85 results were found for WA 0821 1305 0400 Total Biaya Untuk Membangun Kantor Per M2 Terpercaya Gambir Jakarta Pusat.

Results:

• 31. VI_2016_006_rs

  and others, 1981), indicat- ing small groundwater storage capacity of the loose materials in the cirques. These fluctuations along with water temperature of close to 0 C during the summertime, indicate that there is per- mafrost in the debris piles in both cirques. The landscape features of the debris piles suggest past deformations due to an ice core. However, there is no evidence suggesting /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 32. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  ; (1) where N is the number of years between the elevation maps, A1 is the average area (m2) of the ice cap over N years, r is the scaling factor from the density of ice (900 kg m3) to water (1000 kg m3), DV D ¯hA2; (2) is the total volume loss (m3), D ¯h is the N year area- average elevation change (m) for the whole ice cap and A2 is the maximum area (m2) of the ice cap. In this study we use /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 33. Bárðarbunga 2014 - September events

  :55 and M4.0 at 06:24, both at the northeastern rim of the caldera. In total 22 earthquakes have occurred in Bárðarbunga since midnight, 14 of them at the northern rim of the caldera and 8 in the southern part. Twelve earthquakes have occurred in the dyke, the largest one ca M2. 28 September 2014 19:00 - from geoscientist on duty No considerable changes can be seen on earthquake activity /earthquakes-and-volcanism/articles/nr/3001

• 34. Bardarbunga-2014_September-events

  :52 at the northern rim of the caldera. Two other were larger than M3.0; M4.2 at 20:55 and M4.0 at 06:24, both at the northeastern rim of the caldera. In total 22 earthquakes have occurred in Bárðarbunga since midnight, 14 of them at the northern rim of the caldera and 8 in the southern part. Twelve earthquakes have occurred in the dyke, the largest one ca M2. 28 September 2014 19:00 - from /media/jar/Bardarbunga-2014_September-events.pdf

• 35. Bárðarbunga 2014 - September events

  :55 and M4.0 at 06:24, both at the northeastern rim of the caldera. In total 22 earthquakes have occurred in Bárðarbunga since midnight, 14 of them at the northern rim of the caldera and 8 in the southern part. Twelve earthquakes have occurred in the dyke, the largest one ca M2. 28 September 2014 19:00 - from geoscientist on duty No considerable changes can be seen on earthquake activity /earthquakes-and-volcanism/articles/nr/3001/

• 36. Bárðarbunga 2014 - November events

  moment is presented as well. These images were made at 26 Nov at 14:21. 28 November 2014 11:30 - from the Scientific Advisory Board Scientists flew over Bárðarbunga on Wednesday, 26 November. According to data acquired in the flight, the total subsidence of the caldera is 50 meters and the volume is 1.4 cubic kilometers. No signal is now received from the station in the caldera /earthquakes-and-volcanism/articles/nr/3023

• 37. Bardarbunga-2014_November-events

  on the third image by the colours orange or bright red. An ordinary webcam photo from the same moment is presented as well. These images were made at 26 Nov at 14:21. 28 November 2014 11:30 - from the Scientific Advisory Board Scientists flew over Bárðarbunga on Wednesday, 26 November. According to data acquired in the flight, the total subsidence of the caldera is 50 meters /media/jar/Bardarbunga-2014_November-events.pdf

• 38. Bárðarbunga 2014 - November events

  moment is presented as well. These images were made at 26 Nov at 14:21. 28 November 2014 11:30 - from the Scientific Advisory Board Scientists flew over Bárðarbunga on Wednesday, 26 November. According to data acquired in the flight, the total subsidence of the caldera is 50 meters and the volume is 1.4 cubic kilometers. No signal is now received from the station in the caldera /earthquakes-and-volcanism/articles/nr/3023/

• 39. Reykholt-abstracts

  of Iceland * Corresponding author, e-mail: sng4 (at) hi.is ABSTRACT Kotárjökull is one of several outlet glaciers draining the ice-covered central volcano Öræfajökull in SE-Iceland. We estimate the average annual specific mass loss of the glacier, to be 0.22 m (water equivalent) per year over the post Little Ice Age period 1891–2011. The glacial recession corresponds to an areal decrease /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 40. norsem_martin

  a total of 325 well-constrained focal mechanisms were obtained using data from the permanent Icelandic SIL seismic network and a temporary network promptly installed in the source region following the main shocks, which allowed a high-resolution stress inversion in short time intervals during the aftershock period. More than 800 additional focal mechanisms /media/norsem/norsem_martin.pdf