72 results were found for WA 0859 3970 0884 Anggaran Biaya Mengecat Rumah Type 50 M2 Argomulyo Salatiga.

Results:

• 11. norsem_giulia

  a major source of hazard for people and infrastructure. Due to the flank instability of volcanic edifices, landslides, or flank collapses, at active volcanoes can trigger major eruptions or produce tsunami waves when the material enters open or enclosed water bodies. A large landslide occurred at Askja Volcano, Iceland, on July 21st, 2014. The landslide had a total volume between 30 and 50 /media/norsem/norsem_giulia.pdf

• 12. Gradual fading of seismic activity at Bárðarbunga and the dyke intrusion

  of events of magnitudes M1-2 (blue), M2-3 (green) and M>3 (red). Both lower panels show the activity on the caldera rim, moment on the left and event numbers on the right, here the colours for the event numbers are M3-4 (blue), M4-5 (green) and M>5 (red). Please notice that the last data point in all plots represents the ongoing week and might thus still change. Further, the y-scale is logarithmic /earthquakes-and-volcanism/articles/nr/3039

• 13. IPPC-2007-ar4_syr

  judgment and statistical analysis of a body of evidence (e.g. observations or model results), then the following likelihood ranges are used to express the assessed probability of occurrence: virtually certain >99%; extremely likely >95%; very likely >90%; likely >66%; more likely than not > 50%; about as likely as not 33% to 66%; unlikely <33%; very unlikely <10%; extremely unlikely <5 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 14. field_report_03032015

  revealed. Gas measurements Driving toward the western side of the crater a degassing vent releasing brownish gases was identified. The site is 10 min walking across the lava field and presents decoloration of rocks. Some gas measurements have been done with two different type of sensors (standard personal and Alphasens ones). Peak concentration of 7 ppm SO2 and 9 ppm CO were observed /media/jar/field_report_03032015.pdf

• 15. VI_2016_006_rs

  was 0.1–0.2 C and the flow was 40–50 l/s (Árni Hjartarson, 2015). The inner Efri-Botnar area is similar to the outer cirque, but the thickness of the debris appears to be somewhat greater. There are ridges and lateral glacier moraines within the cirque and the thickness of the piles of loose materials near the mouth of the cirque is around 6–8 m. Glacier striations from the end of the last ice age can /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 16. Bárðarbunga 2014 - December events

  :55 (24 Dec.) and at 11:02 this morning (25 Dec.). Four more were over 4 in magnitude. In total, around 50 earthquakes were detected in Bárðarbunga. In the dyke intrusion 9 quakes were detected, all under M2. Now 81 km² An overview map from Christmas Eve. The new lava is now 81 km² (80,6 km² + 0,4 km²) in size. Enlarge. Institute of Earth Sciences. 24 December 2014 12:00 - from /earthquakes-and-volcanism/articles/nr/3055

• 17. Bárðarbunga 2014 - December events

  :55 (24 Dec.) and at 11:02 this morning (25 Dec.). Four more were over 4 in magnitude. In total, around 50 earthquakes were detected in Bárðarbunga. In the dyke intrusion 9 quakes were detected, all under M2. Now 81 km² An overview map from Christmas Eve. The new lava is now 81 km² (80,6 km² + 0,4 km²) in size. Enlarge. Institute of Earth Sciences. 24 December 2014 12:00 - from /earthquakes-and-volcanism/articles/nr/3055/

• 18. Bardarbunga-2014_December-events

  earthquakes in Bárðarbunga (northwestern Vatnajökull) since noon yesterday were 4.5 in magnitude at 18:55 (24 Dec.) and at 11:02 this morning (25 Dec.). Four more were over 4 in magnitude. In total, around 50 earthquakes were detected in Bárðarbunga. In the dyke intrusion 9 quakes were detected, all under M2. Now 81 km² An overview map from Christmas Eve. The new lava is now 81 km² (80,6 km /media/jar/Bardarbunga-2014_December-events.pdf

• 19. Lawrence_Deborah_CES_2010

  -2050 30-year flood XX Flood frequency estimation applied to annual maximum flood series % change in 200-year flood Projected change in 200-yr. flood between 1961-1990 and 2021-2050 Change (%) 90th percentile of 150 models Median of 150 models Change (%) Range of uncertainty in projections Median of 150 models Change (%) Range (%) Range 10 to 90% Downscaling method 0 10 20 30 40 50 60 70 80 90 /media/ces/Lawrence_Deborah_CES_2010.pdf

• 20. Bardarbunga_kafli20140825

  frequency during the last 1100 years is 1 eruption per 50 years on average. Eruptions on the ice covered part of the system have the potential to cause major floods in several rivers flowing southwards and northwards from the Vatnajökull ice cap. _________________________________________________________________________ Central volcano: Bárðarbunga Lat, lon: 68°38´N, 17°31´W Elevation: 2009 /media/jar/Bardarbunga_kafli20140825.pdf