Sites

THIS IS THE ARCHIVE FOR SAHRIS 1.0


THIS SITE IS NOW AN ARCHIVE AND IS NOT SUITABLE FOR MAKING APPLICATIONS

Please be aware that no content and application creation or changes to information on this version of SAHRIS will be retained.

To make applications or utilise SAHRIS for the creation of information, please use the new site:

https://sahris.org.za

Changes to SAHRIS!

The South African Heritage Resources Information System (SAHRIS) has undergone a generational upgrade and restructure. These changes to the site include, but are not limited to:

  • A new & modernised look and layout
  • Improved site usage flows with respect to applications and content creation
  • Improved site performance and stability

Launch for the new version of SAHRIS occurred on Monday the 30th of October 2023.

The new site can be found here:

SAHRIS | SAHRIS

KAT-SIS08

Group

SiteHeader

SiteID: 

46299

FullSiteName: 

Kathu-Sishen 08

SiteCategory: 

PropertyIsSite: 

No

ReferenceList: 

Relationships: 

Group content visibility: 

Use group defaults

Author: 

sandiswa.mkuba

FeaturedSite?: 

NO
Post date: 02/06/2015
Site Comments:

A low density Middle Stone Age (MSA) scatter was observed along the clean water berm route towards the east
on the farm Sekgame. The artefact scatter is mostly constituted out of debris flakes but single formals stone tools such as side scrapers and points, produced on fine grained specularite, jaspilite and banded iron stone, were recorded. Some of the tools display secondary retouch. Similar Stone Age scatters occur frequently in this area along the banks of the Gamagara River and around water pans and these sites has been the subject of detailed archaeological research studies2. The location of Stone Age scatters in the Sishen area corresponds with a general regional Stone Age site distribution pattern where archaeological sites in the landscape occur near water sources close to local sources of rare raw materials in lithic manufacture. As noted previously, the artefacts can typologically be attributed to the Middle Stone Ages when compared to similar recorded assemblages in the area (e.g. Beaumont & Morris 1990). The site is of limited significance due to low concentration of formal and diagnostic lithics as well as the fact that the context of artefacts has been compromised by natural agents such as erosion.

 
 

Search form