Scipsy

Earth view (over Brazil, near French Guyana) (by magisstra)

Earth view (over Brazil, near French Guyana) (by magisstra)

Santiago, Cabo Verde (by Paolo Nespoli)
Tsunami live stream

Tsunami live stream

Magnitude 6.3 OFF EAST COAST OF HONSHU, JAPAN  Friday, March 11, 2011 at 06:48:47 UTC
Live Stream
[CNN]: Massive 8.9-magnitude quake hits Japan
[CNN International]: live stream.
Full Earth when viewed from the Moon shines about 50x brighter than the full Moon viewed from Earth.
@Neil deGrasse Tyson

Pyroclastic Flow Remnants at Shiveluch Volcano (by NASA Goddard Space Flight Center)
Pyroclastic flows are some of the most fearsome hazards posed by  erupting volcanoes. These avalanches of superheated ash, gas, and rock  are responsible for some of the most famous volcanic disasters in  history, including the burial of the ancient Roman city of Pompei and  the destruction of Saint-Pierre in 1902. More recently, pyroclastic  flows from Mount Merapi in Indonesia caused most of the casualties  during the volcano’s 2010 eruption.
The intense heat—over 1,000°  Celsius (1800° Fahrenheit)—the terrific speed—up to 720 kilometers (450  miles) per hour—and the mixture of toxic gases all contribute to the  deadly potential. Pyroclastic flows can incinerate, burn, or asphyxiate  people who cannot get out of the flow path.
This false-color  satellite image from the Advanced Spaceborne Thermal Emission and  Reflection Radiometer (ASTER) on the Terra satellite shows the remnants  of a large pyroclastic flow on the slopes of Shiveluch Volcano.  Fortunately, no one was hurt during the eruption and flow in the  sparsely-populated area.
ASTER  detected heat from the flow during or shortly after an event on January  25, 2011. Note how the heat signatures from January line up with the  dark surface deposits visible on February 25; those deposits cover more  than 10 square kilometers (4 square miles). Light brown ash covers the  snow above the flow deposits, and a tiny plume rises from Shiveluch’s  growing lava dome. Vegetation surrounding the volcano is colored dark  red.

Pyroclastic Flow Remnants at Shiveluch Volcano (by NASA Goddard Space Flight Center)

Pyroclastic flows are some of the most fearsome hazards posed by erupting volcanoes. These avalanches of superheated ash, gas, and rock are responsible for some of the most famous volcanic disasters in history, including the burial of the ancient Roman city of Pompei and the destruction of Saint-Pierre in 1902. More recently, pyroclastic flows from Mount Merapi in Indonesia caused most of the casualties during the volcano’s 2010 eruption.

The intense heat—over 1,000° Celsius (1800° Fahrenheit)—the terrific speed—up to 720 kilometers (450 miles) per hour—and the mixture of toxic gases all contribute to the deadly potential. Pyroclastic flows can incinerate, burn, or asphyxiate people who cannot get out of the flow path.

This false-color satellite image from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on the Terra satellite shows the remnants of a large pyroclastic flow on the slopes of Shiveluch Volcano. Fortunately, no one was hurt during the eruption and flow in the sparsely-populated area.

ASTER detected heat from the flow during or shortly after an event on January 25, 2011. Note how the heat signatures from January line up with the dark surface deposits visible on February 25; those deposits cover more than 10 square kilometers (4 square miles). Light brown ash covers the snow above the flow deposits, and a tiny plume rises from Shiveluch’s growing lava dome. Vegetation surrounding the volcano is colored dark red.

Clay’s “Pic of the Day!” An easy one for the Tweeps today! Enjoy your weekend! (via @Clayton C. Anderson)

Clay’s “Pic of the Day!” An easy one for the Tweeps today! Enjoy your weekend! (via @Clayton C. Anderson)

Ostrov Shikotan (or Shikotan-to) is a volcanic island at the southern end of the Kuril chain. At about 43 degrees North—more than halfway to the Equator—Shikotan lies along the extreme southern edge of winter sea ice in the Northern Hemisphere. (via Sea Ice Surrounds Shikotan)

Ostrov Shikotan (or Shikotan-to) is a volcanic island at the southern end of the Kuril chain. At about 43 degrees North—more than halfway to the Equator—Shikotan lies along the extreme southern edge of winter sea ice in the Northern Hemisphere. (via Sea Ice Surrounds Shikotan)

If you were to write a history of the Earth’s past, allowing just one page per year, your book would be 4,600,000,000 pages long. That’s a very thick book — 145 miles to be exact.
Geologic Time

Capital of Jilin province (by Paolo Nespoli)