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Iridescent clouds - Iridescent clouds - When parts of a cloud are very thin and contain water droplets of the same size, the diffraction of the solar light that passes through them can cause colour comparable to those of crowns. We are talking about iridescent or iridescent clouds. Irization is caused by diffraction of sunlight by small droplets in high altitude clouds
Iridescent clouds - Iridescent clouds - When parts of a cloud are very thin and contain water droplets of the same size, the diffraction of the solar light that passes through them can cause colour comparable to those of crowns. We are talking about iridescent or iridescent clouds. Irization is caused by diffraction of sunlight by small droplets in high altitude clouds

PIX4671609: Iridescent clouds - Iridescent clouds - When parts of a cloud are very thin and contain water droplets of the same size, the diffraction of the solar light that passes through them can cause colour comparable to those of crowns. We are talking about iridescent or iridescent clouds. Irization is caused by diffraction of sunlight by small droplets in high altitude clouds / Bridgeman Images

ID: PIX4671609

Iridescent clouds - Iridescent clouds - When parts of a cloud are very thin and contain water droplets of the same size, the diffraction of the solar light that passes through them can cause colour comparable to those of crowns. We are talking about iridescent or iridescent clouds. Irization is caused by diffraction of sunlight by small droplets in high altitude clouds

Rainbow - Rainbow - Rainbow - Rainbow - Rainbow - fragmented sky appearing the Sun pierces through the clouds. 11 July 2008 Rainbow. July 11, 2008
Rainbow - Rainbow - Rainbow - Rainbow - Rainbow - fragmented sky appearing the Sun pierces through the clouds. 11 July 2008 Rainbow. July 11, 2008

PIX4671130: Rainbow - Rainbow - Rainbow - Rainbow - Rainbow - fragmented sky appearing the Sun pierces through the clouds. 11 July 2008 Rainbow. July 11, 2008 / Bridgeman Images

ID: PIX4671130

Rainbow - Rainbow - Rainbow - Rainbow - Rainbow - fragmented sky appearing the Sun pierces through the clouds. 11 July 2008 Rainbow. July 11, 2008

Rainbow at sunrise - Rainbow at sunrise - Arc - en - ciel observes 17 December 2005. At sunrise, the glowing light of the Sun caused an almost complete absence of blue and green colors in the rainbow. December 17, 2005. Rainbow seen at sunrise. Blue and green colors are almost invisible, because of this bright reddish sunshine
Rainbow at sunrise - Rainbow at sunrise - Arc - en - ciel observes 17 December 2005. At sunrise, the glowing light of the Sun caused an almost complete absence of blue and green colors in the rainbow. December 17, 2005. Rainbow seen at sunrise. Blue and green colors are almost invisible, because of this bright reddish sunshine

PIX4671149: Rainbow at sunrise - Rainbow at sunrise - Arc - en - ciel observes 17 December 2005. At sunrise, the glowing light of the Sun caused an almost complete absence of blue and green colors in the rainbow. December 17, 2005. Rainbow seen at sunrise. Blue and green colors are almost invisible, because of this bright reddish sunshine / Bridgeman Images

ID: PIX4671149

Rainbow at sunrise - Rainbow at sunrise - Arc - en - ciel observes 17 December 2005. At sunrise, the glowing light of the Sun caused an almost complete absence of blue and green colors in the rainbow. December 17, 2005. Rainbow seen at sunrise. Blue and green colors are almost invisible, because of this bright reddish sunshine

Rainbow - Rainbow - Rainbow - Arc - en - ciel tres colorore. 2 December 2008 Rainbow. December 2nd, 2008
Rainbow - Rainbow - Rainbow - Arc - en - ciel tres colorore. 2 December 2008 Rainbow. December 2nd, 2008

PIX4671168: Rainbow - Rainbow - Rainbow - Arc - en - ciel tres colorore. 2 December 2008 Rainbow. December 2nd, 2008 / Bridgeman Images

ID: PIX4671168

Rainbow - Rainbow - Rainbow - Arc - en - ciel tres colorore. 2 December 2008 Rainbow. December 2nd, 2008

Saint Louis Hospital in Paris 75010.
Saint Louis Hospital in Paris 75010.

TEC4671183: Saint Louis Hospital in Paris 75010. / Bridgeman Images

ID: TEC4671183

Saint Louis Hospital in Paris 75010.

