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Coordinates: 48.281078°N, -121.84549°W
Approx. Elevation: 400 feet (122 meters)
USGS Map Area: Mount Higgins
Feature Type: Swamp
| Feature | USGS Topo Map |
|---|---|
| Barnaby Slough Number Two | Rockport |
| Olympia Marsh | La Conner |
| Lake Dorothy | Sultan |
| Roths Swamp | Monroe |
| Harts Swamp | Monroe |
| Musto Marsh | Cavanaugh Creek |
| Old Channel | Anacortes South |
| Waterloo Marsh | Oak Harbor |
| Ronald Bog | Edmonds East |
| Metcalf Marsh | Mount Si |
This is the location of the deadly landslide near the town of Oso that occurred on March 22, 2014. The massive hillside was soaked with precipitation that was 200 percent of normal for over six weeks causing the material to slide and run out well across the North Fork of the Stillaguamish River. The river was blocked and it flooded lands upstream for over a month before it breached and created a new channel.
Forty three people died in the slide and all of the homes and structures on Steelhead Drive were destroyed. Amazingly all of the bodies were recovered.
Oso Landslide March 22, 2014 is listed in the Swamps Category for Snohomish County in the state of Washington. Oso Landslide March 22, 2014 is displayed on the "Mount Higgins" USGS topo map quad. Anyone who is interested in visiting Oso Landslide March 22, 2014 can view and print the free topographic map, terrain map, and other maps using the link above. The location, topography, nearby roads and trails around Oso Landslide March 22, 2014 (Swamp) can be seen in the map layers above. The latitude and longitude coordinates (GPS waypoint) of Oso Landslide March 22, 2014 are 48.281078 (North), -121.84549 (West) and the approximate elevation is 400 feet (122 meters) above sea level. If you have visited Washington's Oso Landslide March 22, 2014 in Snohomish County before, please share your experience with a comment below.
Geologists from the University of Washington have just published an article documenting their analysis of the 2014 landslide near the small town of Oso, Washington. They determined that many slides have occurred along the North Fork Stillaguamish River over the last 10,000 years with several in the last 500 years. This high frequency of slides […]
