en directe
Miya Kaneko Kobayashi Oral History Interview, August 11, 2007 [full interview]
Miya Kaneko Kobayashi was born in Crystal City, Texas. Her parents emigrated from Japan to Peru where they operated an import/export business. Their family was forced by the American and Peruvian governments to relocate to a camp in Crystal City where they lived for the remainder of World War II. After the war Kobayashi, her four siblings, and her parents lived in New Jersey for a short time eventually settling near San Diego, California. She has three children from her first marriage. After marrying Kenge Kobayashi, she moved to Eugene in 1989 and continues to work in a construction company. Kobayashi is an avid quilter.She was interviewed by Elizabeth Uhlig for the Japanese-American Association of Lane County, Oregon Oral History Collection (OH 15), Special Collections and Archives Research Center, Oregon State University Libraries.
More
Play
00:00
Play
Seek 10 seconds backwards
Seek 10 seconds forward
00:00 / 00:00
Mute
Settings
Picture in picture
Fullscreen

Heterogeneity of knappable raw material used for chipped stone artifact production at the Mesolithic site of Lepenski Vir. Kristina Saric

20 Octubre, 2015
Inglés
Icona descarregar Descargar
Icona notificar Notificar

SESSION 6 - Characterising lithic sources
Heterogeneity of knappable raw material used for chipped stone artifact production at the Mesolithic site of Lepenski Vir (Serbia)

Lepenski Vir is a Mesolithic-Neolithic archaeological site situated in Eastern Serbia, on the right bank of the Danube River. Although it is most famous for its unique sculptures made of sandstone, it is also significant in terms of stone tools. Mineralogical-petrographical analyses of the investigated collection of chipped stone artefacts, represented by 910 samples, were done in order to characterize the raw material and its provenance. The results of research confirm the heterogeneity of the stone material used for making tools. The majority of the knapped stone tools were made of cherts and radiolarite (around 70%), quartzite (around 20%), acid volcanic rocks and their volcaniclastics (around 6%), whereas silicified limestones, basalts, diorite and gabbro represent the rest of the material.

Llicència Creative Commons by-nc-nd
© Unitat de Producció Audiovisual