On the Surface: Catalhoyok, 1993-95 (McDonald Institute Monographs): v. 3. 0951942034, 9780951942031

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McDONALD INSTITUTE MONOGRAPHS

On the surface: C::atalhOyiik 1993-95 Edited by Ian Hodder

IMERkO) BRITISH INSTITUTE OF ARCHAEOLOGY AT ANKARA

•

McDONALD INSTITUTE MONOGRAPHS

On the surface:

N

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x

25,---------------------------------------------------------------------------------------·

• platform/bin

Obench

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Re-opening C::a talhoyuk

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10m Figure 1.9. Redrawn plan of Mellaart's level IT.

Figure 1.10. Redrawn plan of Mel!aart's level Ill.

11

Ian Hodder

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Figure 1.13. Redrawn plan of Mellaart's level VIA.

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Figure 1.14. Redrawn plan of Mellaart's level VIB.

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Geoarchaeological Investiga tions

0

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%

%

Organic Matter Content

CaC0 3 Equivalent

I::) Marl 1:::::1 Charcoal 0 Olive G Grey

I Plaster

2 Redeposited Marl

Figure 2.3. Core (H.94-A: lithology and measured parameters. 27

I

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0

0.3

0.6

0.9

xtf

( JlrJ

kg" I)

Organic Clay

Neil Roberts, Peter Boyer & Romola Parish

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Upper Alluvial Clay

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Organic Clay

Bivalve [ ] Mollusc Shells

(See text for details of lithological units )

Figure 2.9. (ar~amba palaeochannel PCI: recorded stratigraphy (1994), north-facing section. (Note exaggerated

vertical scale.) 7

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% Organic Matter Content

Figure 2.10.

(ar~amba

12

0

20 30 40 50 % CaC0 Equivalent

10

3

0.4 0.8 1.2 1.6 0 Mass Specific Magnetic Susceptibility

palaeochannel PCJ: measured parameters for each stratigraphic unit. 34

(~1m 3 kg- 1)

Geoarchaeological Investigations

minerals in the deposits, presumably with some diamagnetics as well. This correlates well with the high carbonate readings, as calcium carbonate is weakly diamagnetic with a mass specific magnetic susceptibility (X) of -0.0048 J..lm3 kg-1 (Dearing 1994). A number of paramagnetic silicates (0.01-0.95 J..lm3 kg- 1) may also have been present, as well as dolomite (CaMg(C03 ) 2) -t

row

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