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PBRs were limited to varnish microlamination (VML) dating techniques and sparse cosmogenic nuclide data; however, VML methods yield.
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Geochemical studies on rock varnish and petroglyphs in the Owens and Rose Valleys, California
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Additional parts of the study include VML dating techniques and new geovisualization techniques of the rock art and RASI factors used to.
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Ronald Dorn. After recognition that debris flows co-occur with human activities, the next step in a hazards analysis involves estimating debris-flow probability. Prior research published in this journal in used varnish microlamination VML dating to determine a minimum occurrence of 5 flows per century over the last years in a small mountain range of South Mountain adjacent to neighborhoods of Phoenix, Arizona. This analysis led to the conclusion that debris flows originating in small mountain ranges in arid regions like the Sonoran Desert could pose a hazard.
Two major precipitation events in the summer of generated 35 debris flows in the same study area of South Mountain—providing support for the importance of probability analysis as a key step in a hazards analysis in warm desert settings. Two distinct mechanisms generated the debris flows: intense precipitation on steep slopes in the first storm; and a firehose effect whereby runoff from the second storm was funneled rapidly by cleaned-out debris-flow chutes to remobilize Pleistocene debris-flow deposits.
When compared to a global database on debris flows, the storms were among the most intense to generate desert debris flows — indicating that storms of lesser intensity are capable of generating debris flows in warm desert settings. Thus, wetter climatic periods of intense rock decay are not needed to resupply desert slopes with fines; instead, a combination of dust deposition supplying fines and dirt cracking generating coarse clasts can re-arm chutes in a warm desert setting with abundant dust.
N2 – After recognition that debris flows co-occur with human activities, the next step in a hazards analysis involves estimating debris-flow probability. AB – After recognition that debris flows co-occur with human activities, the next step in a hazards analysis involves estimating debris-flow probability. Overview Fingerprint.
Abstract After recognition that debris flows co-occur with human activities, the next step in a hazards analysis involves estimating debris-flow probability.
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ISSN Rock varnish microlamination -based age estimates of surface geological and geoarchaeological features boulders, cobbles and artifacts are different in principle and independent of both cation-ratio and AMS 14 C dating methods. Analyzed surface scatters geological and cultural artifacts collected at Planchada la Puntilla PLP archaeological site suggest a minimum surface-exposure age estimate 6,, years BP, and a minimum age estimate of artifact scatters 5,, years BP.
Further, as the layering sequence of varnish microlamination includes a climate record, it is a unique tool to discuss past climatic change in an area where it has been difficult to find more traditional proxies.
Rock varnish microlamination VML dating uses the slow buildup of ‘varnish’ or dark coating on subaerially exposed rock surfaces. It is particularly well preserved and therefore useful in arid and semi-arid regions. Dark layers in varnish are rich in Mn and Ba, but poor in Si and Al. Orange and yellow layers are poor in Mn and Ba, rich in Si and Al. There is also a growing body of evidence that indicates varnish microstratigraphy carries climate record: Mn-poor yellow layers formed during dry periods, Mn-rich black layers deposited during wet periods.
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