Rainbow Rainbow Double Rainbow Double Rainbow
Rainbow Rainbow Double Rainbow Double Rainbow

PIX4671241: Rainbow Rainbow Double Rainbow Double Rainbow / Bridgeman Images

ID: PIX4671241

Rainbow Rainbow Double Rainbow Double Rainbow

Noctilucent clouds in Brittany - Noctilucent clouds in Brittany - Noctulescent clouds, very high altitude clouds, very rarely visible in France, photographs on 24 June 2009 in Ploumanac'h (Cotes d'Armor). These high altitude clouds are usually seen in summer months but nearer the poles than France. Ploumanac'h (Cotes d'Armor), Brittany, June 24 2009
Noctilucent clouds in Brittany - Noctilucent clouds in Brittany - Noctulescent clouds, very high altitude clouds, very rarely visible in France, photographs on 24 June 2009 in Ploumanac'h (Cotes d'Armor). These high altitude clouds are usually seen in summer months but nearer the poles than France. Ploumanac'h (Cotes d'Armor), Brittany, June 24 2009

PIX4671655: Noctilucent clouds in Brittany - Noctilucent clouds in Brittany - Noctulescent clouds, very high altitude clouds, very rarely visible in France, photographs on 24 June 2009 in Ploumanac'h (Cotes d'Armor). These high altitude clouds are usually seen in summer months but nearer the poles than France. Ploumanac'h (Cotes d'Armor), Brittany, June 24 2009 / Bridgeman Images

ID: PIX4671655

Noctilucent clouds in Brittany - Noctilucent clouds in Brittany - Noctulescent clouds, very high altitude clouds, very rarely visible in France, photographs on 24 June 2009 in Ploumanac'h (Cotes d'Armor). These high altitude clouds are usually seen in summer months but nearer the poles than France. Ploumanac'h (Cotes d'Armor), Brittany, June 24 2009

Lunar crown - Lunar corona - A lunar crown is due to the diffraction of the light of the Moon by drops of water in medium-altitude clouds. Lunar corona is caused by the diffraction of the moonlight by water droplets
Lunar crown - Lunar corona - A lunar crown is due to the diffraction of the light of the Moon by drops of water in medium-altitude clouds. Lunar corona is caused by the diffraction of the moonlight by water droplets

PIX4671739: Lunar crown - Lunar corona - A lunar crown is due to the diffraction of the light of the Moon by drops of water in medium-altitude clouds. Lunar corona is caused by the diffraction of the moonlight by water droplets / Bridgeman Images

ID: PIX4671739

Lunar crown - Lunar corona - A lunar crown is due to the diffraction of the light of the Moon by drops of water in medium-altitude clouds. Lunar corona is caused by the diffraction of the moonlight by water droplets

Clouds Altostratus undulatus - Altostratus undulatus clouds - Medium clouds, between 2000m and 5000 m. These undulated clouds are low altostratus
Clouds Altostratus undulatus - Altostratus undulatus clouds - Medium clouds, between 2000m and 5000 m. These undulated clouds are low altostratus

PIX4671804: Clouds Altostratus undulatus - Altostratus undulatus clouds - Medium clouds, between 2000m and 5000 m. These undulated clouds are low altostratus / Bridgeman Images

ID: PIX4671804

Clouds Altostratus undulatus - Altostratus undulatus clouds - Medium clouds, between 2000m and 5000 m. These undulated clouds are low altostratus

Halo around the Sun - Halo around the Sun - Halos are due to the light of the Sun reflected by high-altitude clouds, Cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. In this photo, a parhely is also visible. (c) 2006 Jerry Lodriguss/www.astropix.co
Halo around the Sun - Halo around the Sun - Halos are due to the light of the Sun reflected by high-altitude clouds, Cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. In this photo, a parhely is also visible. (c) 2006 Jerry Lodriguss/www.astropix.co

PIX4670884: Halo around the Sun - Halo around the Sun - Halos are due to the light of the Sun reflected by high-altitude clouds, Cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. In this photo, a parhely is also visible. (c) 2006 Jerry Lodriguss/www.astropix.co / Bridgeman Images

ID: PIX4670884

Halo around the Sun - Halo around the Sun - Halos are due to the light of the Sun reflected by high-altitude clouds, Cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. In this photo, a parhely is also visible. (c) 2006 Jerry Lodriguss/www.astropix.co

