77 results were found for WA 0821 1305 0400 Pembuat Lantai Vynil Sticker Rumah Green Building Di Sukaraja Kab Bogor.

Results:

• 51. Avalanche notices on the web - an improved map

  Medium Avalanche Could bury and destroy a car, damage a truck, destroy a small building or break a few trees Snow avalanche could traverse flat terrain (consideralbly below 30°) over distances of less than 50m Size 4 Large Avalanche could bury and destroy a railway car, large trucks, several buildings or a piece of forest Snow avalanche traverses flat terrain (considerably below 30°) over /about-imo/news/nr/2838/

• 52. Supporting structures stopped most of an avalanche

  of the slope below the structures (see the map below). The supporting structures clearly prevented the release of a much larger avalanche. Map of Tvísteinahlíð showing the outline of the avalanche that was released on 19 March 2012 (thick, red curve). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows /avalanches/articles/nr/2475

• 53. Supporting structures stopped most of an avalanche

  ). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows of supporting structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures. The snow cover /about-imo/news/nr/2476/

• 54. Supporting structures stopped most of an avalanche

  red curve). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows of supporting structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures /avalanches/articles/nr/2475/

• 55. PhD Workshop 2012

  are linked to the first four theme areas of the Conference, which are listed at the Conference website as: (1) Risk assessment and impact response (2) Vulnerability and adaptive capacity (3) Building resilience, and (4) Policy development and implementation. However, an additional focus that cuts across these four themes is also pursued for the PhD Workshop, relating to: Decision making /nonam/adaption/phd-workshop-2012/

• 56. Risk Assessment and Stakeholder Involvement

  : What is the difference between adaptation and adaptive management? Participatory planning process - group model building Uncertainty and risk assessment For all topics, presentations both on theory & methods and on case studies will be given. Information and registration All relevant information is available at the workshop's web-pages /nonam/events/nr/1923

• 57. Karlsdottir-Risk_analysis_IMO_SK

  practices, mitigation/adaption measures Land use planning, structural measures (building codes) Early warning systems A comprehensive risk assessment (WMO - model) Knowledge building in the society education, instructions, research, information distribution Social commitment clear role of institutions, law and regulations Mitigation deployment environmental assessment zoning infrastructure /media/loftslag/Karlsdottir-Risk_analysis_IMO_SK.pdf

• 58. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  and environmental policies; it also legitimizes the EU’s Arctic policy among interest groups and the general public. Sustainable design can be referred to the adaptation of energy industries to form newer, ‘green’ methods of producing energy products. (A working paper on this subject will be presented at the NORDCLAD conference.) Also environmental damage reduction, e.g. carbon emissions mitigation /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 59. IMO_AnnualReport2014

  probably a few meters. An interactive 3D model of the earthquakes during the magma intrusion. The di?rent colours represent the activity in time from 16 August to 12 September. During the magma intrusion, intense earthquake activity related to subsidence of the Bárðarbunga caldera was located at the caldera rim. Over 70 earthquakes above magnitude 5 occurred in the first four months after the onset /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 60. VI_2009_006_tt

  than can be expected to originate from the cauldrons, three to four times the wa- ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be 2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich groundwater from the glacier comes from the cauldrons /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf