We thought it might be fun to summarize the states we drove through on this trip.
California
Oregon (overnight)
Washington (overnights)
Idaho
Montana (overnights)
Wyoming (overnight)
South Dakota (overnight)
Minnesota
Wisconsin
Illinois (overnights)
Indiana
Ohio (overnight)
Pennsylvania
New Jersey (overnights)
Maryland
West Virginia
Virginia (overnight)
Tennessee (overnight)
Arkansas
Oklahoma (overnight)
Texas (two left wheels in the north west corner as we entered New Mexico)
New Mexico
Arizona
California (again)
Saturday, October 18, 2014
10/12 -- Drive Home
Because we were 800 miles from home, we had planned to take a day and a half to drive back, but we are still getting up early, and there is really no place in California between the south east border and San Francisco that we want to spend a night if we don't have to, so we hopped in the car at 7:30am and just drove. If we hadn't stopped for sushi near home, we would have made it in 12 hours.
The scenery across the southern part of the trip is all pretty stark, and it just gets more dreary as you go west. Suffice it to say that I am not a big desert fan, a short visit is interesting, but give me greenery any day. We did get to see two of the airplane mothball fleets, one in Arizona, the other at Tehachapi, CA. There was also a huge wind farm at Tehachapi that looked kind of like a white-haired and sparse crewcut across the hills.
We had a wonderful time, and I might actually consider another cross-country drive, but it sure feels good to get home!
The scenery across the southern part of the trip is all pretty stark, and it just gets more dreary as you go west. Suffice it to say that I am not a big desert fan, a short visit is interesting, but give me greenery any day. We did get to see two of the airplane mothball fleets, one in Arizona, the other at Tehachapi, CA. There was also a huge wind farm at Tehachapi that looked kind of like a white-haired and sparse crewcut across the hills.
Western Arizona scenery |
Happy sign -- back in our home state |
Eastern California -- hard to tell its not Arizona |
Long straight road thru the desert |
Plane heaven in Tehachapi. Windmills in the background. |
Wind farm, creating a crewcut on the hill |
Sun setting in the bay area as we near home. |
We had a wonderful time, and I might actually consider another cross-country drive, but it sure feels good to get home!
Saturday, October 11, 2014
10/11 -- Hiking the Grand Canyon Rim Trail and Recovering
Look at how the tree has twisted |
Part of the Abyss |
A wider section of the rim-side path... |
Jim at one of the lookouts |
Tarantula? It was about 3 inches across -- small for a tarantula, but big and hairy for a spider |
Lunch had a relatively rejuvenating effect on me, so we went to the Geology Museum and stumbled into a ranger talk about how the Grand Canyon was formed. She was really entertaining and played to the school kids in the audience. Basically, the very bottom of the canyon is 'basement rock', an igneous rock that is interleaved with granite. On top are lots of layers of sedimentary rock -- limestone, mudstone, and sandstone, that suggest the area was an inland sea 8 different times over the last 550 million years. Then the plateau was uplifted, but as a flat whole, not like the tilted rocks you see in lots of other places. There are lots of fossils in the sediment, but the top 250 million years worth of sediments have all disappeared, worn away by wind and water erosion so there are no dinosaur fossils. The Colorado river settled on its current channel about 6 million years ago, and has consistently been about 300 feet wide, cutting its way deeper and deeper into the rock. The river falls 14,000 feet from its source in the Rockies to its output in the Pacific, giving it a lot more force than the Mississippi, which only falls 2000 feet from Minnesota to Louisiana. Combined with the dessert climate, which has monsoon style rainfalls for 2 months each summer, the upper layers that river initially cut have been further eroded over the last 6 million years by wind and water to be the 10 miles wide you currently see.
After that, we drove to the main Visitor Center (kind of short on information) and walked to nearby Mather Point for our last outlook to the canyon before heading to our hotel for the night.
