Earth Surface Dynamics
Earth Surface Dynamics
ESurf
Articles | Volume 8, issue 2
Articles | Volume 8, issue 2
https://doi.org/10.5194/esurf-8-289-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-8-289-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 8, issue 2
Research article
 | 
27 Apr 2020
Research article |  | 27 Apr 2020

Early-to-mid Miocene erosion rates inferred from pre-Dead Sea rift Hazeva River fluvial chert pebbles using cosmogenic 21Ne

Michal Ben-Israel, Ari Matmon, Alan J. Hidy, Yoav Avni, and Greg Balco

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Short summary
Early-to-mid Miocene erosion rates were inferred using cosmogenic 21Ne measured in chert pebbles transported by the Miocene Hazeva River (~ 18 Ma). Miocene erosion rates are faster compared to Quaternary rates in the region. Faster Miocene erosion rates could be due to a response to topographic changes brought on by tectonic uplift, wetter climate in the region during the Miocene, or a combination of both.
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