Articles | Volume 9, issue 3
Earth Surf. Dynam., 9, 463–485, 2021
https://doi.org/10.5194/esurf-9-463-2021
Earth Surf. Dynam., 9, 463–485, 2021
https://doi.org/10.5194/esurf-9-463-2021

Research article 02 Jun 2021

Research article | 02 Jun 2021

Implications of the ongoing rock uplift in NW Himalayan interiors

Saptarshi Dey et al.

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Saptarshi Dey on behalf of the Authors (14 Sep 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (25 Sep 2020) by Richard Gloaguen
RR by Stefan Hergarten (20 Oct 2020)
RR by Yann Gavillot (26 Oct 2020)
ED: Reconsider after major revisions (26 Oct 2020) by Richard Gloaguen
AR by Saptarshi Dey on behalf of the Authors (07 Dec 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (10 Mar 2021) by Richard Gloaguen
RR by Anonymous Referee #2 (22 Mar 2021)
RR by Stefan Hergarten (23 Mar 2021)
ED: Publish subject to minor revisions (review by editor) (23 Mar 2021) by Richard Gloaguen
AR by Saptarshi Dey on behalf of the Authors (01 Apr 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (06 Apr 2021) by Richard Gloaguen
ED: Publish subject to technical corrections (19 Apr 2021) by A. Joshua West(Editor)
AR by Saptarshi Dey on behalf of the Authors (25 Apr 2021)  Author's response    Manuscript
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Short summary
Ongoing deformation of the Himalaya is not constrained to its southern extremity. With morphometric analysis using a high-resolution digital elevation model, satellite image analysis, luminescence chronology of fluvial terraces and field observations, we identify a zone of rapid rock uplift in the interior of the Kashmir Himalaya. Our results suggest active tectonic and structural control on the growth of topography in the Himalayan interiors over multi-millennial timescales.