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Pigment-containing materials (Hematite)

Hematite is large-lamellar aggregates with multidirectional leaflets, sometimes replaced by goethite. It belongs to the group of natural pigments that have a high iron content (20-50%). The paints with different shades of red are extracted from it. 

The very high iron content in the composition (82,5%) and the low content of other elements confirm the natural origin of this sample.


Manufacturing technique

Fragments with hematite were split off the pieces of initial raw materials. Fragments were grinded up and then they were used for the paint manufacturing. 

 


Use-wear traces

The sample of hematite has a smoothing along the contour. 


Storage location

North-Eastern State University, Magadan city

Inventory number

Ушки-V-2007

The Museum KAMIS

No

Material

Hematite

Dating

13300 – 12500 years BP

Culture

Ushki V site, cultural layer VII, transition from the Paleolithic to the Neolithic, the end of the Pleistocene.

The author of the excavations

Ponkratova I.Yu.
2007

Publications

Ponkratova I. Yu., Gubar Yu. S., Lbova L. V. Spektralnyy analiz okrashennykh artefaktov sloya VII stoyanki Ushki V (poluostrov Kamchatka) // Universum Humanitarium. 2019. № 1. S. 56–71.


Page authors: Yu. Gubar, I. Ponkratova, L. Lbova