|
|
Mount Saint Helens
| title |
Mount Saint Helens |
| description |
Mount Saint Helens exemplifies how Earth's topographic form can change greatly even within our lifetimes. The mountain is one of several prominent volcanoes of the Cascade Range that stretches from British Columbia, Canada, southward through Washington, Oregon and into northern California. Mount Adams (left background) and Mount Hood (right background) are also seen in this view, which was created entirely from elevation data produced by the Shuttle Radar Topography Mission. Prior to 1980, Mount Saint Helens had a shape roughly similar to other Cascade peaks, a tall, bold, irregular conic form that rose to 9,677 feet (2,950 meters). However, the explosive eruption of May 18, 1980, caused the upper 1,300 feet (400 meters) of the mountain to collapse, slide and spread northward, covering much of the adjacent terrain (lower left), leaving a crater atop the greatly shortened mountain. Subsequent eruptions built a volcanic dome within the crater, and the high rainfall of this area lead to substantial erosion of the poorly consolidated landslide material. Eruptions at Mount Saint Helens subsided in 1986, but renewed volcanic activity here and at other Cascade volcanoes is inevitable. Predicting such eruptions still presents challenges, but migration of magma within these volcanoes often produces distinctive seismic activity and minor but measurable topographic changes that can give warning of a potential eruption. Image credit: NASA/JPL/NGA |
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Hubble Sees Faintest Stars i
…
| Title |
Hubble Sees Faintest Stars in a Globular Cluster |
|
Hubble Sees Faintest Stars i
…
| Title |
Hubble Sees Faintest Stars in a Globular Cluster |
|
Hubble Sees Faintest Stars i
…
| Title |
Hubble Sees Faintest Stars in a Globular Cluster |
|
Hubble Sees Faintest Stars i
…
| Title |
Hubble Sees Faintest Stars in a Globular Cluster |
|
Hubble Sees Faintest Stars i
…
| Title |
Hubble Sees Faintest Stars in a Globular Cluster |
|
How White Dwarfs Get Their '
…
| Title |
How White Dwarfs Get Their 'Kicks' |
|
Hubble Sees Faintest Stars i
…
| Title |
Hubble Sees Faintest Stars in a Globular Cluster |
|
Hubble Sees Faintest Stars i
…
| Title |
Hubble Sees Faintest Stars in a Globular Cluster |
|
How White Dwarfs Get Their '
…
| Title |
How White Dwarfs Get Their 'Kicks' |
|
How White Dwarfs Get Their '
…
| Title |
How White Dwarfs Get Their 'Kicks' |
|
How White Dwarfs Get Their '
…
| Title |
How White Dwarfs Get Their 'Kicks' |
|
Burn Scars in the Pacific No
…
| Title |
Burn Scars in the Pacific Northwest |
| Description |
Fire season is winding down in western North America, but this false-color image from the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Aqua satellite reveals the season?s fire-scarred landscape. Vegetation is in shades of green, while burned areas are red. Scars dot the Northern Rockies from Canada (roughly top half of image) to Montana (bottom right) and Idaho, to its west. Additional large scars are visible in the Coast Mountains (left) which stretch from British Columbia, Canada, southward into Washington. Clouds are white and light blue, lakes and rivers are dark blue, and snow is bright blue. Naturally bare ground (or extremely low vegetation), such as on the highest mountains ridges at top center, or in the Columbia River Basin (bottom center), is pinkish tan. MODIS captured this image on October 4, 2003. Image courtesy Jesse Allen, based on data from the MODIS Rapid Response Team at NASA GSFC |
|
Fires in British Columbia
| Title |
Fires in British Columbia |
| Description |
A large fire in western British Columbia was spilling smoke down over the glacier-covered slopes of the Coast Range Mountains on July 28, 2004. In the deeply carved valleys between the white-capped peaks, turquoise rivers thick with finely ground glacial sediment flow out to the Pacific Ocean through the narrow gap between Vancouver Island (bottom left) and mainland Canada. The Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA's Aqua satellite captured this image, and the places where the sensor detected actively burning fires are outlined in red. The high-resolution image provided above is 250 meters per pixel. The MODIS Rapid Response System provides this image at additional resolutions. Image courtesy Jeff Schmaltz, MODIS Rapid Response Team, NASA-GSFC |
|
Fires in Northern Washington
| Title |
Fires in Northern Washington |
| Description |
In the mountains of northern Washington, the Tripod Complex Fire burned from July into August. This image of the region was captured by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov ] on NASA's Aqua [ http://aqua.nasa.gov ] satellite on August 6, 2006. Places where MODIS detected actively burning fires are marked in red. The actively burning parts of the Tripod Complex make two rough circles in the rugged terrain northeast of the city of Twisp. Smoke billows thickly across the state and into British Columbia, Canada. According to the August 7 report from the National Interagency Fire Center, [ http://www.nifc.gov/information.html ] the Tripod Complex Fire had grown to an estimated 57, 535 acres, and firefighters had it about 10 percent contained. Numerous residences and other structures were threatened by the fire, which was burning through timber that had been killed by beetle infestation. The high-resolution image provided above has a spatial resolution of 250 meters per pixel. NASA image courtesy the MODIS Rapid Response Team, [ http://rapidfire.sci.gsfc.nasa.gov ] Goddard Space Flight Center |
|
Fires in the Northern Rockie
…
| Title |
Fires in the Northern Rockies |
| Description |
On September 6, 2003, dozens of large fires were burning in the northern Rockies of British Columbia (top), Montana (bottom right), Idaho (bottom center), and Washington (bottom left). In Montana, a line of fires stretches southward from the U.S.-Canada border for 190 kilometers (118 miles), creating a wall of smoke that hangs over the Lewis Range Mountains east of Flathead Lake. This image of the fires (marked in red) was captured by the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Aqua satellite on September 6. The high-resolution image provided above is 500 meters per pixel. The MODIS Rapid Response System provides this image at MODIS' maximum spatial resolution of 250 meters. Image courtesy Jacques Descloitres, MODIS Rapid Response Team at NASA GSFC |
|
Fires in Western Canada
| Title |
Fires in Western Canada |
| Description |
On August 1, 2003, dozens of large fires were burning across western North America in Canada (top half of image) and the United States (bottom half). Huge plumes of smoke were streaming northeastward from massive fires in Canada's British Columbia (left) and Alberta (right) provinces, while across the international border, fires were burning in (left to right) Washington, Idaho, and Montana. This image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Aqua satellite. The high-resolution image provided above is 500 meters per pixel. The MODIS Rapid Response System provides this image at MODIS' maximum spatial resolution of 250 meters. Image courtesy Jeff Schmaltz, MODIS Rapid Response Team, NASA GSFC |
|
Fires in Western Canada
| Title |
Fires in Western Canada |
| Description |
Dozens of large fires were burning across British Columbia, Canada, on August 20, 2003. The fires (marked with yellow) have forced hundreds of people to evacuate their homes and put thousands on evacuation alert. This image of the fires was captured by the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Aqua satellite. British Columbia is at top left, with Alberta to the east. At the bottom are Washington, Idaho, and Montana. The high-resolution image provided above is 500 meters per pixel. The MODIS Rapid Response System provides this image at MODIS' maximum spatial resolution of 250 meters. Image courtesy Jacques Descloitres, MODIS Rapid Response Team at NASA GSFC |
|
Fires in Western Canada: Nat
…
nasa, nasanaturalhazards
On August 1, 2003, dozens of
…
UnitedStates.AMOA2003213
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003-08-01 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
UnitedStates.AMOA2003213 |
|
Earth observations taken dur
…
johnsonspacecentermediaarchi
…
Earth observations taken dur
…
sts047-151-488
| mediatype |
IMAGE |
| mediatype |
image |
| date |
09/15/92 |
| creator |
NASA |
| identifier |
sts047-151-488 |
|
Okanagan Fire, British Colum
…
nasa, nasaimageofthedaygalle
…
About 50 miles north of the
…
okanagan_ast_2003245
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003-09-05 |
| creator |
NASA -- Image courtesy NASA/GSFC/MITI/ERSDAC/JAROS, and U.S./Japan asterweb.jpl.nasa.gov/ ASTER Science Team |
| identifier |
okanagan_ast_2003245 |
|
Fires in Western Canada: Nat
…
nasa, nasanaturalhazards
Dozens of large fires were b
…
Canada.AMOA2003232
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003-08-20 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
Canada.AMOA2003232 |
|
Burn Scars in the Pacific No
…
nasa, nasanaturalhazards
Fire season is winding down
…
aqua_pacnwscars_04oct03
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003-10-04 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
aqua_pacnwscars_04oct03 |
|
Fires in the Northern Rockie
…
nasa, nasanaturalhazards
On September 6, 2003, dozens
…
Montana.AMOA2003249
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003-09-06 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
Montana.AMOA2003249 |
|
Western United States and So
…
nasa, nasaimageofthedaygalle
…
This natural-color image fro
…
PIA04330
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003 |
| creator |
NASA -- Image courtesy NASA/GSFC/LaRC/JPL, MISR Team. mailto:jknighton@clear-light.com Jim Knighton of Clear Light Image Products produced the image mosaic. Please note that the high-resolution TIF image is provided here at a pixel resolution of approximately 1.1 kilometers, but is available from the producer at a resolution of 278 meters. Text by Clare Averill (Acro Service Corporation/JPL). |
| identifier |
PIA04330 |
|
Tagish Lake, Canada : Image
…
nasa, nasaimageofthedaygalle
…
On January 18, 2000, meteori
…
landsat_tagish
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2000-05-08 |
| creator |
NASA -- Image courtesy Brian Montgomery, NASA GSFC, Landsat 7 data provided by the edc.usgs.gov/ EROS Data Center. |
| identifier |
landsat_tagish |
|
Anaglyph, North America
PIA03378
Sol (our sun)
C-Band Interferometric Radar
| Title |
Anaglyph, North America |
| Original Caption Released with Image |
This anaglyph (stereoscopic view) of North America was generated with data from the Shuttle Radar Topography Mission (SRTM). It is best viewed at or near full resolution with anaglyph glasses. For this broad view the resolution of the data was first reduced to 30 arcseconds (about 928 meters north-south and 736 meters east-west in central North America), matching the best previously existing global digital topographic data set called GTOPO30. The data were then resampled to a Mercator projection with approximately square pixels (about one kilometer, or 0.6 miles, on each side). Even at this decreased resolution the variety of landforms comprising the North American continent is readily apparent. Active tectonics (structural deformation of the Earth's crust) along and near the Pacific North American plate boundary creates the great topographic relief seen along the Pacific coast. Earth's crustal plates converge in southern Mexico and in the northwest United States, melting the crust and producing volcanic cones. Along the California coast, the plates are sliding laterally past each other, producing a pattern of slices within the San Andreas fault system. And, where the plates are diverging, the crust appears torn apart as one huge tear along the Gulf of California (northwest Mexico), and as the several fractures comprising the Basin and Range province (in and around Nevada). Across the Great Plains, erosional patterns dominate, with stream channels surrounding and penetrating the remnants of older smooth slopes east of the Rocky Mountains. This same erosion process is exposing the bedrock structural patterns of the Black Hills in South Dakota and the Ozark Mountains in Arkansas. Lateral erosion and sediment deposition by the Mississippi River has produced the flatlands of the lower Mississippi Valley and the Mississippi Delta. To the north, evidence of the glaciers of the last ice age is widely found, particularly east of the Canadian Rocky Mountains and around the Great Lakes. From northeastern British Columbia, across Alberta, Saskatchewan, and Manitoba to North Dakota and Minnesota, huge striations clearly show the flow pattern of the glaciers. And southwest of Lakes Michigan, Huron, and Erie, arcing ridges of sediment, called terminal moraines, show where glaciers dumped sediment at their melting ends. In eastern Canada, New York, and New England, the terrain has been scoured by glaciers, and eroded by streams, particularly along fractures in the bedrock. In Labrador and Quebec, the Mistastin, Manicougan, and Clearwater Lakes meteor impact craters can also be seen. Further south, narrow curving ridges of upturned and eroded layered rocks form most of the Appalachian Mountains. In contrast, around the Caribbean Sea region (Yucatan, Florida, and the Bahamas), flat-lying, stable limestone platforms are common, while the most eastern islands of the Caribbean include active volcanoes along another convergence zone of tectonic plates. This, anaglyph was created by deriving a shaded relief image from the SRTM data, draping it back over the SRTM elevation model, and then generating two differing perspectives, one for each eye. Illumination is from the north (top). When viewed through special glasses, the anaglyph is a vertically exaggerated view of the Earth's surface in its full three dimensions. Anaglyph glasses cover the left eye with a red filter and cover the right eye with a blue filter. Elevation data used in this image were acquired by the SRTM aboard the Space Shuttle Endeavour, launched on Feb. 11, 2000. SRTM used the same radar instrument that