81 results were found for gpt header corruption has(🏅xnseo.cc🏅)gpt header corruption has.SVD.

Results:

• 31. Eyjafjallajokull_status_2010-05-09_IES_IMO

  (a.s.l.): 4-5 km/14-17,000 ft but sometimes shoots up to 6 km /20.000 ft. Heading: Southeast. But low level winds are easterly. Colour: Grey/light gray. Tephra fallout: Farther west now, ashfall started at Þorvaldseyri (south of eruption) around 08:00h, has also been reported at Skógar this morning (7-8 km east of Þorvaldseyri). The ash is black. Lightning: No detections today over /media/jar/Eyjafjallajokull_status_2010-05-09_IES_IMO.pdf

• 32. Eyjafjallajokull_status_2010-05-17_IES_IMO-1

  is drifting east. Colour: Dark-gray at 6 km (seen on webcam). Tephra fallout: Ash has fallen in the Gnúpverjahreppur area, on the road to Stultartangi Power Station and in the Biskupstungur area (very fine- particled and gray). Lightning: Constant lightning (up to 10 flashes per hour) has been detected. Noises: In Hafnarfjörður. Meltwater: Low water discharge at Gígjökull. Conditions /media/jar/Eyjafjallajokull_status_2010-05-17_IES_IMO-1.pdf

• 33. Eyjafjallajokull_status_2010-05-26_IES_IMO

  : Similar as yesterday, estimated through a webcamera. But in the afternoon the visibility has been very poor caused by ash that has been blown up around the volcano. Because of this, the visibility in Vestmannaeyjar was 1 km and 2 km in Vatnsskarðshólar and the volcano could not be seen on the webcameras in the afternoon. Seismic tremor: Volcanic tremor is still more than before /media/jar/Eyjafjallajokull_status_2010-05-26_IES_IMO.pdf

• 34. Factsheet-Bardarbunga-140906

  at Bárðarbunga was measured with the radar system of Isavia’s aircraft. The measurements show large changes on the ice-surface. Up to 15 m subsidence has occurred in the centre of the caldera, which corresponds to a volume change of 0.25 km3. The shape of the subsidence area is in accordance with the elevation of the caldera floor having lowered by that amount. o Subsidence of this order has /media/jar/Factsheet-Bardarbunga-140906.pdf

• 35. Grimsvotn_status_2011-05-23_IES_IMO

  data; weather radar; ashfall reports; UK Met Office ATDnet; MODIS satellite images. Eruption plume: Height (a.s.l.): The ash plume reached heights of 8 to 10 km last night and this morning. In the last hours, the plume has reached heights of 5 to 9 km, but northerly winds have been very strong which can effect the height. Heading: Most of the ash cloud heads to the south /media/jar/Grimsvotn_status_2011-05-23_IES_IMO.pdf

• 36. Eyjafjallajokull_status_2010-05-06_IES_IMO

  at Rauðafell, observed the ash plume to be dark-gray. Observation from ICG: dark. Tephra fallout: Considerable ashfall at Þykkvabæjarklaustur in Álftaver (at a distance of 65-70 km), (everything has turned black). It has not been established whether the ash cloud south of Eyjafjallajökull is ashfall or ash that has already fallen and is being blown from the ground. Ashfall seems to start midway /media/jar/Eyjafjallajokull_status_2010-05-06_IES_IMO.pdf

• 37. Status of unrest in Askja

  inflation related to a shallow magma intrusion which commenced at the start of august 2021. GNSS station OLAC is displayed by the black triangle. Approximately 35 cm of inflation has been measured at this site during the past 12 months. Status of unrest in Askja /about-imo/news/status-of-unrest-in-askja

• 38. Eyjafjallajokull_status_2010-05-20_IES_IMO

  radar measurements, web cameras, ATDnet – UK Met. Offices lightning detection system, NOAA satellite images and web-based ash reports from the public. Eruption plume: Height (a.s.l.): According to radar obersvations, the plume has been at around 5 km/18,000ft. today. Over the volcano, winds blow from the south at 10 m/s, but at the top of the plume the wind is south-southwesterly at 13 /media/jar/Eyjafjallajokull_status_2010-05-20_IES_IMO.pdf

• 39. Flood from Skaftá

  The flood in Skaftá is still ongoing but the discharge has lowered significantly. 10.9.2021 Updated 10.09. 15:25The flood in Skaftá is still ongoing but the discharge has lowered significantly.The water level in Tungulækur, which is a groundwater stream from Eldhraun /about-imo/news/flood-in-estern-skafta

• 40. Re-evaluation needed of the size of the hazard area

  activity was characterized by continuous lava fountains, while the activity changed at around midnight on the 2nd of May, and has since been showing pulsating behaviour. These pulses have intermittent active periods of 8-12 minutes, with 1-2 minutes of rest periods in between. The active pulses start with a strong fountain activity, with fountains reaching up to 100-150 m above ground level, and some /about-imo/news/new-fissure-near-the-eruption-site-in-geldingadalir