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Age Estimation of Alqosh Main Landslide, North Iraq Using Exposure Dating Method
Iraq Geological Survey, Baghdad.
Luleå University of Technology, Department of Civil, Environmental and Natural Resources Engineering, Mining and Geotechnical Engineering.ORCID iD: 0000-0002-6790-2653
Luleå University of Technology, Department of Civil, Environmental and Natural Resources Engineering, Mining and Geotechnical Engineering.ORCID iD: 0000-0002-1365-8552
2016 (English)In: Journal of Earth Sciences and Geotechnical Engineering, ISSN 1792-9040, E-ISSN 1792-9660, Vol. 6, no 3, 163-176 p.Article in journal (Refereed) Published
Abstract [en]

Alqosh town is located in the central part of north Iraq, along the southernlimb of Alqosh anticline, a rugged mountain with maximum elevation of 837 m(a.s.l.) in the study area. The exposed formation is Pila Spi (Eocene), it consists of thickly well bedded and hard dolostone, dolomitic limestone with some marlintercalations. The dip amount varies from (15 – 45) southwards. The southernlimb of Alqosh anticline is densely dissected by deep valleys; some of them are in canyon form. The spacing between valleys ranges from (115 – 235) m, they all run almost in straight courses downslope, with some slight meandering.Alqosh town is one of the old towns in the vicinity, it dates back to 1000years B.C. with population of about 11 000 inhabitants. In the old part of the town, the houses are built of large blocks of dolostone and dolomitic limestone quarried from the Pila Spi Formation. Due to north of the town, a large and very old landslide exists, the toe has reached the extreme northern part of the town. Tens of houses are built on the toe area; indicating that the landslide is very old. The involved area by the landslide is about 50 000 m2 with length and width of 500 m and (62 – 144) m, respectively. To estimate the age of the landslide, field work was carried out to map the toe area, check about the slid materials and to measure the size of the existing slid blocks and any other evidence of the landslide. The exposure dating method is used to estimate the age of the landslide. The old living people in the town were asked about the age of the houses that are built on the toe to estimate the age of the landslide. Moreover, the covered materials of the toe and other parts of the landslide were carefully inspected to find indications for age estimation. Some archaeological data also were used for age estimation. Depending on all available data, the age of the landslide is estimated to be about 3000 (three thousand) years.

Place, publisher, year, edition, pages
2016. Vol. 6, no 3, 163-176 p.
National Category
Geotechnical Engineering
Research subject
Soil Mechanics
Identifiers
URN: urn:nbn:se:ltu:diva-11424Local ID: a61f4e05-2c58-4349-b327-9e87fee4918aOAI: oai:DiVA.org:ltu-11424DiVA: diva2:984374
Note
Validerad; 2016; Nivå 1; 20160822 (nadhir)Available from: 2016-09-29 Created: 2016-09-29 Last updated: 2017-11-24Bibliographically approved

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