About this ebook
Dan Bosserman
Dan Bosserman, a resident of Oregon since 1950, grew up 13 miles from Sandy. He has lived near Sandy for 40 years and has been a writer for local newspapers, known for his historical columns. He is a volunteer in community organizations, including the Sandy Historical Society, which, along with descendants of original settlers, has provided photographs for this history of Sandy.
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Boring - Dan Bosserman
INTRODUCTION
Dominating the landscape east of Portland, Oregon, and for 50 miles in every direction, is Mount Hood, 11,249 feet high. Its Multnomah Indian name is Wy’east, and there are various legends about how the mountain came to be. In one version, the two sons of the Great Spirit Sahale fell in love with the beautiful maiden Loowit, who could not decide which to choose. The two braves, Wy’east and Klickitat, burned forests and villages in their battle over her. Their great anger led to their transformation into volcanoes.
Their battle is said to have destroyed the Bridge of the Gods and thus created the great Cascades Rapids of the Columbia River. Sahale became enraged and smote the three lovers. Seeing what he had done, he erected three symbolic mountain peaks to mark where each had fallen. He made beautiful Mount St. Helens for Loowit, proud and erect Mount Hood for Wy’east, and the somber Mount Adams for Klickitat, as if still mourning the loss of Loowit.
The mountain was given its present name in 1792 by Lt. William Broughton, a member of Capt. George Vancouver’s discovery expedition, in honor of Lord Samuel Hood, a British admiral at the Battle of the Chesapeake. Lieutenant Broughton observed its peak from Belle Vue Point at what is now called Sauvie Island during his travels up the Columbia River, writing, A very high, snowy mountain now appeared rising beautifully conspicuous in the midst of an extensive tract of low or moderately elevated land.
(This was the location of today’s Vancouver, Washington.)
The Portland metropolitan area, including suburbs, is one of the few places in the continental United States to have extinct volcanoes within a city’s limits. Boring itself lies at the base of one of these lava domes, and the generic term for at least 32 cinder cones and small shield volcanoes lying within a 13-mile radius is Boring Lava Field.
When the first of the Boring family came to the farming community, they little suspected that a broad geologic phenomenon stretching from Oregon to Washington across the Columbia River would also eventually bear their name.
The Boring Lava Field is an extinct Plio-Pleistocene volcanic field zone. The tiny, unincorporated town of Boring lies just to the southeast of the densest cluster of lava vents, which became active at least 2.7 million years ago and have been extinct for about 300,000 years. But what gave the area its distinct character—particularly its rolling hills, fish-filled streams, and fertile valleys—was the Missoula Flood at the end of the last glacial period around 15,000 years ago, when giant Lake Missoula in western Montana burst through an ice dam, sending a torrent of water that tossed boulders and ripped off cliff faces down the Columbia River and the Willamette Valley. Every few decades for several hundred years, the lake refilled until it pushed through again.
Scientists believe it was about this time that a land bridge connecting Alaska and Russia across what is now the Bering Strait sank into the sea; sometime before that, the first humans came to this continent, quickly spreading all across and down to South America. Why did the migrants come in the first place? Perhaps it was to follow herds of bison or other game that were migrating across the land bridge. Perhaps it was because of some change in living conditions on the Asian side of the bridge. Perhaps they thought the grass was greener on the other side of the Bering Strait. Nobody knows. Nor do we know if the wanderers spent years living on the land bridge, if they crossed in one quick motion, or if the migration comprised several distinct movements.
And we do not know yet if the original Americans used boats to cruise the Pacific coast to South America, where archeological sites are nearly as old as those in Alaska. There is now evidence that an ice shelf at the south of the land bridge may have been an ideal place for migrating, since the migrants would have had access to sea mammals and fish as they moved. Some scientists speculate that the first people of the Americas might have come by sea, having been blown off course by storms, since some human artifacts in eastern Oregon and South America seem to predate the end of the land bridge across the Bering Strait.
In any case, they quickly (in geological time) spread throughout North and South America and were the only occupants for some 12,000 years before European navigators discovered the New World.
The first Europeans to see the Oregon coast were Spanish sailors in the mid-16th century, who produced rough maps describing the area. In 1579, English seaman Francis Drake, in quest of Spanish loot and the Northwest Passage in his Golden Hind, anchored in an inlet north of the Golden Gate and took possession of a portion of the Pacific coast for Queen Elizabeth I. In 1778, the English sea captain James Cook visited and traded in Oregon.
In 1787, Boston merchants sent Robert Gray to the Oregon Country. On his second voyage, in 1792, Gray sailed over the bar of the Columbia River and named it for his ship, the Columbia. This was the first American claim to the Pacific Northwest by right of discovery. With the Louisiana Purchase and the Lewis and Clark Expedition in 1803, the Oregon Country’s destiny was inextricably joined to that of the United States.
The Oregon Trail began as an unconnected series of trails used by Native Americans. Fur traders expanded the route to transport
