STS41B-42-2483
NASA Photo ID | STS41B-42-2483 |
Focal Length | 250mm |
Date taken | 1984.02.__ |
Time taken | GMT |
Resolutions offered for this image:
5321 x 5321 pixels 639 x 639 pixels 5700 x 5900 pixels 483 x 500 pixels 640 x 480 pixels
5321 x 5321 pixels 639 x 639 pixels 5700 x 5900 pixels 483 x 500 pixels 640 x 480 pixels
Cloud masks available for this image:
Country or Geographic Name: | PARAGUAY |
Features: | RIO PARANA |
Features Found Using Machine Learning: | |
Cloud Cover Percentage: | 0 (no clouds present) |
Sun Elevation Angle: | ° |
Sun Azimuth: | ° |
Camera: | Hasselblad |
Focal Length: | 250mm |
Camera Tilt: | Near Vertical |
Format: | 6017: Kodak Ektachrome 64, 220 Roll Format |
Film Exposure: | Normal |
Additional Information | |
Width | Height | Annotated | Cropped | Purpose | Links |
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5321 pixels | 5321 pixels | No | No | Earth From Space collection | Download Image |
639 pixels | 639 pixels | No | No | Earth From Space collection | Download Image |
5700 pixels | 5900 pixels | No | No | Download Image | |
483 pixels | 500 pixels | No | No | Download Image | |
640 pixels | 480 pixels | No | No | Download Image |
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Image Caption: STS41B-42-2483 Parana River, Argentina and Paraguay February 1984
The effects of the rainy season in south-central South America are vividly documented in this near-vertical photograph of the confluence of the Parana and Paraguay Rivers northeast of the Argentine town of Corrientes. The Parana River flows westward; after merging with the Paraguay River, it begins to flow almost due south. Both rivers are sediment laden and appear to be out of their normal watercourses, thereby producing flooding conditions. The Paraguay River is characterized by the widely varying, meandering main channel; many oxbow lakes; and a tan sediment load. The Parana River has a smaller floodplain, a deeper channel, and a reddish-brown sediment load. As the two rivers merge and begin to flow southwestward, their individual sediment patterns do not mix readily, a common occurrence in which rivers with different densities of suspended particles tend to retain their individual color characteristics for many miles downstream. The Parana River, which flows approximately 2000 miles (3200 kilometers), is the second largest drainage system in South America; the Amazon River is the largest. An old river channel south of the Parana River parallels the present river channel. This much older stream channel seems to flow toward the city of Corrientes (estimated population of 200 000), the commercial center for this rich agricultural region of northeast Argentina and southwest Paraguay.
The effects of the rainy season in south-central South America are vividly documented in this near-vertical photograph of the confluence of the Parana and Paraguay Rivers northeast of the Argentine town of Corrientes. The Parana River flows westward; after merging with the Paraguay River, it begins to flow almost due south. Both rivers are sediment laden and appear to be out of their normal watercourses, thereby producing flooding conditions. The Paraguay River is characterized by the widely varying, meandering main channel; many oxbow lakes; and a tan sediment load. The Parana River has a smaller floodplain, a deeper channel, and a reddish-brown sediment load. As the two rivers merge and begin to flow southwestward, their individual sediment patterns do not mix readily, a common occurrence in which rivers with different densities of suspended particles tend to retain their individual color characteristics for many miles downstream. The Parana River, which flows approximately 2000 miles (3200 kilometers), is the second largest drainage system in South America; the Amazon River is the largest. An old river channel south of the Parana River parallels the present river channel. This much older stream channel seems to flow toward the city of Corrientes (estimated population of 200 000), the commercial center for this rich agricultural region of northeast Argentina and southwest Paraguay.