subsidence effects
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2013 ◽  
Vol 122 (3) ◽  
pp. 172-183 ◽  
Author(s):  
C Zhang ◽  
R Mitra ◽  
B Hebblewhite
Keyword(s):  

2010 ◽  
Vol 10 (9) ◽  
pp. 1807-1814 ◽  
Author(s):  
H. Akcin ◽  
H. S. Kutoglu ◽  
H. Kemaldere ◽  
T. Deguchi ◽  
E. Koksal

Abstract. Zonguldak Hardcoal Basin is the largest bituminous coal region in Turkey where extensive underground mining activity exists. Because of this activity subsidence effects have been experienced in different locations of the city. In this study, surface deformations caused by the subsidence have been observed by D-InSAR technique using C-Band RADARSAT data. InSAR data process of 16 RADARSAT images acquired between 24 July 2005–23 October 2006 has resulted in significant deformations in the order of about 6 cm in the most populated region of the city. The deformation map obtained has been integrated with digitized mine production maps and Quickbird Orthoimage into GIS. According to GIS analysis, there are three mine seams at different levels driven below the deformed zone. Many governmental and private buildings located in this area have a high potential risk of subsidence damage. Also, this area covers approximately 12 km of transportation routes.


2000 ◽  
Vol 65 (3) ◽  
pp. 525-541 ◽  
Author(s):  
R. Barry Lewis

This article examines the archaeological effects of two major geologic factors, eustatic sea-level rise and land subsidence, on the archaeological site distributions of low-energy coastlines. It describes an inexpensive, quick approach to identify these effects, which exploits the interpretive value of state-maintained archaeological site location files. The application of this approach to the Mississippi Gulf Coast suggests that coastal sites older than roughly 3500 B.P. were submerged or destroyed by eustatic sea-level rise; more recent sites were affected little by this process. Among subsidence factors, endogenic or deep-earth subsidence has had little impact on local site distributions. Exogenic or surficial subsidence processes, however, are sufficient to explain the temporal gradient of tidally inundated marsh sites.


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