Hard to believe that ribbon of a river is 300 ft wide, but it is about a mile down. |
Our grand adventure is nearly over -- we are 795 miles from home and heading out tomorrow. Based on where we will probably be by 5 or 6pm, a typical stopping time, we may just tough it out and go all the way home. In some ways I am glad to be going home -- tired of living out of a suitcase and with the limited clothing selection I guessed at 7 weeks ago. But this adventure has been such a hoot in so many ways, it's a shame it is almost over.
10/10 - The Grand Canyon
In the spirit of adventure, instead of taking I-40 to the Grand Canyon, we took state roads north along the Colorado and Utah borders and drove through the enormous Navaho Nation. It was raining in Taos and some weather reports talked about locally heavy snow along our route, but the hotel staff verified we weren't taking high altitude roads, so off we went.
At first, we drove down the Rio Grande Canyon, then set off along drier areas. The scenery was often spectacular and reminded me of Utah, but I can't imagine how people support themselves or why I would want to live there.
Once we got to the Grand Canyon east entrance, we gained an hour and had time to spare before checking in, so we stopped at almost all the viewpoints and one museum. The museum showed the Tusayan Ruins -- parts of the walls and two kivas (ceremonial halls) of the Tusayan culture. The homes were stone built and entered from the top, as were the kivas. Not sure that would be a good place to be old in!
I was here for a few hours with Kristen in 1975 and nothing but the canyon itself is recognizable. Jim was here for 2 days in the late 50s and he sees stuff he saw then, but a lot has changed. The canyons are amazing, but I'm afraid the photos will be inadequate, like they were in 1975.
We went to dinner at a different lodge and began to understand why the park emphasizes using the free shuttle. Parking was ridiculous close by, and I got all turned around when we found a parking lot, and luckily Jim prevailed and we got some help and found we were only a 7 minute walk to our restaurant. On the way driving to dinner, bunches of people near our hotel were ogling the deer near the road and I was like so 'ho-hum, another deer'. On the way back from dinner, a small herd of elk crossed the road in front of us and I fumbled with the camera to get settings to take a decent photo. So much for wildlife ennui!
The only bad part is that there is only internet access in the lobby and dining room, a hike from our room, so staying in touch will be a challenge.
Rio Grande Canyon walls |
Rio Grande in the Taos area |
Cliffs somewhere in New Mexico, above and below |
Shiprock in New Mexico, in Navaho Nation |
Hoodoos above, other rock formations below. In Navaho Nation, either New Mexico or Arizona |
Drawing of what the original abodes would have looked like. What we saw were the foundations, a couple of stones high. |
The Grand Canyon, looking west from the Desert View (eastern) stop |
Jim at another viewpoint, looking west |
Grand Canyon eastern view |
Grand Canyon eastern view at sunset |
I was here for a few hours with Kristen in 1975 and nothing but the canyon itself is recognizable. Jim was here for 2 days in the late 50s and he sees stuff he saw then, but a lot has changed. The canyons are amazing, but I'm afraid the photos will be inadequate, like they were in 1975.
We went to dinner at a different lodge and began to understand why the park emphasizes using the free shuttle. Parking was ridiculous close by, and I got all turned around when we found a parking lot, and luckily Jim prevailed and we got some help and found we were only a 7 minute walk to our restaurant. On the way driving to dinner, bunches of people near our hotel were ogling the deer near the road and I was like so 'ho-hum, another deer'. On the way back from dinner, a small herd of elk crossed the road in front of us and I fumbled with the camera to get settings to take a decent photo. So much for wildlife ennui!
Dumb camera didn't want to use flash, did multiple photos and combined while nasty elk refused to stay in one place. You CAN discern mother and calf, however. |
The only bad part is that there is only internet access in the lobby and dining room, a hike from our room, so staying in touch will be a challenge.
