Results of ground penetrating radar sounding


View Original Image at Full Size

Fig. 4: Compared to ERT, investigations using GPR deliver additional data on internal subsurface structure. Herein, the near surface permafrost table (3 - 4 m) could be clearly distinguished from underlying massive ground ice (~ 12 - 15 m), whereas ERT just shows a successive increase in resistivity.

Image 14993 is a 1726 by 1890 pixel JPEG
Uploaded: Apr14 09


Permanent URL: http://serc.carleton.edu/download/images/14993/results_ground_penetrating_rad.jpg

The file is referred to in 1 page
Provenance
Jan-Christoph Otto
Reuse
This item is offered under a Creative Commons Attribution-NonCommercial-ShareAlike license http://creativecommons.org/licenses/by-nc-sa/3.0/ You may reuse this item for non-commercial purposes as long as you provide attribution and offer any derivative works under a similar license.