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Images of 'Water Droplets' found, 107

 
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Water Droplets on Old Camera Lens. Nostalgic 1970s Video of Niagara Falls

FVP8973239

Water Droplets on Old Camera Lens. Nostalgic 1970s Video of Niagara Falls

FVP8973239

 
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  • Content within this clip may require additional clearances (eg: trademark, audio rights and/or property/personality releases) depending on Licensee’s specific use of material.
Niagara Falls Frontal View from Above with Water Droplets on Vintage Camera Lens

FVP8973242

Niagara Falls Frontal View from Above with Water Droplets on Vintage Camera Lens

FVP8973242

 
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Rogier van der Weyden

ARP480628

Rogier van der Weyden

ARP480628

 
Arc de fog - Fogbow - Arc de fog observed in Brittany on 5 May 2006. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on May 5, 2006. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refracted under ang

Laurent Laveder

PIX4671386

Arc de fog - Fogbow - Arc de fog observed in Brittany on 5 May 2006. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on May 5, 2006. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refracted under ang

Laurent Laveder

PIX4671386

 
Arc de fog - Fogbow - Arc de fog observed in Brittany on 5 May 2006. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on May 5, 2006. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refracted under ang

Laurent Laveder

PIX4671404

Arc de fog - Fogbow - Arc de fog observed in Brittany on 5 May 2006. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on May 5, 2006. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refracted under ang

Laurent Laveder

PIX4671404

 
Fog arc - Fogbow - Fog arc observed in La Palma, Canary Islands. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, diffraction in fog droplets is preponderant, which has the effect of refracting colors at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Fogbow in La Palma, Canary Islands

Alex Tudorica

PIX4671437

Fog arc - Fogbow - Fog arc observed in La Palma, Canary Islands. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, diffraction in fog droplets is preponderant, which has the effect of refracting colors at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Fogbow in La Palma, Canary Islands

Alex Tudorica

PIX4671437

 
Fog arc - Fogbow - Fog arc observed in La Palma, Canary Islands. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, diffraction in fog droplets is preponderant, which has the effect of refracting colors at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Fogbow in La Palma, Canary Islands

Alex Tudorica

PIX4671433

Fog arc - Fogbow - Fog arc observed in La Palma, Canary Islands. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, diffraction in fog droplets is preponderant, which has the effect of refracting colors at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Fogbow in La Palma, Canary Islands

Alex Tudorica

PIX4671433

 
Arc de fog - Fogbow - Arc de fog observed in Brittany on 5 May 2006. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on May 5, 2006. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refracted under ang

Laurent Laveder

PIX4671379

Arc de fog - Fogbow - Arc de fog observed in Brittany on 5 May 2006. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on May 5, 2006. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refracted under ang

Laurent Laveder

PIX4671379

 
Arc de fog - Fogbow - Arc de brume observed in Brittany on February 23, 2008. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on Feb 23, 2008. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refracted

Laurent Laveder

PIX4671410

Arc de fog - Fogbow - Arc de brume observed in Brittany on February 23, 2008. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on Feb 23, 2008. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refracted

Laurent Laveder

PIX4671410

 
Arc de fog - Fogbow - Arc de brume observed in Brittany on 16 December 2008. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on December 16, 2008. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refra

Laurent Laveder

PIX4671412

Arc de fog - Fogbow - Arc de brume observed in Brittany on 16 December 2008. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on December 16, 2008. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refra

Laurent Laveder

PIX4671412

 
Fog arc - Fogbow - Fog arc observed in La Palma, Canary Islands. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, diffraction in fog droplets is preponderant, which has the effect of refracting colors at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Fogbow in La Palma, Canary Islands

Alex Tudorica

PIX4671440

Fog arc - Fogbow - Fog arc observed in La Palma, Canary Islands. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, diffraction in fog droplets is preponderant, which has the effect of refracting colors at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Fogbow in La Palma, Canary Islands

Alex Tudorica

PIX4671440

 
Arc de fog - Fogbow - Arc de fog observed in Brittany on 5 May 2006. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on May 5, 2006. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refracted under ang

Laurent Laveder

PIX4671396

Arc de fog - Fogbow - Arc de fog observed in Brittany on 5 May 2006. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Thus, all colours blend and one sees a white arch of light, sometimes slightly bluish on the inside and red on the outside, wider than a rainbow. Fogbow seen in Brittany on May 5, 2006. A fogbow is forming like a rainbow. The sunlight reflects in the fog droplets, but thoses droplets are much more smaller than the raindrops: about hundredths millimeters for the fog instead of about one millimeter for the rain. Thus, the diffraction in the fog droplets is leading, then the colors are refracted under ang

Laurent Laveder

PIX4671396

 
Fog arc - Fogbow - Fog arc in formation observed at La Palma, Canary Islands. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, diffraction in fog droplets is preponderant, which has the effect of refracting colors at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Fogbow forming in ascending clouds in La Palma, Canary islands

Alex Tudorica

PIX4671426

Fog arc - Fogbow - Fog arc in formation observed at La Palma, Canary Islands. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, diffraction in fog droplets is preponderant, which has the effect of refracting colors at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Fogbow forming in ascending clouds in La Palma, Canary islands

Alex Tudorica

PIX4671426

 
Fog bow on the telescope Grantecan - Fogbow above Grantecan - Fog bow above the telescope Grantecan (Gran Telescopio Canarias) in La Palma, Canary Islands. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Fogbow above the telescope Grantecan (Gran Telescopio Canarias) in La Palma, Canary islands

Alex Tudorica

PIX4654492

Fog bow on the telescope Grantecan - Fogbow above Grantecan - Fog bow above the telescope Grantecan (Gran Telescopio Canarias) in La Palma, Canary Islands. A haze arc is formed in the way of a rainbow. The light of the Sun is reflected in the water drops of the mist, but unlike raindrops, the mist droplets are much smaller: about a millimetre for the rain versus a few centiemes for the mist. As a result, the diffraction in the mist droplets is preponderant, which results in colour refracting at random angles, between 30 and 45* around the anti-sun point (opposite the Sun). Fogbow above the telescope Grantecan (Gran Telescopio Canarias) in La Palma, Canary islands

Alex Tudorica

PIX4654492

 
Colored crown around the Moon and irizations - Corona around the Moon with irisation - Provoked by the microscopic drops of water that form these clouds, the crowns are colored blue as close to the Moon, then degrade from yellow to brick red. In the distance, on the edge of the cloud strip, another luminous phenomene is noticeable: these are colourful irisations such as those seen sometimes on some puddles. In meteorology, a lunar corona is produced by the diffraction of light from the Moon by small water droplets in a cloud

G. Cannat

PIX4671856

Colored crown around the Moon and irizations - Corona around the Moon with irisation - Provoked by the microscopic drops of water that form these clouds, the crowns are colored blue as close to the Moon, then degrade from yellow to brick red. In the distance, on the edge of the cloud strip, another luminous phenomene is noticeable: these are colourful irisations such as those seen sometimes on some puddles. In meteorology, a lunar corona is produced by the diffraction of light from the Moon by small water droplets in a cloud

G. Cannat

PIX4671856

 
Usage restrictions from our Content Partners
  • Not available to clients invoiced in the UK
Particle Imaging, Cloud Chamber Cloud chamber, 1947

UIS5065932

Particle Imaging, Cloud Chamber Cloud chamber, 1947

UIS5065932

 
Usage restrictions from our Content Partners
  • Not available to clients invoiced in the UK
Electrical Apparatus Armstrong's hydro-electric machine, 1845

UIS5061525

Electrical Apparatus Armstrong's hydro-electric machine, 1845

UIS5061525

 
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  • Not available to clients invoiced in the UK
Spectre of the Brocken, 1902

UIS5083545

Spectre of the Brocken, 1902

UIS5083545

 
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  • Permission required for non-editorial use (inc book and magazine covers). Please contact us
A large figure, most likely representing Hermes Trismegistus; at his head, a largely illegible scroll; he is embracing a large, stoppered flask (the arms of which bear writing and symbols), which contains a black frog, feathers and tadpoles or droplets of liquid at the top, and eight roundels connected to a central roundel by chains, representing stages in the alchemical process. Seven of the roundels depict figures conducting alchemical experiments involving a large flask containing homunculi atop a furnace; the eighth roundel contains a sun and and moon, corresponding silver and gold figures, and two figures dressed in red robes wielding tools. A large scroll, bearing an inscription: 'Terra stat unda lavat pyr purgat spiritus vivificat'; beneath, a further inscription: 'The mouth of the Collorick beware and thereof be wise'; two walls, enclosing a burst of flame. - a tree, its upper branches bearing inscriptions 'spiritus' and 'anima'; a naked, dragon-tailed woman is straddling its

BL3292659

A large figure, most likely representing Hermes Trismegistus; at his head, a largely illegible scroll; he is embracing a large, stoppered flask (the arms of which bear writing and symbols), which contains a black frog, feathers and tadpoles or droplets of liquid at the top, and eight roundels connected to a central roundel by chains, representing stages in the alchemical process. Seven of the roundels depict figures conducting alchemical experiments involving a large flask containing homunculi atop a furnace; the eighth roundel contains a sun and and moon, corresponding silver and gold figures, and two figures dressed in red robes wielding tools. A large scroll, bearing an inscription: 'Terra stat unda lavat pyr purgat spiritus vivificat'; beneath, a further inscription: 'The mouth of the Collorick beware and thereof be wise'; two walls, enclosing a burst of flame. - a tree, its upper branches bearing inscriptions 'spiritus' and 'anima'; a naked, dragon-tailed woman is straddling its

BL3292659

 
Earth's atmosphere and setting sun - Earth's atmosphere and setting sun - Earth's atmosphere seen at sunset from the International Space Station (ISS) on May 25, 2010. This spectacular image of sunset on the Indian Ocean was taken by astronauts aboard the International Space Station (ISS). The image presents an edge - on, or limb view, of the Earth's atmosphere as seen from orbit. The Earth's curvature is visible along the horizon line, or limb, that extends across the image from center left to lower right. Above the darkened surface of the Earth, a brilliant sequence of colors roughly denotes several layers of the atmosphere. Deep oranges and yellows appear in the troposphere, which extends from the Earth's surface to 6 - 20 km high. This layer contains over 80 percent of the mass of the atmosphere and almost all of the water vapor, clouds, and precipitation. Several dark cloud layers are visible within this layer. Variations in the colors are due mainly to varying concentrations of e

PIX4675392

Earth's atmosphere and setting sun - Earth's atmosphere and setting sun - Earth's atmosphere seen at sunset from the International Space Station (ISS) on May 25, 2010. This spectacular image of sunset on the Indian Ocean was taken by astronauts aboard the International Space Station (ISS). The image presents an edge - on, or limb view, of the Earth's atmosphere as seen from orbit. The Earth's curvature is visible along the horizon line, or limb, that extends across the image from center left to lower right. Above the darkened surface of the Earth, a brilliant sequence of colors roughly denotes several layers of the atmosphere. Deep oranges and yellows appear in the troposphere, which extends from the Earth's surface to 6 - 20 km high. This layer contains over 80 percent of the mass of the atmosphere and almost all of the water vapor, clouds, and precipitation. Several dark cloud layers are visible within this layer. Variations in the colors are due mainly to varying concentrations of e

PIX4675392

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