Halo around the Sun and condensation train - Sun Halo and contrail. - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and thus cause a perfect circle around the Sun. 14 May 2006, Finistere. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. May 14, 2006
Halo around the Sun and condensation train - Sun Halo and contrail. - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and thus cause a perfect circle around the Sun. 14 May 2006, Finistere. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. May 14, 2006

PIX4670961: Halo around the Sun and condensation train - Sun Halo and contrail. - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and thus cause a perfect circle around the Sun. 14 May 2006, Finistere. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. May 14, 2006 / Bridgeman Images

ID: PIX4670961

Halo around the Sun and condensation train - Sun Halo and contrail. - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and thus cause a perfect circle around the Sun. 14 May 2006, Finistere. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. May 14, 2006

Storm under the stars - Lightning under the stars - A thunderstorm eclate at the tombee of the night
Storm under the stars - Lightning under the stars - A thunderstorm eclate at the tombee of the night

PIX4670850: Storm under the stars - Lightning under the stars - A thunderstorm eclate at the tombee of the night / Bridgeman Images

ID: PIX4670850

Storm under the stars - Lightning under the stars - A thunderstorm eclate at the tombee of the night

Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele”” to the halo of 22* radius, the arc of Parry. - near the zenith, the arc cirucmzenithal, very colourful. Quimper Halos are caused by sunlight being refracted by cirro-stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. In brief: - around the Sun, the 22* halo, not very contrasted. - atop the 22* halo, the upper tangent arc (a splayed U shape). - above it, “” parallel”” to the 22* halo, the Parry arc. - near the zenith, the cirucmzenithal arc, very colorful. October 28, 2006 Quimper (France)
Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele”” to the halo of 22* radius, the arc of Parry. - near the zenith, the arc cirucmzenithal, very colourful. Quimper Halos are caused by sunlight being refracted by cirro-stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. In brief: - around the Sun, the 22* halo, not very contrasted. - atop the 22* halo, the upper tangent arc (a splayed U shape). - above it, “” parallel”” to the 22* halo, the Parry arc. - near the zenith, the cirucmzenithal arc, very colorful. October 28, 2006 Quimper (France)

PIX4670923: Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele”” to the halo of 22* radius, the arc of Parry. - near the zenith, the arc cirucmzenithal, very colourful. Quimper Halos are caused by sunlight being refracted by cirro-stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. In brief: - around the Sun, the 22* halo, not very contrasted. - atop the 22* halo, the upper tangent arc (a splayed U shape). - above it, “” parallel”” to the 22* halo, the Parry arc. - near the zenith, the cirucmzenithal arc, very colorful. October 28, 2006 Quimper (France) / Bridgeman Images

ID: PIX4670923

Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. Here we can see: - around the Sun, the halo of 22* radius, rather little contrast. - at the top of the halo of 22* radius, the upper arc tangent in the shape of a U evase. - above, “” parallele”” to the halo of 22* radius, the arc of Parry. - near the zenith, the arc cirucmzenithal, very colourful. Quimper Halos are caused by sunlight being refracted by cirro-stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. In brief: - around the Sun, the 22* halo, not very contrasted. - atop the 22* halo, the upper tangent arc (a splayed U shape). - above it, “” parallel”” to the 22* halo, the Parry arc. - near the zenith, the cirucmzenitha

Noctulescent clouds - Noctilucent clouds - Noctilucent clouds, very high altitude clouds, photographs in July 2009 in Russia. These rare clouds are called noctilucent or “” night shining” as they seem to glow in the dark. They are caused by ice crystals at about 80 km altitude. These crystals reflect sunlight when the sun is well below the horizon. They are properly known as polar mesospheric clouds and are under intense study as it remains a mystery as to how they are formed. Image taken in july 2009 in Russia
Noctulescent clouds - Noctilucent clouds - Noctilucent clouds, very high altitude clouds, photographs in July 2009 in Russia. These rare clouds are called noctilucent or “” night shining” as they seem to glow in the dark. They are caused by ice crystals at about 80 km altitude. These crystals reflect sunlight when the sun is well below the horizon. They are properly known as polar mesospheric clouds and are under intense study as it remains a mystery as to how they are formed. Image taken in july 2009 in Russia

PIX4671634: Noctulescent clouds - Noctilucent clouds - Noctilucent clouds, very high altitude clouds, photographs in July 2009 in Russia. These rare clouds are called noctilucent or “” night shining” as they seem to glow in the dark. They are caused by ice crystals at about 80 km altitude. These crystals reflect sunlight when the sun is well below the horizon. They are properly known as polar mesospheric clouds and are under intense study as it remains a mystery as to how they are formed. Image taken in july 2009 in Russia / Bridgeman Images

ID: PIX4671634

Noctulescent clouds - Noctilucent clouds - Noctilucent clouds, very high altitude clouds, photographs in July 2009 in Russia. These rare clouds are called noctilucent or “” night shining” as they seem to glow in the dark. They are caused by ice crystals at about 80 km altitude. These crystals reflect sunlight when the sun is well below the horizon. They are properly known as polar mesospheric clouds and are under intense study as it remains a mystery as to how they are formed. Image taken in july 2009 in Russia

Pollen crown - Pollen corona - Irisee crown around the Sun due to the presence of pollen in the atmosphere. Corona around the Sun created by the diffraction of light by pollen grains in the atmosphere
Pollen crown - Pollen corona - Irisee crown around the Sun due to the presence of pollen in the atmosphere. Corona around the Sun created by the diffraction of light by pollen grains in the atmosphere

PIX4671650: Pollen crown - Pollen corona - Irisee crown around the Sun due to the presence of pollen in the atmosphere. Corona around the Sun created by the diffraction of light by pollen grains in the atmosphere / Bridgeman Images

ID: PIX4671650

Pollen crown - Pollen corona - Irisee crown around the Sun due to the presence of pollen in the atmosphere. Corona around the Sun created by the diffraction of light by pollen grains in the atmosphere

Halo around the Moon - Lunar Halo - This halo is due to the light of the Moon reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Moon. This 22-degree lunar halo is quite contrasting and colourful, although the Moon is not Full (three days after the Full Moon). October 2, 2004. Lunar halos are caused by moonlight being refracted by cirro - stratus clouds. These thin clouds are located very high in the atmosphere, and are composed of ice crystals. This 22 degrees lunar halo is rather contrasted, although the Moon was not Full (three days after the full moon). 2 October 2004
Halo around the Moon - Lunar Halo - This halo is due to the light of the Moon reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Moon. This 22-degree lunar halo is quite contrasting and colourful, although the Moon is not Full (three days after the Full Moon). October 2, 2004. Lunar halos are caused by moonlight being refracted by cirro - stratus clouds. These thin clouds are located very high in the atmosphere, and are composed of ice crystals. This 22 degrees lunar halo is rather contrasted, although the Moon was not Full (three days after the full moon). 2 October 2004

PIX4671692: Halo around the Moon - Lunar Halo - This halo is due to the light of the Moon reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Moon. This 22-degree lunar halo is quite contrasting and colourful, although the Moon is not Full (three days after the Full Moon). October 2, 2004. Lunar halos are caused by moonlight being refracted by cirro - stratus clouds. These thin clouds are located very high in the atmosphere, and are composed of ice crystals. This 22 degrees lunar halo is rather contrasted, although the Moon was not Full (three days after the full moon). 2 October 2004 / Bridgeman Images

ID: PIX4671692

Halo around the Moon - Lunar Halo - This halo is due to the light of the Moon reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Moon. This 22-degree lunar halo is quite contrasting and colourful, although the Moon is not Full (three days after the Full Moon). October 2, 2004. Lunar halos are caused by moonlight being refracted by cirro - stratus clouds. These thin clouds are located very high in the atmosphere, and are composed of ice crystals. This 22 degrees lunar halo is rather contrasted, although the Moon was not Full (three days after the full moon). 2 October 2004

Storm on Los Angeles - Storm on Los Angele
Storm on Los Angeles - Storm on Los Angele

PIX4670836: Storm on Los Angeles - Storm on Los Angele / Bridgeman Images

ID: PIX4670836

Storm on Los Angeles - Storm on Los Angele

Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. February 2010. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. February 2010
Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. February 2010. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. February 2010

PIX4671043: Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. February 2010. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. February 2010 / Bridgeman Images

ID: PIX4671043

Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. February 2010. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter. February 2010

Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter
Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter

PIX4671060: Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter / Bridgeman Images

ID: PIX4671060

Halo around the Sun - Sun Halo - Halos are due to the light of the Sun reflected by high-altitude clouds, cirrostratus, composed of ice crystals. They bend the light and cause a perfect circle around the Sun. Halos are caused by sunlight being refracted by cirro - stratus clouds. These are thin clouds, very high in the atmosphere, and are composed of ice crystals. They bend light at a 22 degree angle, which creates a halo around the sun that is 44 degrees in diameter

Mirage inferior - Inferior mirage - Mirage inferior caused by the difference in temperature of the sea warmer than that of the air. 1 November 2006, Beg Meil (Finistere). Inferior mirage caused by the differences of temperature between sea and air. November 1 2006, Beg Meil (Finistere - France
Mirage inferior - Inferior mirage - Mirage inferior caused by the difference in temperature of the sea warmer than that of the air. 1 November 2006, Beg Meil (Finistere). Inferior mirage caused by the differences of temperature between sea and air. November 1 2006, Beg Meil (Finistere - France

PIX4672030: Mirage inferior - Inferior mirage - Mirage inferior caused by the difference in temperature of the sea warmer than that of the air. 1 November 2006, Beg Meil (Finistere). Inferior mirage caused by the differences of temperature between sea and air. November 1 2006, Beg Meil (Finistere - France / Bridgeman Images

ID: PIX4672030

Mirage inferior - Inferior mirage - Mirage inferior caused by the difference in temperature of the sea warmer than that of the air. 1 November 2006, Beg Meil (Finistere). Inferior mirage caused by the differences of temperature between sea and air. November 1 2006, Beg Meil (Finistere - France

Mirage inferior - Inferior mirage - Mirage inferior caused by the difference in temperature of the sea warmer than that of the air. 1 November 2006, Beg Meil (Finistere). Inferior mirage caused by the differences of temperature between sea and air. November 1 2006, Beg Meil (Finistere - France
Mirage inferior - Inferior mirage - Mirage inferior caused by the difference in temperature of the sea warmer than that of the air. 1 November 2006, Beg Meil (Finistere). Inferior mirage caused by the differences of temperature between sea and air. November 1 2006, Beg Meil (Finistere - France

PIX4672040: Mirage inferior - Inferior mirage - Mirage inferior caused by the difference in temperature of the sea warmer than that of the air. 1 November 2006, Beg Meil (Finistere). Inferior mirage caused by the differences of temperature between sea and air. November 1 2006, Beg Meil (Finistere - France / Bridgeman Images

ID: PIX4672040

Mirage inferior - Inferior mirage - Mirage inferior caused by the difference in temperature of the sea warmer than that of the air. 1 November 2006, Beg Meil (Finistere). Inferior mirage caused by the differences of temperature between sea and air. November 1 2006, Beg Meil (Finistere - France

Mirage - Mirage 'mountains' over tidal flat
Mirage - Mirage 'mountains' over tidal flat

PIX4672042: Mirage - Mirage 'mountains' over tidal flat / Bridgeman Images

ID: PIX4672042

Mirage - Mirage 'mountains' over tidal flat

Lower Mirage - Inferior mirage - Lower Mirage which gives the illusion that the rocks (on the left and at the entrance of the port) float above the horizon, not far from the Eckmuehl lighthouse (Penmarc'h, South Finistere). Inferior mirage (at left) near lighthouse in Penmarc'h, Brittany, France. Inferior mirages are caused by the differences of temperature between sea and air
Lower Mirage - Inferior mirage - Lower Mirage which gives the illusion that the rocks (on the left and at the entrance of the port) float above the horizon, not far from the Eckmuehl lighthouse (Penmarc'h, South Finistere). Inferior mirage (at left) near lighthouse in Penmarc'h, Brittany, France. Inferior mirages are caused by the differences of temperature between sea and air

PIX4672071: Lower Mirage - Inferior mirage - Lower Mirage which gives the illusion that the rocks (on the left and at the entrance of the port) float above the horizon, not far from the Eckmuehl lighthouse (Penmarc'h, South Finistere). Inferior mirage (at left) near lighthouse in Penmarc'h, Brittany, France. Inferior mirages are caused by the differences of temperature between sea and air / Bridgeman Images

ID: PIX4672071

Lower Mirage - Inferior mirage - Lower Mirage which gives the illusion that the rocks (on the left and at the entrance of the port) float above the horizon, not far from the Eckmuehl lighthouse (Penmarc'h, South Finistere). Inferior mirage (at left) near lighthouse in Penmarc'h, Brittany, France. Inferior mirages are caused by the differences of temperature between sea and air

Les sculptures habitacles d'Andre Bloc (1896-1966) à Meudon (Hauts de Seine). Plastic intervention 1964-1966. Photography 10/06/95.
Les sculptures habitacles d'Andre Bloc (1896-1966) à Meudon (Hauts de Seine). Plastic intervention 1964-1966. Photography 10/06/95.