comprised the Spaceborne Imaging Radar-C/X-Band Synthetic Aperture Radar (SIR-C/X-SAR) that flew twice on the Space Shuttle Endeavour in 1994. SRTM was designed to collect 3-D measurements of the Earth's surface. To collect the 3-D data, engineers added a 60-meter (approximately 200-foot) mast, installed additional C-band and X-band antennas, and improved tracking and navigation devices. The mission is a cooperative project between NASA, the National Imagery and Mapping Agency (NIMA) of the U.S. Department of Defense and the German and Italian space agencies. It is managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif., for NASA's Earth Science Enterprise, Washington, D.C. Location: 15 to 60 degrees North latitude, 50 to 130 degrees West longitude Orientation: North toward the top, Mercator projection Image Data: Shaded SRTM elevation model Original Data Resolution: SRTM 1 arcsecond (about 30 meters or 98 feet) Date Acquired: February 2000 |
|
Shaded Relief with Height as
…
PIA03377
Sol (our sun)
C-Band Interferometric Radar
| Title |
Shaded Relief with Height as Color, North America |
| Original Caption Released with Image |
This image of North America was generated with data from the Shuttle Radar Topography Mission (SRTM). For this broad view the resolution of the data was first reduced to 30 arcseconds (about 928 meters north-south and 736 meters east-west in central North America), matching the best previously existing global digital topographic data set called GTOPO30. The data were then resampled to a Mercator projection with approximately square pixels (about one kilometer, or 0.6 miles, on each side). Even at this decreased resolution the variety of landforms comprising the North American continent is readily apparent. Active tectonics (structural deformation of the Earth's crust) along and near the Pacific -- North American plate boundary creates the great topographic relief seen along the Pacific coast. Earth's crustal plates converge in southern Mexico and in the northwest United States, melting the crust and producing volcanic cones. Along the California coast, the plates are sliding laterally past each other, producing a pattern of slices within the San Andreas fault system. And, where the plates are diverging, the crust appears torn apart as one huge tear along the Gulf of California (northwest Mexico), and as the several fractures comprising the Basin and Range province (in and around Nevada). Across the Great Plains, erosional patterns dominate, with streams channels surrounding and penetrating the remnants of older smooth slopes east of the Rocky Mountains. This same erosion process is exposing the bedrock structural patterns of the Black Hills in South Dakota and the Ozark Mountains in Arkansas. Lateral erosion and sediment deposition by the Mississippi River has produced the flatlands of the lower Mississippi Valley and the Mississippi Delta. To the north, evidence of the glaciers of the last ice age is widely found, particularly east of the Canadian Rocky Mountains and around the Great Lakes. From northeastern British Columbia, across Alberta, Saskatchewan, and Manitoba to North Dakota and Minnesota, huge striations clearly show the flow pattern of the glaciers. And southwest of Lakes Michigan, Huron, and Erie, arcing ridges of sediment, called terminal moraines, show where glaciers dumped sediment at their melting ends. In eastern Canada, New York, and New England, the terrain has been scoured by glaciers, and eroded by streams, particularly along fractures in the bedrock. In Labrador and Quebec, the Mistastin, Manicougan, and Clearwater Lakes meteor impact craters can also be seen. Further south, narrow curving ridges of upturned and eroded layered rocks form most of the Appalachian Mountains. In contrast, around the Caribbean Sea region (Yucatan, Florida, and the Bahamas), flat-lying, stable limestone platforms are common, while the most eastern islands of the Caribbean include active volcanoes along another convergence zone of tectonic plates. Two visualization methods were combined to produce the image: shading and color coding of, topographic height. The shade image was derived by computing topographic slope in the northwest-southeast direction, so that northwest slopes appear bright and southeast slopes appear dark. Color coding is directly related to topographic height, with green at the lower elevations, rising through yellow and tan, to white at the highest elevations. Elevation data used in this image were acquired by the Shuttle Radar Topography Mission aboard the Space Shuttle Endeavour, launched on Feb. 11, 2000. SRTM used the same radar instrument that comprised the Spaceborne Imaging Radar-C/X-Band Synthetic Aperture Radar (SIR-C/X-SAR) that flew twice on the Space Shuttle Endeavour in 1994. SRTM was designed to collect 3-D measurements of the Earth's surface. To collect the 3-D data, engineers added a 60-meter (approximately 200-foot) mast, installed additional C-band and X-band antennas, and improved tracking and navigation devices. The mission is a cooperative project between NASA, the National Imagery and Mapping Agency (NIMA) of the U.S. Department of Defense and the German and Italian space agencies. It is managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif., for NASA's Earth Science Enterprise, Washington, D.C. Location: 15 to 60 degrees North latitude, 50 to 130 degrees West longitude Orientation: North toward the top, Mercator projection Image Data: shaded and colored SRTM elevation model Original Data Resolution: SRTM 1 arcsecond (about 30 meters or 98 feet) Date Acquired: February 2000 |
|
Natural Color Mosaic of Nort
…
PIA04361
Sol (our sun)
C-Band Interferometric Radar
…
| Title |
Natural Color Mosaic of North America |
| Original Caption Released with Image |
This natural-color image combines cloud-free data from over 500 Multi-angle Imaging SpectroRadiometer (MISR) orbits with shaded relief Digital Terrain Elevation models from the Shuttle Radar Topography Mission (SRTM) and other sources. An astonishing diversity of geological features, ecological systems and human landscapes across North America is indicated within the image, which spans from 56N, 136W at the upper left to 16N 48W at lower right. In addition to the contiguous United States, the scene spans from British Columbia in the northwest to Newfoundland in the northeast, and extends eastward to the lonely Bermuda Islands and southward to the Bahamas, Cuba and Mexico. Draped in green, the eastern and central United States and Canada contrast with the vibrant geology that is laid bare across the arid portions of the southwestern United States and central Mexico. Along Mexico's east coast, the lush vegetation to the east of the Sierra Madre mountain range indicates the orographic rainfall gradient along this subtropical-tropical coast. In the high Rocky Mountains and in British Columbia's Coast Range, many peaks remain snow-covered year-round. The Multi-angle Imaging SpectroRadiometer observes the daylit Earth continuously and every 9 days views the entire globe between 82 north and 82 south latitude. This data product was generated from a portion of the imagery acquired during years 2000 - 2004. The image is displayed in an Albers Conic Equal Area projection with the projection center at 36 North, 92 West. MISR was built and is managed by NASA's Jet Propulsion Laboratory, Pasadena, CA, for NASA's Office of Earth Science, Washington, DC. The Terra satellite is managed by NASA's Goddard Space Flight Center, Greenbelt, MD. JPL is a division of the California Institute of Technology. |
|
Mount Saint Helens, Washingt
…
PIA06668
Sol (our sun)
C-Band Imaging Radar, X-Band
…
| Title |
Mount Saint Helens, Washington, USA, SRTM Perspective: Shaded Relief and Colored Height |
| Original Caption Released with Image |
(about 100 miles) Location: 46.2 degrees North latitude, 122.2 degrees West longitude Orientation: View Southeast Image Data: Shaded and colored SRTM elevation model Date Acquired: February 2000, Mount Saint Helens is a prime example of how Earth's topographic form can greatly change even within our lifetimes. The mountain is one of several prominent volcanoes of the Cascade Range that stretches from British Columbia, Canada, southward through Washington, Oregon, and into northern California. Mount Adams (left background) and Mount Hood (right background) are also seen in this view, which was created entirely from elevation data produced by the Shuttle Radar Topography Mission. Prior to 1980, Mount Saint Helens had a shape roughly similar to other Cascade peaks, a tall, bold, irregular conic form that rose to 2950 meters (9677 feet). However, the explosive eruption of May 18, 1980, caused the upper 400 meters (1300 feet) of the mountain to collapse, slide, and spread northward, covering much of the adjacent terrain (lower left), leaving a crater atop the greatly shortened mountain. Subsequent eruptions built a volcanic dome within the crater, and the high rainfall of this area lead to substantial erosion of the poorly consolidated landslide material. Eruptions at Mount Saint Helens subsided in 1986, but renewed volcanic activity here and at other Cascade volcanoes is inevitable. Predicting such eruptions still presents challenges, but migration of magma within these volcanoes often produces distinctive seismic activity and minor but measurable topographic changes that can give warning of a potential eruption. Three visualization methods were combined to