By George R. R. Martin

BUZ VE ATEŞİN ŞARKISI II

Krallar çarpışırken tüm diyar titrer...

George R. R. Martin, Taht Oyunları'nın sabırsızlıkla beklenen devam kitabı Kralların Çarpışması'nda okuyucuları eşsiz hayal gücüyle buluşturuyor. Büyü, intikam ve savaşla dolu, eşi benzeri görülmemiş bir dünyanın kapıları açılırken büyük bir serüven başlıyor.

Alev ve kan rengine bürünmüş bir kuyruklu yıldız, gökyüzünü baştan başa kaplamıştır. Ejderha Kayası'nın kadim kalesinden, Kışyarı'nın haşin topraklarına kadar korkunç bir keşmekeş hâkimdir. Altı güç, Demir Taht'ı ve parçalanmış Yedi Krallık'ı ele geçirmek için kıyametvari bir savaşa hazırlanmaktadır. Gecenin karanlığında ölüler yürümekte, kardeş kardeşi katletmektedir. Bir akıl şövalyesi, tehlike saçan bir büyücü kadını zehirlemek peşindedir. Bir prenses, öksüz oğlan kılığında dolaşmakta; Ay Dağları'nın vahşi adamları, yağma için inmektedir. Kardeş katli, zillet, simya ve kıyımla ilerleyen bu macerada zafer, kılıcı ve kanı en soğuk olanların dahi olabilir...

"Martin, birinci ciltteki vaadini fazlasıyla yerine getiriyor ve yazılmış en iyi fantastik eser olmaya aday serisine devam ediyor."

The Denver Post

"George Martin kesinlikle destansı fantastik edebiyatın yeni ustalarından."

Katharine Kerr

"Kendisinden her zaman en iyi işleri beklediğim George R. R. Martin beni asla şaşırtmıyor."

Robert Jordan

"Muhteşem bir öykü, muhteşem bir tarihi fantastik yapıt! Göz kamaştırıcı."

Anne McCaffrey

"Muhtemelen gelmiş geçmiş en iyi epik fantastik eser."

Marion Zimmer Bradley

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Additional resources for Game of Thrones Buz ve Ateşin Şarkısı Kralların Çarpışması 2.Kitap

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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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