Pliocene and Quaternary regional uplift in western Turkey: the Gediz River terrace staircase and the volcanism at Kula

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


2008 ◽  
Vol 189 (1) ◽  
pp. 115-128 ◽  
Author(s):  
Darrel Maddy ◽  
Tuncer Demir ◽  
David R. Bridgland ◽  
Antonie Veldkamp ◽  
Chris Stemerdink ◽  
...  

Geomorphology ◽  
2012 ◽  
Vol 165-166 ◽  
pp. 62-77 ◽  
Author(s):  
D. Maddy ◽  
A. Veldkamp ◽  
A.G. Jongmans ◽  
I. Candy ◽  
T. Demir ◽  
...  

2005 ◽  
Vol 63 (3) ◽  
pp. 339-346 ◽  
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 ◽  
...  

2020 ◽  
Vol 29 (1) ◽  
pp. 33-57
Author(s):  
V.M. Loskot ◽  
G.B. Bakhtadze

Geographic distribution and habitat preferences of Saxicola rubicola rubicola (Linnaeus, 1766), S. maurus variegatus (S.G. Gmelin, 1774), and S. m. armenicus (Stegman, 1935) inhabiting the Caucasian Isthmus and adjacent areas are described in detail. We examined the individual, sexual, age, seasonal and geographical variations of seven main diagnostic features of both plumage and morphometrics (exactly, the length of wing and tail) using 381 skin specimens. Substantially improved diagnoses of S. m. variegatus and S. m. armenicus are provided. After a thorough examination of the materials and history of the expedition of Samuel Gmelin in 1768–1774, and his description of Parus variegatus, it was concluded that the type locality of this taxon was the vicinity of Shamakhi in Azerbaijan not Enzeli in North-Western Turkey. It is also shown the fallacy of the recently proposed attribution of the holotype of the northern subspecies S. m. variegatus to the southern taxon S. m. armenicus and synonymisation of these names, as well as the replacement of the name S. m. variegatus by its junior synonym S. m. hemrichii Ehrenberg, 1833 for the northern subspecies.


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