produce this image: shading of topographic slopes, color coding of topographic height, and then projection into a perspective view. The shade image was derived by computing topographic slope in the northeast-southwest (left to right) direction, so that northeast slopes appear bright and southwest slopes appear dark. Color coding is directly related to topographic height, with green at the lower elevations, rising through yellow and tan, to white at the highest elevations. The perspective view simulates the geometry of the surface as it would be viewed on a clear day. Elevation data used in this image were acquired by the Shuttle Radar Topography Mission aboard the Space Shuttle Endeavour, launched on Feb. 11, 2000. SRTM used the same radar instrument that comprised the Spaceborne Imaging Radar-C/X-Band Synthetic Aperture Radar (SIR-C/X-SAR) that flew twice on the Space Shuttle Endeavour in 1994. SRTM was designed to collect 3-D measurements of the Earth's surface. To collect the 3-D data, engineers added a 60-meter (approximately 200-foot) mast, installed additional C-band and X-band antennas, and improved tracking and navigation devices. The mission is a cooperative project between NASA, the National Geospatial-Intelligence Agency (NGA) of the U.S. Department of Defense and the German and Italian space agencies. It is managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif., for NASA's NASA's Science Mission Directorate, Washington, D.C. Size: View distance about 150 km |
|
Western United States and So
…
PIA04330
Sol (our sun)
Multi-angle Imaging SpectroR
…
| Title |
Western United States and Southwestern Canada |
| Original Caption Released with Image |
This natural-color image from the Multi-angle Imaging SpectroRadiometer (MISR) captures the beauty of the western United States and Canada. Data from 45 swaths from MISR's vertical-viewing (nadir) camera were combined to create this cloud-free mosaic. The image extends from 48° N 128° W in the northwest, to 32°N, 104° W in the southeast, and has been draped over a shaded relief Digital Terrain Elevation Model from the United States Geological Survey. The image area includes much of British Columbia, Alberta and Saskatchewan in the north, and extends southward to California, Arizona and New Mexico. The snow-capped Rocky Mountains are a prominent feature extending through British Columbia, Montana, Wyoming, Colorado and New Mexico. Many major rivers originate in the Columbia Plateau region of Washington, Oregon and Idaho. The Colorado Plateau region is characterized by the vibrant red-colored rocks of the Painted Desert in Utah and Arizona, and in New Mexico, White Sands National Park is the large white feature in the Southeast corner of the image with the Malpais lava flow just to its North. The southwest is dominated by the Mojave Desert of California and Nevada, California's San Joaquin Valley, the Los Angeles basin and the Pacific Ocean. The Multi-angle Imaging SpectroRadiometer observes the daylit Earth continuously from pole to pole, and every 9 days views the entire globe between 82 degrees north and 82 degrees south latitude. This data product was generated from a portion of the imagery acquired during 2000-2002. The panels utilize data from blocks 45 to 65 within World Reference System-2 paths 31 to 53. MISR was built and is managed by NASA's Jet Propulsion Laboratory, Pasadena, CA, for NASA's Office of Earth Science, Washington, DC. The Terra satellite is managed by NASA's Goddard Space Flight Center, Greenbelt, MD. JPL is a division of the California Institute of Technology. |
|
Northwest Washington State
| Title |
Northwest Washington State |
| Description |
Portions of northwest Washington State (48.0N, 122.5) can be seen in this view as well as portions of British Columbia, Canada. The snow covered Cascade Mountains are on the eastern side of the scene. Vancouver Island is visible in the northeast corner of the photo. The strait of Juan de Fuca separates Vancouver Islannd from the northwest corner of Washington. Seattle is near the center and the snow covered Olympic Mountains are to the east. |
| Date Taken |
1973-06-22 |
|
Puget Sound, Seattle, WA, US
…
| Title |
Puget Sound, Seattle, WA, USA, Vancouver, British Columbia, Canada |
| Description |
The Olympic Peninsula of NW Washington state, Puget Sound and the Cascade Range of British Columbia, Canada form the setting for this unusually clear photo of one of the most cloudy sections of North America (48.0N, 123.0W) where rainfall exceeds 120 inches anually. The cities of Seattle/Tacoma and Burlington, as well as the Canadian city of Vancouver can be seen in great detail along the heavily indented coastline of this glacier sculpted scene. |
| Date Taken |
1992-09-20 |
|
|
