cathy, without a plan...
You probably need a sense of humor and a certain playful attitude toward life and the world around us to appreciate my blog. If you lack either of these, perhaps you can download them from the internet. If you've been here, I'd love to know - please leave me a 'comment.'
Wednesday, April 20, 2011
Sunday, April 17, 2011
Friday, April 15, 2011
Geology
On our tour of Utah's National Parks...
By the time we got to Capital Reef, we were thinking about Geology: About the 'layer cake' of rock we were walking on, miles thick, made up of sandstone, mudstone, shale, salts, and limestone, all 'icing-ed' over each other in their respective ages - as the area was at times under an inland sea collecting the detritus of the coral reefs; part of a wind-blown desert where there were dunes of sand ultimately compressed into rock; or covered by river floodplains (dinosaurs and giant trees!) now seen as shale. There is gypsum, quartz and clay. Where did it all come from - and when? The timescale is staggering, as is the contemplation of what has been laid down under our feet over the millennia. And it’s all been carved up and exposed in irregular cuts from erosion, leaving behind spectacular cliffs and hoodoos.
Our Park notes indicate the exposed formation to be from the middle Jurassic Period (180 million years ago) to the Cretaceous Period (95 million years ago.) The Carmel Formation - oldest - has layers of gypsum which forms white striations in the red colored cliffs. Just above is the Entrada - formed from deposits laid down during the mid-to-late Jurassic Period and mostly fine-grained sandstone.
We know that rock layers (strata) are laid down in succession over time. Geologic time is identified in a complex system of categories that labels those layers... Evidently we are now in the Cenozoic Era and the Quaternary Period and the Holocene Epoch (with no "age" yet designated as far as my limited research indicated before I got bored with the whole subject.)
Perhaps you know already where all this Geology talk is going. Being us, we just HAD to start speculation about what is being 'laid down' in modern times and what future Geologists will make of it.
Mark designated it the "Cretinous" age and predicted its strata to be full of plastic water bottles, disposable diapers, petrified pizza boxes and Diet Coke cans.
Stunned by Bryce Canyon
Yes, Bryce was amazing. And it isn't too much to say we were stunned. And we've been here before! But walking down into the maze of hoodoos - sort of a stalagtite outside of a cave - and seeing the complex shapes and colors and heights of these formations was thrilling. Mark called it his favorite... but I'm reserving judgement until I look at some more pictures of the rest of the parks. Just sorting out some 'representative' pictures of Bryce was hard enough! Anyway, here's what I have to say about Bryce:
Wednesday, April 13, 2011
Tucson etc.
Tuesday, April 12, 2011
Zion (2)
Monday, April 11, 2011
Zion National Park (1)
Sunday, April 10, 2011
And we're back
I looked at my last posting, 'before vacation,' and thought again about what an odd thing time is. On paper - or computer screen, in this case - there is just a half inch between the last blog post and this one - yet so much has gone on in between. We drove another 3,000+ miles, visited with family and friends, saw incredibly diverse sights, got snowed on, got sunburned, and took, literally, thousands of pictures... and here we are again, home, writing a blog post that is only a half inch above the last one. College basketball is over - Arizona didn't win again - and baseball has started - the Mariners aren't winning again either - but it is still winter here and tomorrow we have to go back to work.
We had a wonderful trip - with really bad weather on the days we were driving and really good weather on the days we were sightseeing and hiking. In one place the snow was so deep that we were unable to access a trail we'd been hoping to hike, and in another place we dashed from shade to shade with our water bottles at the ready to keep from heat stroke. And we realized, once again, that it is hard for sea-level dwellers to hike at 5-8,000 foot levels. ("That's our excuse and we're sticking to it," is what we say to all you skinny folks who are smirking at this comment, knowing us...)
It's going to take me a while to process all the photos. We took both cameras and we both enjoyed taking pictures, right next to each other. It turns out that Mark's philosophy of photo-shooting is similar to his attitude toward target shooting: point and shoot, and do it a lot. Where one click might do, 3 or 4 are surely better. And having been to 4 national parks (Zion, Bryce, Capital Reef and Arches,) a national monument (Tumacacori,) the Desert Museum, Tombstone and all the 'scenic views' in between, that was a lot of 'shooting.'
There was a lot of people-watching too - something you can't really avoid while out and about to that extent. I'm afraid it is mostly our habit to notice the negative behaviors rather than the positive, but, that aside,we were surprised at the number of times people approached us to ask if we would take their picture in front of the scenery. They invariably offered to return the favor by taking our picture too...
And there we run into a little trouble. We have NO pictures of ourselves, together, on this wonderful vacation. The first time someone offered to take our picture Mark's gut reaction was to say "thanks, but every time someone takes our picture, two fat, old people show up in the developed shot and we are tired of wondering where they came from." We stuck to THAT story too. And now I wish we hadn't.
So. I will post pictures, but none of us. It will take forever for me to sort them out but I'll enjoy every minute of it, and after all, it IS still winter here.
We are finally in the big league. Other people are 'frequent flyers' or 'high rollers' or 'preferred customers.' We are, evidently 'elite' as well. Kings, as it were, at the grocery store. Woe to them the next time they are out of my brand of peanut butter.
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