13 results were found for 강원소개팅어플「카톡@secs4」카톡@secs4 강원매너만남 강원폰섹∞강원거유㉤강원만남톡 じ㴵 delineation.

Results:

• 11. VI_2016_006_rs

  wide and 1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 12. 2010_012rs

  thus enabling the delineation of active faults in near-real time. Foreshocks preceding a large earthquake by more than 20 minutes will already have been located with high precision before the main shock occurs, and may already have delineated the fault plane of the coming main shock, thus allowing its faulting mechanism to be immediately inferred. Due to its size, the main shock /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 13. VI_2014_001

  6 0 20 40 60 80 10 0 12 0 14 0 −ln(−ln(1−1/T)) Q( T) (m ?s) 1 2 5 10 20 50 100 T (years) l Obs. WaSiM vhm51 heM 95?bh ??Obs 95?bh ??W aSiM 95?bh heM Annual max. Q : GEV Distributions for vhm51 Index flood model no. 6 l l l l l l l l l l l l l l l l l l −2 0 2 4 6 0 50 10 0 15 0 −ln(−ln(1−1/T)) Q( T) (m ?s) 1 2 5 10 20 50 100 T (years) l Obs. WaSiM vhm52 heM 95?bh Obs 95?bh /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf