70 results were found for WA 0821 1305 0400 Pengadaan Material Geoteknik Geomat di Sumbawa Nusa Tenggara Barat.

Results:

• 31. Big_landslides_Table_ENG

  Naustavík/Náttfaravíkur by Skjálfandi bay Heavy snowmelt, accumulation of water at the boundary between rock and loose material 1.2 June 1995 Þormóðsstaðir in Sölvadalur in Eyjafjörður Heavy snowmelt, accumulation of water in ancient rockslide deposit 0.6–0.8 March 2007 Morsárjökull Unstable slope by a glacier 4–4.5 April 2007 Stóra-Selfjall in Múladalur/Geithellnadalur in Álftafjörður /media/frettir-myndasafn-2018/Big_landslides_Table_ENG.pdf

• 32. ved-eng-2007

  to the average. December was very stormy and recurrent fierce wind-storms caused some material damages and interrupted air and land communication on several occasions. Except for a two-week period in January, the snow cover in 2007 was very light compared to the long-term mean (1961-1990). /media/vedurstofan/utgafa/skylduskil/ved-eng-2007.pdf

• 33. 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

• 34. Refsgaard_1-Welcome

  physical planners from the Central Denmark Region and Horsens Municipality will be present and comment on the group work on Friday – Two cases, each split in scenario and stakeholder involvement • Water management – Horsens • Road maintenance - Finland • Plenary discussions • Poster session – Monday afternoon Course material • Papers – Download from http://www.fiva.dk/courses.asp?show=92 /media/loftslag/Refsgaard_1-Welcome.pdf

• 35. askja_minnisblad_ens

  means that the failure surface of the slide is concave. The volume of the slide is roughly estimated 30–50 million m3, however, the estimation may change when further measurements and analyses have been carried out, especially on the part that is in the lake and regarding the depth of the sliding surface. If the bottom of the slide reaches below the lake bottom, the total volume of material /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 36. Milly_etal-2008-Stationarity-dead-Science

  6University of Washington, Seattle, WA 98195, USA. 7NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. *Author for correspondence. E-mail: cmilly@usgs.gov. An uncertain future challenges water planners. Published by AAAS on July 12, 201 1 www.sciencemag.or g Downloaded from 1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574 POLICYFORUM combined with opera- tions /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 37. A large landslide falls in Hítardalur valley

  displacements and might be an old landslide deposit. The displaced material is a mixture of e.g. rock debris, scree from the lower part of the hillside, swamp soil and sediments from ancient lakes on the valley bottom. A preliminary estimate of the volume of the slide is 10–20 million m3. The area of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many /about-imo/news/a-large-landslide-falls-in-hitardalur-valley

• 38. Bárðarbunga and Holuhraun - overview

  A list of links to the relevant web-material 20.8.2014 An overview of the Bárðarbunga seismic events and the Holuhraun eruption, 2014 - 2015, is given here with notes, factsheets and observations. New material was added to the top of each monthly article. Combined /earthquakes-and-volcanism/articles/nr/2947

• 39. Pyroclastic flow

  a small amount of their heat to the atmosphere when the currents form. The temperature of the current can vary from 100°C up to 800°C. Depending on the density PDCs can be categorized into two groups. If the column contains a lot of solid material while it collapses it is called pyroclastic flows, however, if the quantity of solid material is low compared to the gases it is called a pyroclastic /volcanoes/volcanic-hazards/pyroclastic-flow/

• 40. A large landslide falls in Hítardalur valley

  displacements and might be an old landslide deposit. The displaced material is a mixture of e.g. rock debris, scree from the lower part of the hillside, swamp soil and sediments from ancient lakes on the valley bottom. A preliminary estimate of the volume of the slide is 10–20 million m3. The area of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many /about-imo/news/a-large-landslide-falls-in-hitardalur-valley/