Volcanic disruption and drainage diversion of the palaeo-Hudut River, a tributary of the Early Pleistocene Gediz River, Western Turkey

Geomorphology ◽  
2012 ◽  
Vol 165-166 ◽  
pp. 62-77 ◽  
Author(s):  
D. Maddy ◽  
A. Veldkamp ◽  
A.G. Jongmans ◽  
I. Candy ◽  
T. Demir ◽  
...  
2008 ◽  
Vol 189 (1) ◽  
pp. 115-128 ◽  
Author(s):  
Darrel Maddy ◽  
Tuncer Demir ◽  
David R. Bridgland ◽  
Antonie Veldkamp ◽  
Chris Stemerdink ◽  
...  

2012 ◽  
Vol 169 (1) ◽  
pp. 67-82 ◽  
Author(s):  
Darrel Maddy ◽  
Tuncer Demir ◽  
Antonie Veldkamp ◽  
David R. Bridgland ◽  
Chris Stemerdink ◽  
...  

2006 ◽  
Vol 51 (3-4) ◽  
pp. 131-171 ◽  
Author(s):  
Rob Westaway ◽  
Hervé Guillou ◽  
Sema Yurtmen ◽  
Anthony Beck ◽  
David Bridgland ◽  
...  

2015 ◽  
Vol 40 (3) ◽  
Author(s):  
Tuğba Şentürk ◽  
Şükran Yıldız

AbstractObjective: This present investigation aimed at assessing the water quality of the Gediz River located in western Turkey.Methods: Some physicochemical parameters and nutrient concentrations of the surface water of Gediz River were determined over a period of twelve months (October to September 2012) at 5 sampling sites along the river.Results: Data on some ions namely NHConclusion: This indicates pollution of the river water samples from the areas studied. Our findings highlighted the deterioration of water quality of the river due to anthropogenic and agriculturel activities.


2001 ◽  
Vol 138 (2) ◽  
pp. 185-192 ◽  
Author(s):  
J. M. BUNBURY ◽  
L. HALL ◽  
G. J. ANDERSON ◽  
A. STANNARD

The Kula volcanic province lies in an area of active normal faulting in western Turkey. In this study, we show that the interaction of the basalts with the local drainage, and in particular the Gediz river, can be used to determine the history of fault movements downstream. The lava flows have been studied previously, and some of them dated. We use these results and combine them with new field observations of lavas that flowed into the river valley to measure the rate of down-cutting of the river and hence the rate of uplift of the footwall block due to movement of the graben-bounding fault. We show that there has been, in general, an acceleration of fault movement with time during the last 2 Ma. This increased activity of the graben-bounding fault is matched by an intensification of volcanic activity. An inferred four-fold increase in fault movement rate over the last 0.2 Ma has been matched by a similar increase in volume of volcanic activity.


Geomorphology ◽  
2020 ◽  
Vol 358 ◽  
pp. 107102 ◽  
Author(s):  
D. Maddy ◽  
A. Veldkamp ◽  
T. Demir ◽  
A.S. Aytaç ◽  
J.M. Schoorl ◽  
...  

2005 ◽  
Vol 63 (3) ◽  
pp. 339-346 ◽  
Author(s):  
Darrel Maddy ◽  
Tuncer Demir ◽  
David R. Bridgland ◽  
Antonie Veldkamp ◽  
Chris Stemerdink ◽  
...  

2004 ◽  
Vol 391 (1-4) ◽  
pp. 121-169 ◽  
Author(s):  
Rob Westaway ◽  
Malcolm Pringle ◽  
Sema Yurtmen ◽  
Tuncer Demir ◽  
David Bridgland ◽  
...  

2007 ◽  
Vol 26 (22-24) ◽  
pp. 2864-2882 ◽  
Author(s):  
Darrel Maddy ◽  
Tuncer Demir ◽  
David R. Bridgland ◽  
Antonie Veldkamp ◽  
Chris Stemerdink ◽  
...  

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