TEC4672100: Les sculptures habitacles d'Andre Bloc (1896-1966) à Meudon (Hauts de Seine). Plastic intervention 1964-1966. Photography 10/06/95. / Bridgeman Images

ID: TEC4672100

Les sculptures habitacles d'Andre Bloc (1896-1966) à Meudon (Hauts de Seine). Plastic intervention 1964-1966. Photography 10/06/95.

Les sculptures habitacles d'Andre Bloc (1896-1966) à Meudon (Hauts de Seine). Plastic intervention 1964-1966. Photography 10/06/95.
Les sculptures habitacles d'Andre Bloc (1896-1966) à Meudon (Hauts de Seine). Plastic intervention 1964-1966. Photography 10/06/95.

TEC4672111: Les sculptures habitacles d'Andre Bloc (1896-1966) à Meudon (Hauts de Seine). Plastic intervention 1964-1966. Photography 10/06/95. / Bridgeman Images

ID: TEC4672111

Les sculptures habitacles d'Andre Bloc (1896-1966) à Meudon (Hauts de Seine). Plastic intervention 1964-1966. Photography 10/06/95.

Crepuscular rays - Crepuscular rays - Crepuscular rays seen on November 6, 2006. Crepuscular rays. November 6 2006
Crepuscular rays - Crepuscular rays - Crepuscular rays seen on November 6, 2006. Crepuscular rays. November 6 2006

PIX4672131: Crepuscular rays - Crepuscular rays - Crepuscular rays seen on November 6, 2006. Crepuscular rays. November 6 2006 / Bridgeman Images

ID: PIX4672131

Crepuscular rays - Crepuscular rays - Crepuscular rays seen on November 6, 2006. Crepuscular rays. November 6 2006

Crepuscular rays - Crepuscular rays - Crepuscular rays seen on November 6, 2006. Crepuscular rays. November 6 2006
Crepuscular rays - Crepuscular rays - Crepuscular rays seen on November 6, 2006. Crepuscular rays. November 6 2006

PIX4672153: Crepuscular rays - Crepuscular rays - Crepuscular rays seen on November 6, 2006. Crepuscular rays. November 6 2006 / Bridgeman Images

ID: PIX4672153

Crepuscular rays - Crepuscular rays - Crepuscular rays seen on November 6, 2006. Crepuscular rays. November 6 2006

Dawn - Dawn - Micocoulier at sunrise. 30 December 2004. Celtis seen at dawn. December 30 2004
Dawn - Dawn - Micocoulier at sunrise. 30 December 2004. Celtis seen at dawn. December 30 2004

PIX4672224: Dawn - Dawn - Micocoulier at sunrise. 30 December 2004. Celtis seen at dawn. December 30 2004 / Bridgeman Images

ID: PIX4672224

Dawn - Dawn - Micocoulier at sunrise. 30 December 2004. Celtis seen at dawn. December 30 2004

Trainee left by a missile - Trainee left by a missile - Cloud left by a missile Photo obtained in Arizona about 500 km from White Sands launch base
Trainee left by a missile - Trainee left by a missile - Cloud left by a missile Photo obtained in Arizona about 500 km from White Sands launch base

PIX4672291: Trainee left by a missile - Trainee left by a missile - Cloud left by a missile Photo obtained in Arizona about 500 km from White Sands launch base / Bridgeman Images

ID: PIX4672291

Trainee left by a missile - Trainee left by a missile - Cloud left by a missile Photo obtained in Arizona about 500 km from White Sands launch base

The Moon, Venus and a train left by a rocket - The Moon, Venus and a train left by a rocket - Cloud left by a missile or rocket over the Moon and Venus
The Moon, Venus and a train left by a rocket - The Moon, Venus and a train left by a rocket - Cloud left by a missile or rocket over the Moon and Venus

