We returned from Canada on the fourth of August (Gee, nearly four weeks ago), stopping for a couple of night in Bellingham, Washington, This is a small city on the coast about 15 to 20 miles from the Canadian border. There we met some of our RV friends we have been traveling with on and off and on through our trip to the Yukon and Alaska. For me there was a bit of cultural shock --- getting used to all the traffic, all the people, the preoccupation of TV news on the Iraq War and American politics (sorry to say almost the exact same story with no progress, as when we crossed the border going north ten weeks ago), and distances now stated in miles rather than kilometers. For Madie, there was a great relief to have reliable telephone service to check on the family and grandchildren.
We returned from Canada on the fourth of August (Gee, nearly four weeks ago), stopping for a couple of night in Bellingham, Washington, This is a small city on the coast about 15 to 20 miles from the Canadian border. There we met some of our RV friends we have been traveling with on and off and on through our trip to the Yukon and Alaska. For me there was a bit of cultural shock --- getting used to all the traffic, all the people, the preoccupation of TV news on the Iraq War and American politics (sorry to say almost the exact same story with no progress, as when we crossed the border going north ten weeks ago), and distances now stated in miles rather than kilometers. For Madie, there was a great relief to have reliable telephone service to check on the family and grandchildren.
From Bellingham, we journeyed south and stopped to visit my sister-in-law who resides in an assisted living home in Bainbridge Island, across the strait from Seattle. This necessitated a pleasant ferry ride and a trip down west side of Puget Sound. From there we traveled on to Eugene, Oregon, to visit our relatives, and then on to Bend, Oregon.
Bend, Oregon is on the west side of the Cascade Mountains, about 120 miles west of Eugene. The drive between Eugene is very pretty, up fairly steep mountains, which are covered with dense spruce forest on the east side of the divide. Once you cross over the mountains, there is an obvious climate change, with the west side obviously much dryer. Although the area around Bend is heavily forested, it is obviously dryer.
We went to Bend, Oregon to visit a friend, Paul K, who was one of my mentors during my working life. We had a very nice visit and he showed us the sights around Bend. One day we visited Tumalo Falls, a very pretty water fall, up in the Cascade Mountains, which is the source of Bend’s water supply. See the picture of Paul and me with the waterfall in background.
The following day Paul took us to the Newberry National Volcanic Monument. The Cascades must be relatively new mountains, as there is much evidence of volcanic activity everywhere. As one drives down the highways, one see fairly high cinder cones from old volcanoes, as well as extensive lava beds. The Newberry National Monument features Paullina Peak, whose summit of nearly 8,000 feet overlooks a huge caldera. The peak of the mountain can be reached by a reasonable dirt road. From the peak, one can view two lakes, Paullina and East Lake. See the photo of a view of one of these lakes and the Obsidien Flow, described below.
The following day Paul took us to the Newberry National Volcanic Monument. The Cascades must be relatively new mountains, as there is much evidence of volcanic activity everywhere. As one drives down the highways, one see fairly high cinder cones from old volcanoes, as well as extensive lava beds. The Newberry National Monument features Paullina Peak, whose summit of nearly 8,000 feet overlooks a huge caldera. The peak of the mountain can be reached by a reasonable dirt road. From the peak, one can view two lakes, Paullina and East Lake. See the photo of a view of one of these lakes and the Obsidien Flow, described below.
Photos of chunks of obsidien. The picture is the edge of the flow. These rocks are about one and a half to two feet in diameter.
There is also a view of a lava flow named, Big Obsidian Flow. This is a lava flow with huge chunks of obsidian, a glass that apparently forms when lava cools so quickly, the silica can not crystallize. We drove down to the Obsidian Flow, and hiked on a trail made through it. The obsidian was black in blocks ranging from a few inches many measuring perhaps eight to ten feet on a side. The sides of many of the chunks were sharp. I am told that the material can be knapped, and was used by Native Americans to form arrowheads, spear points and cutting tools. I am sure the obsidian must have been traded by Native Americans, since deposits such as this while not extremely rare, are not to commonly found either. On the way back from Bend, we stopped and looked at Salt Creek Falls. This is a beautiful waterfall, dropping over the edge of an old lava flow into a valley below. See picure.
After our Oregon visits, we went to the Bay area in California, where we visited family. We are now in Sacramento, continuing family visits. Next week we will start toward Albuquerque to attend the Balloon Festival.
After our Oregon visits, we went to the Bay area in California, where we visited family. We are now in Sacramento, continuing family visits. Next week we will start toward Albuquerque to attend the Balloon Festival.