Thursday, October 9, 2014
10/9 -- Capulin Volcano and Taos
Just a note to anyone considering staying overnight in Clayton, NM. Don't. Unless you have earplugs or take your hearing aids out at night (like me). The train runs right thru town and starts rolling around dinner time and a new one comes thru every hour or so, horns blaring. Apparently no one here objects. Maybe a place with double pane windows would be better. Kind of a shame, because for a dinky place in the middle of nowhere, it was actually quite nice. Except for the night trains.
On a cheerier note, we had an energetic day today. It was raining a bit as we headed out, but we drove out of it before we got to the Capulin Volcano National Monument. It is a cinder cone volcano that last erupted about 42,000 years ago. There are several trails and we did all but one. The parking lot of the highest hike was at 7800 feet of elevation and the rim trail went up 305 feet from there -- and partway back down and up again. It was rated as 'moderate' and it was nicely paved, but going that much up when you are not adapted to the elevation made it more like strenuous. Our other big hike, the 'Boca Trail' started out much lower, maybe 7200 feet (Endomondo hiccuped and couldn't track us on GPS, so we don't know for sure). This trail was listed as strenuous to moderate and even though it was twice as long, it was lots easier. From the top of the rim, the views of the area were spectacular. We also did a short nature trail with some interesting rock formations where lava sort of squeezed out at a week spot -- sort of a lava pimple on a flat plain.
Back in the car, we headed to Taos. We went thru the Cimmaron Canyon state park, which was beyond lovely -- very steep cliffs, bubbly little river and wonderfully contrasting trees on the mountains -- lots of dark green firs interspersed with bright yellow aspens and birches -- totally spectacular.
Taos itself is a bit of a disappointment. After reading about the 'Santa Fake' building style in Santa Fe, I had expected better in Taos. Maybe all the downtown buildings are original, but I wouldn't want to bet on it. It is very touristy -- sort of a southwestern Carmel. We did have lovely lunch and walked around the downtown for an hour before heading to our hotel. This month is a big one for Taos -- apparently people come from all over to see the trees change color like going to New Hampshire or Vermont back east. So the place is totally busy -- heading north to our hotel at 3:30, we were stunned at the traffic backup going south through town. Taos does have good restaurants! Our yummy lunch was followed by an interesting dinner -- I had buffalo filet mignon -- very tasty.
A tree is growing out of one of the 'lava pimples' near the Visitor Center. |
There are a lot of extinct volcanoes in the area. |
Jim hiking the rim trail with the plains far below. |
More lovely 4-lane 70mph road in remote New Mexico |
Our first view of the interspersed green and yellow trees |
The aspens close up. We saw birches later with the same bright yellow leaves. |
The Taos main square |
Wednesday, October 8, 2014
10/8 -- On to New Mexico
West Oklahoma looks more like what we expected |
Drilling for oil we think, or maybe fracking |
Older storage tanks for something - natural gas? |
Big wind farms with more mills being added |
Some of the old windmills still work. Looks like many are pumping water for the cattle. |
Slightly hilly, but the road sure is straight. |
One of the charming old homes - probably could get it cheap. |
One of many derricks |
It was a relatively short driving day and we got to Clayton and our ancient hotel (Hotel Eklund) just before 3pm, except the time zone had just changed so it was way too early to check in. The desk clerk suggested we check out the local history museum, which was wonderful. Though I have to say that seeing stuff in a museum that I recognized using in my youth was kind of humbling! We're becoming antiques! The very chatty proprietor of the museum recommended a stop at Clayton Lake State Park, which has a very large collection of dinosaur footprints, discovered after a dam created the lake.
We headed out there through some very interesting territory and wandered out to the footprints. On the way there and back we saw lots of grasshoppers and butterflies and a praying mantis (first one I've seen in the wild since I was a kid) and a probable locust. The foot prints were hard to decipher despite the interpretive displays. I think someone must have known what they were looking at to be able to even say what they were, but it was interesting, it got us out of the car and walking (YAY) and killed enough time to let us check in.
