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1). very separates (Fig. CHAPTER 34 2 from the adjacent phyllite series. The farmstead building is on the dolomite contact (in the parking area). The immediately adjacent to the phyllite to light gray, to is predominantly dark dolomite gray, but itweathers gray or white. It is massively bedded, with the bedding planes grayish brown, so the local dip and strike. , large the other hand, the dolomite along the contact with the phyllite into angular rock fragments. They have is highly fractured or brecciated been recemented together, indicating brittle fracture during overthrusting.

5. Metacarbonate Figure tion near the metallurgy foliation as dominant features, and so we have chosen to call these rocks metacarbonates Next (Fig. 5). above the Phyllite nappe is another carbonate series, theTripolitza nappe, comprising massively bedded and reefal carbonates and dolomites. Rocks of the Tripolitza in the far east of Crete, nappe are widespread especially south and east of Siteia. Still higher in the pile are the Pindos and Subpelagonian in eastern nappes, which are less widely distributed are Crete.

31. Flemming, Czartoryska, and 1973, table 1. 32. Soles 1978. and Hunter this now sea. the Flemming, 1973. 34. lier 5. Czartoryska, et al. 1976, and p. 7. Cliffs north of the metal lurgy site, looking toward the island of Pseira Local Bedrock site is on an isolated point of land metallurgical Chrysokamino m above the sea with no immediately about 38 adjacent boat perched a but site is backed available. The by sharp, passable ridge rising landing The another 80 m without areas. The point of land where the cove on the north side (Fig.

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