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SILICATES, LM Silicon wafer
 
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SILICATES, LM Silicon wafer

UIS5078699

SILICATES, LM Silicon wafer

UIS5078699

SILICATES, LM Sodium silicate
 
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SILICATES, LM Sodium silicate

UIS5078732

SILICATES, LM Sodium silicate

UIS5078732

SILICATES, LM Sodium silicate
 
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SILICATES, LM Sodium silicate

UIS5078622

SILICATES, LM Sodium silicate

UIS5078622

Advert for Silicated Carbon Filter Company 1888
 
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Advert for Silicated Carbon Filter Company 1888

EPL6812128

Advert for Silicated Carbon Filter Company 1888

EPL6812128

SILICATES, LM Colloidal silica deposit on steel
 
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SILICATES, LM Colloidal silica deposit on steel

UIS5078380

SILICATES, LM Colloidal silica deposit on steel

UIS5078380

Hemimorphite (photo)
 
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Hemimorphite (photo)

NHM1451865

Hemimorphite (photo)

NHM1451865

Slab of the Lueders meteorite
 
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Slab of the Lueders meteorite

NHM1459227

Slab of the Lueders meteorite

NHM1459227

Cordierite (photo)
 
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Cordierite (photo)

NHM1451908

Cordierite (photo)

NHM1451908

Heulandite (photo)
 
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Heulandite (photo)

NHM1453514

Heulandite (photo)

NHM1453514

Asbestos (photo)
 
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Asbestos (photo)

NHM1455079

Asbestos (photo)

NHM1455079

SILICATES, LM Interference layer with colloidal silica de Interference layer with colloidal silica deposit
 
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SILICATES, LM Interference layer with colloidal silica de Interference layer with colloidal silica deposit

UIS5078703

SILICATES, LM Interference layer with colloidal silica de Interference layer with colloidal silica deposit

UIS5078703

SILICATES, LM Silicon wafer with colloidal silica deposit Silicon wafer with colloidal silica deposit
 
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SILICATES, LM Silicon wafer with colloidal silica deposit Silicon wafer with colloidal silica deposit

UIS5078720

SILICATES, LM Silicon wafer with colloidal silica deposit Silicon wafer with colloidal silica deposit

UIS5078720

Tourmaline (photo)
 
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Tourmaline (photo)

NHM1453594

Tourmaline (photo)

NHM1453594

The Formation of the Earth - Artist's View - Meteorite strike on infant Earth - The Earth was formed 4.6 billion years ago from a gigantic cloud of gas and dust. These dust accreted to form our planet; it was subjected to a large bombardment of meteorites. A molten, infant Earth is impacted by an object about 10 miles in diameter, releasing 200 million times a much energy as the largest manmade explosion. While this collision appears negligible when compared to the scars of much larger encounters, a similar impact four billion years later may have resulted in the extinction of the dinosaurs. The Earth accrued the majority of its mass during the 100 million years following the formation of the Sun, a period referred to as the cosmic bombardment. During this era of frequent impacts and radioactive heating, the entire Earth remained molten long enough for the heavy metals iron and nickel to settle to the center of the Earth while lighter silicates floated to the surface. Today, over four and a half billion years later, the Earth is still cooling. The silicates, forming a crust only a few tens of miles thick, still float on an “” ocean”” of molten metals and minerals, and the temperature at the center of the Earth may yet be hotter than the surface of the Sun
 
The Formation of the Earth - Artist's View - Meteorite strike on infant Earth - The Earth was formed 4.6 billion years ago from a gigantic cloud of gas and dust. These dust accreted to form our planet; it was subjected to a large bombardment of meteorites. A molten, infant Earth is impacted by an object about 10 miles in diameter, releasing 200 million times a much energy as the largest manmade explosion. While this collision appears negligible when compared to the scars of much larger encounters, a similar impact four billion years later may have resulted in the extinction of the dinosaurs. The Earth accrued the majority of its mass during the 100 million years following the formation of the Sun, a period referred to as the cosmic bombardment. During this era of frequent impacts and radioactive heating, the entire Earth remained molten long enough for the heavy metals iron and nickel to settle to the center of the Earth while lighter silicates floated to the surface. Today, over four

Walter B Myers

PIX4633457

The Formation of the Earth - Artist's View - Meteorite strike on infant Earth - The Earth was formed 4.6 billion years ago from a gigantic cloud of gas and dust. These dust accreted to form our planet; it was subjected to a large bombardment of meteorites. A molten, infant Earth is impacted by an object about 10 miles in diameter, releasing 200 million times a much energy as the largest manmade explosion. While this collision appears negligible when compared to the scars of much larger encounters, a similar impact four billion years later may have resulted in the extinction of the dinosaurs. The Earth accrued the majority of its mass during the 100 million years following the formation of the Sun, a period referred to as the cosmic bombardment. During this era of frequent impacts and radioactive heating, the entire Earth remained molten long enough for the heavy metals iron and nickel to settle to the center of the Earth while lighter silicates floated to the surface. Today, over four

