/page/2
distant-traveller:

First X-ray view of Martian soil

This graphic shows results of the first analysis of Martian soil by the Chemistry and Mineralogy (CheMin) experiment on NASA’s Curiosity rover. The image reveals the presence of crystalline feldspar, pyroxenes and olivine mixed with some amorphous (non-crystalline) material. The soil sample, taken from a wind-blown deposit within Gale Crater, where the rover landed, is similar to volcanic soils in Hawaii.
Curiosity scooped the soil on Oct. 15, 2012, the 69th sol, or Martian day, of operations. It was delivered to CheMin for X-ray diffraction analysis on October 17, 2012, the 71st sol. By directing an X-ray beam at a sample and recording how X-rays are scattered by the sample at an atomic level, the instrument can definitively identify and quantify minerals on Mars for the first time. Each mineral has a unique pattern of rings, or “fingerprint,” revealing its presence. The colors in the graphic represent the intensity of the X-rays, with red being the most intense.

Image credit: NASA/JPL-Caltech/Ames

distant-traveller:

First X-ray view of Martian soil

This graphic shows results of the first analysis of Martian soil by the Chemistry and Mineralogy (CheMin) experiment on NASA’s Curiosity rover. The image reveals the presence of crystalline feldspar, pyroxenes and olivine mixed with some amorphous (non-crystalline) material. The soil sample, taken from a wind-blown deposit within Gale Crater, where the rover landed, is similar to volcanic soils in Hawaii.

Curiosity scooped the soil on Oct. 15, 2012, the 69th sol, or Martian day, of operations. It was delivered to CheMin for X-ray diffraction analysis on October 17, 2012, the 71st sol. By directing an X-ray beam at a sample and recording how X-rays are scattered by the sample at an atomic level, the instrument can definitively identify and quantify minerals on Mars for the first time. Each mineral has a unique pattern of rings, or “fingerprint,” revealing its presence. The colors in the graphic represent the intensity of the X-rays, with red being the most intense.

Image credit: NASA/JPL-Caltech/Ames

内臓脂肪は、どうすれば
増えないようにすることができるのでしょう。

運動はもちろんですが、
いちばん大事なのは、寝る前の少なくとも
4時間は食事をとらず、空腹で寝ることです。
私はこれを「4時間ルール」と呼んでいます。
個人差はありますけが、
少なくとも空腹で就寝した場合は
内臓脂肪が分解されるほうに体が働きます。
ところがいくらダイエットをしていても、
寝る前に食事をしてしまうと、
内臓脂肪が合成される方向に働くのです。

pleoros:

NAVIS

Yellowstone

(via pipco)

distant-traveller:

First X-ray view of Martian soil

This graphic shows results of the first analysis of Martian soil by the Chemistry and Mineralogy (CheMin) experiment on NASA’s Curiosity rover. The image reveals the presence of crystalline feldspar, pyroxenes and olivine mixed with some amorphous (non-crystalline) material. The soil sample, taken from a wind-blown deposit within Gale Crater, where the rover landed, is similar to volcanic soils in Hawaii.
Curiosity scooped the soil on Oct. 15, 2012, the 69th sol, or Martian day, of operations. It was delivered to CheMin for X-ray diffraction analysis on October 17, 2012, the 71st sol. By directing an X-ray beam at a sample and recording how X-rays are scattered by the sample at an atomic level, the instrument can definitively identify and quantify minerals on Mars for the first time. Each mineral has a unique pattern of rings, or “fingerprint,” revealing its presence. The colors in the graphic represent the intensity of the X-rays, with red being the most intense.

Image credit: NASA/JPL-Caltech/Ames

distant-traveller:

First X-ray view of Martian soil

This graphic shows results of the first analysis of Martian soil by the Chemistry and Mineralogy (CheMin) experiment on NASA’s Curiosity rover. The image reveals the presence of crystalline feldspar, pyroxenes and olivine mixed with some amorphous (non-crystalline) material. The soil sample, taken from a wind-blown deposit within Gale Crater, where the rover landed, is similar to volcanic soils in Hawaii.

Curiosity scooped the soil on Oct. 15, 2012, the 69th sol, or Martian day, of operations. It was delivered to CheMin for X-ray diffraction analysis on October 17, 2012, the 71st sol. By directing an X-ray beam at a sample and recording how X-rays are scattered by the sample at an atomic level, the instrument can definitively identify and quantify minerals on Mars for the first time. Each mineral has a unique pattern of rings, or “fingerprint,” revealing its presence. The colors in the graphic represent the intensity of the X-rays, with red being the most intense.

Image credit: NASA/JPL-Caltech/Ames

Mount Fuji by Yukio Ohyama

(Source: from89, via suzukichiyo)

pleoros:

Remigiusz Agatowski
Stausee Mooserboden

pleoros:

Remigiusz Agatowski

Stausee Mooserboden

(Source: flickr.com, via pipco)

内臓脂肪は、どうすれば
増えないようにすることができるのでしょう。

運動はもちろんですが、
いちばん大事なのは、寝る前の少なくとも
4時間は食事をとらず、空腹で寝ることです。
私はこれを「4時間ルール」と呼んでいます。
個人差はありますけが、
少なくとも空腹で就寝した場合は
内臓脂肪が分解されるほうに体が働きます。
ところがいくらダイエットをしていても、
寝る前に食事をしてしまうと、
内臓脂肪が合成される方向に働くのです。

"

内臓脂肪は、どうすれば
増えないようにすることができるのでしょう。

運動はもちろんですが、
いちばん大事なのは、寝る前の少なくとも
4時間は食事をとらず、空腹で寝ることです。
私はこれを「4時間ルール」と呼んでいます。
個人差はありますけが、
少なくとも空腹で就寝した場合は
内臓脂肪が分解されるほうに体が働きます。
ところがいくらダイエットをしていても、
寝る前に食事をしてしまうと、
内臓脂肪が合成される方向に働くのです。

"

About:

01

Following: