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Kayaking-Madagascar-reptiles1.tif
Kayaking-Madagascar-reptiles7.jpg
Kayaking-Madagascar-reptiles3.jpg
Kayaking-Madagascar-reptiles4.jpg
Kayaking-Madagascar-reptiles6.jpg
Kayaking-Madagascar-reptiles5.jpg
Kayaking-Madagascar-reptiles2.tif
Palawan-invertebrates22.tif
Kayak-Madagascar-invertebrateNew-Mad...jpg
kayaking-Madagascar-frogs40.jpg
kayaking-Madagascar-frogs41.jpg
MtKinabalo-13.tif
Palawan-invertebrates6.tif
Palawan-invertebrates9.tif
Mt.Kinabalo-moth.jpg
marine-life-Puerto-Princesa39.jpg
marine-life-Puerto-Princesa41.jpg
Puerto-Princesa-festivals6.tif
kayaking-Madagascar-frogs73.tif
kayaking-Madagascar-frogs21.jpg
marine-life-Puerto-Princesa38.jpg
marine-life-Puerto-Princesa42.jpg
Mt.Kinabalo-stick-insect.jpg
MtKinabalo-2.tif
Puerto-Princesa-festivals5.tif
Puerto-Princesa-festivals4.tif
Puerto-Princesa-festivals3.tif
Kayaking-Bacuit-Archipelago15.tif
Kayaking- Gulf-of-California50.jpg
marine-life-Puerto-Princesa40.jpg
Borneo-Gunung-Mulu-frog1.tif
Puerto-Princesa-festivals1.tif
Puerto-Princesa-festivals2.tif
Alaska-vegetation25.jpg
Kayaking-Madagascar-reptiles35.jpg
Alaska-vegetation3.jpg
Alaska-vegetation23.jpg
Kayaking- Gulf-of-California52.jpg
Kayaking-Madagascar-reptiles36.jpg
Kayaking-Madagascar-reptiles39.jpg
Kayaking-Madagascar-reptiles37.jpg
Southeast-Alaska-huckleberry1.jpg
Alaska-camping-kayaking8.jpg
Alaska-vegetation8.jpg
Alaska-vegetation24.jpg
Alaska-vegetation12.jpg
Alaska-wildlife-bearAlaska-wildlifeA...jpg
Kayaking-West-Coast-Scotland14.jpg
Kayaking-Madagascar-journey47.jpg
vegetation-12.tif
Kayaking-Madagascar-reptiles38.jpg
Alaska-vegetation10-2.jpg
Alaska-vegetation11-2.jpg
Alaska-vegetation32.jpg
$Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.$

Southeast-Alaska-glaciation12.jpg
$Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.$

Southeast-Alaska-glaciation18.jpg
$Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.$

Southeast-Alaska-glaciation15.jpg
$Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.$

Southeast-Alaska-glaciation19.jpg
$Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.$

Southeast-Alaska-glaciation17.jpg
$Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.$

Southeast-Alaska-glaciation16.jpg
$Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.$

Southeast-Alaska-glaciation13.jpg
$Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.$

Southeast-Alaska-glaciation14.jpg