ISS018-E-15908
NASA Photo ID | ISS018-E-15908 |
Focal Length | 180mm |
Date taken | 2008.12.29 |
Time taken | 07:41:49 GMT |
Resolutions offered for this image:
1000 x 656 pixels 540 x 354 pixels 720 x 480 pixels 3072 x 2098 pixels 640 x 437 pixels
1000 x 656 pixels 540 x 354 pixels 720 x 480 pixels 3072 x 2098 pixels 640 x 437 pixels
Cloud masks available for this image:
Country or Geographic Name: | CROATIA |
Features: | SVETI JURE, BIOKOVO RA., COAST |
Features Found Using Machine Learning: | |
Cloud Cover Percentage: | 10 (1-10)% |
Sun Elevation Angle: | 8° |
Sun Azimuth: | 134° |
Camera: | Nikon D2Xs Electronic Still Camera |
Focal Length: | 180mm |
Camera Tilt: | 46 degrees |
Format: | 4288E: 4288 x 2848 pixel CMOS sensor, RGBG imager color filter |
Film Exposure: | |
Additional Information | |
Width | Height | Annotated | Cropped | Purpose | Links |
---|---|---|---|---|---|
1000 pixels | 656 pixels | No | Yes | Earth From Space collection | Download Image |
540 pixels | 354 pixels | Yes | Yes | Earth From Space collection | Download Image |
720 pixels | 480 pixels | Yes | Yes | NASA's Earth Observatory web site | Download Image |
3072 pixels | 2098 pixels | No | No | Download Image | |
640 pixels | 437 pixels | No | No | Download Image |
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Image Caption: Biokovo Range, Croatia
The Biokovo Range in Croatia is part of the Dinaric Alps that extend northwest-southeast along the coastline of the Adriatic Sea. The range itself is the location of a national park; the nearby city of Makarska, located between the mountains and the sea, is a popular tourist destination. The highest peak in the range is Sveti Jure (1,762 meters above sea level). The Biokovo Range is comprised mainly of Mesozoic-age carbonate rocks, primarily limestone, that were deposited in relatively warm, shallow waters. Later tectonic processes uplifted and exposed the carbonate rocks to erosion, leading to a distinctive geological surface known as karst topography.
Karst topography occurs when naturally occurring acids in surface and ground water dissolve the carbonate rocks. As the rock dissolves, underground networks of drainages and caves form. As more empty space develops underground, the overlaying rock and soil collapse to form a variety of landforms including sinkholes, blind valleys, and towers. In the Biokovo Range, much of the karst surface has a pitted appearance, easily visible in the early morning light in this astronaut photograph. The pitted appearance is produced by numerous circular or semi-circular collapse valleys known locally as vrtace. While this image captures Sveti Jure covered with snow, there are no glaciers or ice fields in the Biokovo Range.
The Biokovo Range in Croatia is part of the Dinaric Alps that extend northwest-southeast along the coastline of the Adriatic Sea. The range itself is the location of a national park; the nearby city of Makarska, located between the mountains and the sea, is a popular tourist destination. The highest peak in the range is Sveti Jure (1,762 meters above sea level). The Biokovo Range is comprised mainly of Mesozoic-age carbonate rocks, primarily limestone, that were deposited in relatively warm, shallow waters. Later tectonic processes uplifted and exposed the carbonate rocks to erosion, leading to a distinctive geological surface known as karst topography.
Karst topography occurs when naturally occurring acids in surface and ground water dissolve the carbonate rocks. As the rock dissolves, underground networks of drainages and caves form. As more empty space develops underground, the overlaying rock and soil collapse to form a variety of landforms including sinkholes, blind valleys, and towers. In the Biokovo Range, much of the karst surface has a pitted appearance, easily visible in the early morning light in this astronaut photograph. The pitted appearance is produced by numerous circular or semi-circular collapse valleys known locally as vrtace. While this image captures Sveti Jure covered with snow, there are no glaciers or ice fields in the Biokovo Range.