PIX4672293: The Moon, Venus and a train left by a rocket - The Moon, Venus and a train left by a rocket - Cloud left by a missile or rocket over the Moon and Venus / Bridgeman Images

ID: PIX4672293

The Moon, Venus and a train left by a rocket - The Moon, Venus and a train left by a rocket - Cloud left by a missile or rocket over the Moon and Venus

Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France

PIX4672327: Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France / Bridgeman Images

ID: PIX4672327

Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France

Grand Canyon, Arizona - Hiker on South Kaibab Trail in Grand Canyon - A tourist admires the Grand Canyon from Skeleton Point on the South Kaibab Trail. Skeleton Point on South Kaibab Trail in Grand Canyon National Park
Grand Canyon, Arizona - Hiker on South Kaibab Trail in Grand Canyon - A tourist admires the Grand Canyon from Skeleton Point on the South Kaibab Trail. Skeleton Point on South Kaibab Trail in Grand Canyon National Park

PIX4672749: Grand Canyon, Arizona - Hiker on South Kaibab Trail in Grand Canyon - A tourist admires the Grand Canyon from Skeleton Point on the South Kaibab Trail. Skeleton Point on South Kaibab Trail in Grand Canyon National Park / Bridgeman Images

ID: PIX4672749

Grand Canyon, Arizona - Hiker on South Kaibab Trail in Grand Canyon - A tourist admires the Grand Canyon from Skeleton Point on the South Kaibab Trail. Skeleton Point on South Kaibab Trail in Grand Canyon National Park

Grand Canyon, Arizona - South Kaibab Trail in Grand Canyon - Mules on the South Kaibab Trail. Mules going up South Kaibab Trail in Grand Canyon National Park
Grand Canyon, Arizona - South Kaibab Trail in Grand Canyon - Mules on the South Kaibab Trail. Mules going up South Kaibab Trail in Grand Canyon National Park

PIX4672752: Grand Canyon, Arizona - South Kaibab Trail in Grand Canyon - Mules on the South Kaibab Trail. Mules going up South Kaibab Trail in Grand Canyon National Park / Bridgeman Images

ID: PIX4672752

Grand Canyon, Arizona - South Kaibab Trail in Grand Canyon - Mules on the South Kaibab Trail. Mules going up South Kaibab Trail in Grand Canyon National Park

3 April 2016 - Canopee - Les Halles, Paris, Architects: Patrick Berger and Jacques Anziutti
3 April 2016 - Canopee - Les Halles, Paris, Architects: Patrick Berger and Jacques Anziutti

OMG4672763: 3 April 2016 - Canopee - Les Halles, Paris, Architects: Patrick Berger and Jacques Anziutti / Bridgeman Images

ID: OMG4672763

3 April 2016 - Canopee - Les Halles, Paris, Architects: Patrick Berger and Jacques Anziutti

Bahamas by Space Shuttle - 10 - 1992 - The Grand Bank of the Bahamas with Andros Island in the foreground. Image obtained from Shuttle Columbia on October 26, 1992. Mission STS-5
Bahamas by Space Shuttle - 10 - 1992 - The Grand Bank of the Bahamas with Andros Island in the foreground. Image obtained from Shuttle Columbia on October 26, 1992. Mission STS-5

PIX4672802: Bahamas by Space Shuttle - 10 - 1992 - The Grand Bank of the Bahamas with Andros Island in the foreground. Image obtained from Shuttle Columbia on October 26, 1992. Mission STS-5 / Bridgeman Images

ID: PIX4672802

Bahamas by Space Shuttle - 10 - 1992 - The Grand Bank of the Bahamas with Andros Island in the foreground. Image obtained from Shuttle Columbia on October 26, 1992. Mission STS-5

Southern California seen by Gemini 5 - 1965 - Imperial Valley and Salton Sea, Southern California, observed by Gemini - 5 on 21/08/1965
Southern California seen by Gemini 5 - 1965 - Imperial Valley and Salton Sea, Southern California, observed by Gemini - 5 on 21/08/1965

PIX4672824: Southern California seen by Gemini 5 - 1965 - Imperial Valley and Salton Sea, Southern California, observed by Gemini - 5 on 21/08/1965 / Bridgeman Images

ID: PIX4672824

Southern California seen by Gemini 5 - 1965 - Imperial Valley and Salton Sea, Southern California, observed by Gemini - 5 on 21/08/1965


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