37 results were found for WA 0821 7001 0763 (MEVVAH) Marble Wall Panels Pemulutan Kabupaten Ogan Ilir Sumatera Selatan.

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1. Articles

with time between the onset of the earthquake swarm on 16 August 2014 (week 0) and today (week 18). The cumulative moment and numbers of events are calculated for each week; that means for each week the earthquakes of certain magnitude ranges were counted and the moment of all earthquakes was simply summed up. Both upper panels show the activity in the dyke, where left panel shows the cumulative moment /earthquakes-and-volcanism/articles/bigimg/3039
2. CES_D2.4_solar_CMIP3

radiation for years 2000-2085, relative to the baseline period 1971-2000 mean. Left panels: south-eastern Finland (62.5◦N, 27.5◦E); right panels: southern Denmark (55◦N, 10◦E). The upper row shows time series for winter, the lower row for summer; note the different scale for the two seasons. The curves represent 30-year running means of the 18-model mean change, separately for the A2 (red), A1B /media/ces/CES_D2.4_solar_CMIP3.pdf
3. Eyjafjallajokull_status_2010-06-15_IES_IMO

and western sides of the crater lake is a wall of ice. On the northern side a tephra wall rises 20 meters above the water. The ice walls at the southwestern corner of the crater are melting, i.e. at the site of the vent that was active 4 – 6 June. The rate of melting is assumed to be about one cuber meter per second. Seismic tremor: Low tremor level. Pulses are observed off and on. Earthquakes /media/jar/Eyjafjallajokull_status_2010-06-15_IES_IMO.pdf
4. IPPC-2007-ar4_syr

of different country groupings in 2004. The percentages in the bars in both panels indicate a region’s share in global GHG emissions. {WGIII Figures SPM.3a, SPM.3b} Regional distribution of GHG emissions by population and by GDPPPP and M&Tand M& T sectoral sources of GHGs in 2004 are considered in Figure 2.1c. {WGIII 1.3, SPM} The effect on global emissions of the decrease in global energy intensity /media/loftslag/IPPC-2007-ar4_syr.pdf
5. Gradual fading of seismic activity at Bárðarbunga and the dyke intrusion

0) and today, 16 December (week 18). The cumulative moment and numbers of events are calculated for each week; i.e. for each week the earthquakes of certain magnitude ranges were counted and the moment of all earthquakes was simply summed up. Both upper panels show the activity in the dyke, where left panel shows the cumulative moment release per week and the right panel the weekly number /earthquakes-and-volcanism/articles/nr/3039
6. Gas concentrations in the Hofsjökull ice cave

those already reported. Oxygen was measured at normal levels, so there is no evidence of carbon dioxide (CO2) accumulation, but this was not measured on these devices. Sulfur dioxide (SO2) was not detected in the cave.An addition hazard is the potential for roof collapse. During another visit in the past week, an ice block sized 2*4*0.4 m was seen to have collapsed from a side wall near /about-imo/news/gas-concentrations-in-the-hofsjokull-ice-cave
7. Increased seismic activity between Krýsuvík and Ölfus

be displaced and wall plastering might be damaged. Severe damage of well-built dwellings is not expected. The intensity of a large earthquake in this region can reach levels VI-VII on the Mercalli Scale. It is important to regularly remind all inhabitants in seismically active regions about potential earthquake hazards. People should review their own security measures and preparedness for a large /about-imo/news/nr/3150
8. ESC-IASPEI-statement-LAquila-2012-1

by IASPEI. of the International Council for Science: the free thinking and conduct of scientific development is a principle of modern society and cannot be hindered or limited by threats of personal retaliation. - When serving on high-level advisory panels for governments and authorities, scientists have the duty to provide the state of knowledge in a comprehensive and unbiased fashion /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf
9. Hare-2011-ParticipatoryModelling

ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec ied .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
10. Landslides

increase Landslides also occur at central volcanoes without any volcanic trigger. An example of this is the rockslide in Askja in 2014 where long term subsidence of a caldera wall, formed in volcanic activity in 1875, caused the slope instability. The slide is considered to be one of the biggest rock slides event in Iceland during historical times. More about this landslide in Icelandic can /volcanoes/volcanic-hazards/landslides/