78 results were found for WA 0859 3970 0884 Pesan Canopy Baja Ringan Atap Go Green Ungaran Barat Kab Semarang.

Results:

• 41. “The small eruption” in

  to measure the composition and the flux rate”, says Melissa.Figure 8. Gas is one of the hazards from the volcano. The specialists from IMO go regularly to the eruption site to measure the composition and emission rate of the gases. They need to wear special equipment to protect themselves from the gas and to make the measurements. In the photo Melissa Anne Pfeffer is preparing Baldur Bergsson /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months

• 42. “The small eruption” in

  to measure the composition and the flux rate”, says Melissa.Figure 8. Gas is one of the hazards from the volcano. The specialists from IMO go regularly to the eruption site to measure the composition and emission rate of the gases. They need to wear special equipment to protect themselves from the gas and to make the measurements. In the photo Melissa Anne Pfeffer is preparing Baldur Bergsson /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/

• 43. Lava flows

  : Type of the magma and its viscosityThe steepness of the slope surface.If the magma flows as one big spread or in a narrow channel or a magma tunnel.The rate of the magma coming from the ventBasaltic magma can flow tens of kilometers from the eruption vent and the margin of the lava can go up to 10 km/hour depending on slope. Usually the transport time is shorter, but if the slope gradient /volcanoes/volcanic-hazards/lava-flow/

• 44. ESC-IASPEI-statement-LAquila-2012-1

  of IASPEI's most brilliant scientists, who dedicated their lives to the reduction of seismic risk and to whom go our sympathy and support. , on behalf of the world community of seismologists, expresses its deepest concern for the L’Aquila verdict and prison sentence, that condemns for involuntary manslaughter seven prominent Italian scientists and members of the Great Risks Commission /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf

• 45. Moberg_Anders_CES_2010

  1500 years and IPCC future temperature scenarios • Significant climate changes have occurred in the last millennium – affecting both temperature and hydrology • Future changes in this century will likely go substantially beyond what we have seen in the recent past IPCC 2007, SPM Fig. 5Mann et al. Science 2009, 326, p.1257, Fig. 1 /media/ces/Moberg_Anders_CES_2010.pdf

• 46. norsem_slunga

  are as large as the friction allows) directly leads to boundaries on the k-values and that these curves not only has a simple physical meaning, they also show a significant difference from the numerical fitting. This encouraged me to later go on and use the same assumptions to put boundaries on the pore pressure within wet crust which then was the base for the QuakeLook complete stress /media/norsem/norsem_slunga.pdf

• 47. Hare_2-participation

  and groups come and go frrom processes (how do you keep them turning up year after year?) • Participatory burn-out – legislators want it everywhere – too often with not enough results 5. Overselling of participation the tyranny of participation? Cooke & Kothari (2000) • Experiences in Cooperation and Development projects – Ignorance of existing power structures in local communities • Which /media/loftslag/Hare_2-participation.pdf

• 48. vanRoosmalen_etal-2009-WRR_2007WR006760

  and evapotranspiration to the surface and groundwater system. The vegetation type deter- mines the transpiration properties through the crop factor and the root depth, and the fraction of precipitation that is intercepted by the canopy. Land use changes can therefore reduce or amplify future climate change induced hydrological impacts in a catchment. [3] A number of studies have focused on the effects /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 49. Update on the earthquake swarm in Geldingadalir

  there were around 1300 earthquakes detected in the Reykjanes peninsula as a whole. This is a lot less than the day before when around 2300 earthquakes were detected. The scientific Advisory board for the civil protection services met on the 27th of December to go over the situation near Fagradalsfjall. GPS instruments and satellite interferograms show that the magmatic intrusion is limited /about-imo/news/update-on-the-eruption-in-geldingadalir

• 50. Update on the earthquake swarm in Geldingadalir

  there were around 1300 earthquakes detected in the Reykjanes peninsula as a whole. This is a lot less than the day before when around 2300 earthquakes were detected. The scientific Advisory board for the civil protection services met on the 27th of December to go over the situation near Fagradalsfjall. GPS instruments and satellite interferograms show that the magmatic intrusion is limited /about-imo/news/update-on-the-eruption-in-geldingadalir/