Walter B Myers

PIX4633457

François Arago
 
François Arago

XLF3787674

François Arago

XLF3787674

Spiral galaxy M81 infrared view - Spiral galaxy M81 seen in infrared - View obtained by Spitzer space telescope in different wavelengths. In infrared, Spitzer sees dust rather than stars, thus improving our understanding of star formation. The M81 spiral galaxy is located 12 million light years away from Earth. Its arms are home to star-forming regions while its core is surrounded by much older yellow stars. Located in the northern constellation of Ursa Major (which also includes the Big Dipper), this galaxy is easily visible through binoculars or a small telescope. M81 is located at a distance of 12 million light - years. These infrared images were obtained by Spitzer's infrared array camera. At these wavelengths, Spitzer sees the dust, rather than the stars, within the disc of silicates and carbonaceous grains. It is well - mixed with gas, which is best seen at radio wavelengths, to form the essential ingredients for future star formation
 
Spiral galaxy M81 infrared view - Spiral galaxy M81 seen in infrared - View obtained by Spitzer space telescope in different wavelengths. In infrared, Spitzer sees dust rather than stars, thus improving our understanding of star formation. The M81 spiral galaxy is located 12 million light years away from Earth. Its arms are home to star-forming regions while its core is surrounded by much older yellow stars. Located in the northern constellation of Ursa Major (which also includes the Big Dipper), this galaxy is easily visible through binoculars or a small telescope. M81 is located at a distance of 12 million light - years. These infrared images were obtained by Spitzer's infrared array camera. At these wavelengths, Spitzer sees the dust, rather than the stars, within the disc of silicates and carbonaceous grains. It is well - mixed with gas, which is best seen at radio wavelengths, to form the essential ingredients for future star formation

PIX4610385

Spiral galaxy M81 infrared view - Spiral galaxy M81 seen in infrared - View obtained by Spitzer space telescope in different wavelengths. In infrared, Spitzer sees dust rather than stars, thus improving our understanding of star formation. The M81 spiral galaxy is located 12 million light years away from Earth. Its arms are home to star-forming regions while its core is surrounded by much older yellow stars. Located in the northern constellation of Ursa Major (which also includes the Big Dipper), this galaxy is easily visible through binoculars or a small telescope. M81 is located at a distance of 12 million light - years. These infrared images were obtained by Spitzer's infrared array camera. At these wavelengths, Spitzer sees the dust, rather than the stars, within the disc of silicates and carbonaceous grains. It is well - mixed with gas, which is best seen at radio wavelengths, to form the essential ingredients for future star formation

PIX4610385

Size comparison: Earth, Moon and Galilean satellites - Jupiter's four largest satellites and Earth and the Moon compared - Jupiter's four largest satellites, called Galilean satellites, compared to Earth and Moon. At the top, from left to right, in order of their distance to the planet Jupiter, we find Io, Europe, Ganymede and Callisto. Ganymede is the largest satellite in the solar system. Jupiter's four largest satellites, also known as the “” Galilean”” satellites since they were first observed by the Italian astronomer Galileo over 400 years ago, are worlds in their own right. Top row, left to right, in order from their distances from Jupiter, are: Io, Europa, Ganymede, Callisto Io is the most volcanic world in the Solar System, resurfacing itself continually with extremely hot and massive eruptions that spew material over 200 miles into space. Europa is about the same size as Earth's Moon, however unlike the Moon which is made up mostly of dry silicate materials, Europa is believed to be composed primarily of water ice, and may even contain a vast ocean of liquid salt water beneath its crust. For this reason, Europa is now emerging as one of the most viable candidates for hosting extraterrestrial life. Ganymede and Callisto are each larger than the planet Mercury, while Ganymede is the largest of all satellites in the Solar System. Io, Europa, and Ganymede are locked in a gravitational resonance where for every orbit Ganymede completes, Europa completes two orbits and Io completes four
 
Size comparison: Earth, Moon and Galilean satellites - Jupiter's four largest satellites and Earth and the Moon compared - Jupiter's four largest satellites, called Galilean satellites, compared to Earth and Moon. At the top, from left to right, in order of their distance to the planet Jupiter, we find Io, Europe, Ganymede and Callisto. Ganymede is the largest satellite in the solar system. Jupiter's four largest satellites, also known as the “” Galilean”” satellites since they were first observed by the Italian astronomer Galileo over 400 years ago, are worlds in their own right. Top row, left to right, in order from their distances from Jupiter, are: Io, Europa, Ganymede, Callisto Io is the most volcanic world in the Solar System, resurfacing itself continually with extremely hot and massive eruptions that spew material over 200 miles into space. Europa is about the same size as Earth's Moon, however unlike the Moon which is made up mostly of dry silicate materials, Europa is believe

Walter B Myers

PIX4629924

Size comparison: Earth, Moon and Galilean satellites - Jupiter's four largest satellites and Earth and the Moon compared - Jupiter's four largest satellites, called Galilean satellites, compared to Earth and Moon. At the top, from left to right, in order of their distance to the planet Jupiter, we find Io, Europe, Ganymede and Callisto. Ganymede is the largest satellite in the solar system. Jupiter's four largest satellites, also known as the “” Galilean”” satellites since they were first observed by the Italian astronomer Galileo over 400 years ago, are worlds in their own right. Top row, left to right, in order from their distances from Jupiter, are: Io, Europa, Ganymede, Callisto Io is the most volcanic world in the Solar System, resurfacing itself continually with extremely hot and massive eruptions that spew material over 200 miles into space. Europa is about the same size as Earth's Moon, however unlike the Moon which is made up mostly of dry silicate materials, Europa is believe

Walter B Myers

PIX4629924

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