Locust? |
Praying Mantis |
Dino foot print -- the long, shallow depression to the right was its tail |
Several footprints, captured in mud |
Tuesday, October 7, 2014
10/7 -- Arkansas and Oklahoma
We started out later than usual, hoping the rain would taper off, but no such luck. It was heavy at times, but cleared, fortunately, before Memphis. Then it was smooth sailing over the Mississippi and into Arkansas. We were surprised at the terrain of the state. It started out kind of swampy at times on the eastern edge and grew more into a flat farming area, reminiscent of Minnesota. After we passed Little Rock and started following the Arkansas River, it changed again into lovely wooded rolling hills and we navigated between the Ouachita and Ozark Mountains.
We also encountered a NASTY traffic jam for 10 miles, right after we re-entered the freeway when we stopped for gas. The road narrowed to one lane for 4 miles, but there was a 6 mile backup as 2 lanes of trucks and cars jockeyed for position. It added 30 minutes to our trip, and kept us from getting past Oklahoma City.
For lunch, we let Liesl (the car's GPS) help us find something and thought the Pudgy Pig BBQ sounded unique. Unfortunately, Liesl's database is a bit out of date because the pig was apparently not sustainable and no longer existed, so we opted for the Waffle House instead. We have seen them all over down here and you will be pleased to know that they serve more than waffles. Lunch options are a bit limited, and make up in volume what they lack in taste. I am still full 6 hours later and I didn't finish everything! Now we can add that to the list of places to avoid, at least for lunch.
Oklahoma has also been beautiful so far -- at least up to Shawnee, where we stopped, about 30 miles out of Oklahoma City. The terrain is like western Arkansas -- rolling hills and lots of trees and greenery, with the occasional oil rig thrown in for good measure. It is also interesting on I-40 to see the litany of Indian tribes that have been relocated here. It seems like we are continually seeing signs identifying which nations we are leaving and entering. I thought it was mostly Cherokee, but we have seen signs for Seminoles, Potawatami, Sac, and Fox so far.
We are well on our way to being a day ahead of schedule getting to Taos, with no hotel room until the 9th, so today we debated our options. One thought was to go to Santa Fe and head up to Taos the next day. Jim read through the AAA Tour Book description and mostly noted the number of churches and museums highlighted to visit (neither is a focus for us) and that the architectural style is locally called "Santa Fake" because the government has decreed that all buildings will look as though they are flat-roofed adobes while allowing actual current building codes to apply. Then I remembered researching National Parks and reading about one called the Capulin Volcano in north-east New Mexico, and that was more outdoor oriented, so it looks like we'll add that to the agenda.
A reservoir along I-40. Looks like they drowned some trees recently. |
Scenic overlook from western Arkansas |
The star of the trip -- the new car (now a year old) and primary driver (who is wondering what I am up to). |
For lunch, we let Liesl (the car's GPS) help us find something and thought the Pudgy Pig BBQ sounded unique. Unfortunately, Liesl's database is a bit out of date because the pig was apparently not sustainable and no longer existed, so we opted for the Waffle House instead. We have seen them all over down here and you will be pleased to know that they serve more than waffles. Lunch options are a bit limited, and make up in volume what they lack in taste. I am still full 6 hours later and I didn't finish everything! Now we can add that to the list of places to avoid, at least for lunch.
I-40 corridor in Oklahoma, this photo and next |
Reservoir along I-40 |
We are well on our way to being a day ahead of schedule getting to Taos, with no hotel room until the 9th, so today we debated our options. One thought was to go to Santa Fe and head up to Taos the next day. Jim read through the AAA Tour Book description and mostly noted the number of churches and museums highlighted to visit (neither is a focus for us) and that the architectural style is locally called "Santa Fake" because the government has decreed that all buildings will look as though they are flat-roofed adobes while allowing actual current building codes to apply. Then I remembered researching National Parks and reading about one called the Capulin Volcano in north-east New Mexico, and that was more outdoor oriented, so it looks like we'll add that to the agenda.
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