey Lord."

The novels have been additionally published as audio books, and as trilogy units- every one set having edited types of three novels on 6 cassettes (running nine hours, or nearly three hours in step with novel), and in a while cds (1 in keeping with booklet, three consistent with trilogy set, less than the identify "Richard Blade Journeys". those have been published as Americana Audiobooks by means of Americana Publishing in English.

The novels have been a sequence of adventures that includes the titular personality (MI6A's certain agent Richard Blade), who was once teleported right into a random trade size at first of every novel and compelled to depend on his wits and power. alongside the way in which, he may have a number of explicitly defined sexual encounters with attractive ladies (both in England and within the exchange dimensions), and may often go back from his event with a few merchandise, or little bit of wisdom precious to Britain (the ostensible reason behind him being despatched within the first place). Richard Blade used to be exceptionally British, and all of the tales are set in England (at least in the beginning and finish, with Blade being teleported to a couple different measurement for the majority of every tale). The sequence used to be translated into a number of languages, together with Russian, Swedish, French and German.

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Additional resources for Champion of the Gods (Blade, Book 21)

Example text

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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