Dakota Datebook

Steinbeck

Saturday, November 8, 2003

In the fall of 1960, celebrated novelist, John Steinbeck, along with his poodle, Charley, toured the country in a camper called Rociante and recorded his experiences in his book, Travels with Charley. Today, we begin a 2-part series on his experiences while in North Dakota.

If there had been room in Rocinante I would have packed the W.P.A. Guides to the States, all forty-eight volumes of them… I would have looked up Detroit Lakes, MN, where I stopped, and would have known why it is called Detroit Lakes, who named it, when, and why. I stopped near there late at night and so did Charley, and I don’t know any more about it than he does.

The next day a long-cultivated ambition was to blossom and fruit. Curious how a place unvisited can take such hold on the mind so that the very name sets up a ringing. To me such a place was Fargo, North Dakota. Perhaps its first impact is in the name Wells-Fargo, but my interest certainly goes beyond that. If you will take a map of the United States and fold it in the middle, eastern edge against western, and crease it sharply, right in the crease will be Fargo. On double-page maps sometimes Fargo gets lost in the binding. That may not be a very scientific method for finding the east-west middle of the country, but it will do.

But beyond this, Fargo to me is brother to the fabulous places of the earth, kin to those magically remote spots mentioned by Herodutus and Marco Polo and Mandeville. From my earliest memory, if it was a cold day, Fargo was the coldest place on the continent. If heat was the subject, then at that time the papers listed Fargo as hotter than anyplace else, or wetter or drier, or deeper in snow. That’s my impression, anyway.

But I know that a dozen or half a hundred towns will rise up in injured wrath to denounce me with claims and figures for having much more dreadful weather than Fargo. I apologize to them in advance. As…I passed through Moorhead, Minnesota, and rattled across the Red River into Fargo on the other side, it was a golden autumn day, the town as traffic-troubled, as neon-plastered, as cluttered and milling with activity as any other up-and-coming town of forty-six thousand souls. The countryside was no different from Minnesota over the river.

I drove through the town as usual, seeing little but the truck ahead of me and the Thunderbird in my rear-view mirror. It’s bad to have one’s myth shaken up like that. Would Samarkand or Cathay or Cipango have suffered the same fate if visited?

As soon as I had cleared the outskirts, the broken-metal-and-glass outer ring, and moved through Mapleton I found a pleasant place to stop on the Maple River not far from Alice – what a wonderful name for a town, Alice. It had 162 inhabitants in 1950 and 124 at the last census – and so much for the population explosion at Alice.

Anyway, on the Maple River I drew into a little copse, of sycamore I think, that overhung the stream, and paused to lick my mythological wounds. And I found with joy that the fact of Fargo had in no way disturbed my mind’s picture of it. I could still think of Fargo as I always had – blizzard-driven, heat-blasted, dust-raddled. I am happy to report that in the war between reality and romance, reality is not the stronger.

Stay tuned tomorrow as Steinbeck gets his first look at the Badlands.

SourceURL:file://localhost/Users/moffutt/Desktop/DAKOTA%20DATEBOOKS%20BY%20SUBJECT.doc

Crater

October 10

Yesterday, we talked about a five-foot meteorite that landed near Carrington in 1910. But about 214 million years ago, a meteorite that landed in what is now McKenzie County was so large that it left a crater 5 miles across.

Many people confuse meteors with shooting stars. Generally, a shooting star is the size of a grain of sand. A meteor, on the other hand, is large enough to survive its fiery trip through the atmosphere to reach the earth’s surface – at which point it becomes a meteorite. Meteors of this size are often asteroids or comets or fragments from a comet’s tail.

The Red Wing Creek crater near Williston is believed by many scientists to be connected to a group of at least five massive comet fragments that bombarded the earth within hours of each other during the Triassic Period about 240 millions years ago.

The largest crater formed by these collisions – the Manicouagan in Quebec – is 62 miles across. The remaining three of the group are in Manitoba, France and the Ukraine. The craters are located very far apart from each other, but at the time of impact, the planet’s continents were still primarily one land mass, and the five locations were very close together.

When large meteors like these collide with the earth, the damage can be spectacular. Shock waves roll over the earth’s surface, through its fragile crust and into its mantel & core. Trillions of tons of debris can be sent into the atmosphere.

Dust and debris from cosmic collisions and explosions can remain in the atmosphere for months and sometimes even years. Around the year 535 AD, Earth was wrapped in a swarm of atmospheric debris that produced two years of continuous winter. It’s believed that this vast dust cloud came from either outer space or from a massive volcanic eruption somewhere on the globe.

During those two years, it snowed in the winter, drought-stricken areas had constant flooding, crops failed, and famine decimated Italy, China and the Middle East. A 6th-century Syrian bishop wrote, “The sun became dark… Each day it shone for about four hours and still this light was only a feeble shadow.” This event marked the beginning of… the Dark Ages.

When the Red Wing Creek grouping landed, the impact of comet fragments was nothing short of catastrophic. In fact, it’s believed that these collisions caused history’s 3rd largest mass extinction, affecting approximately 80% of the planet’s species and bringing the Triassic Period to a close.

Many millions of years later, a massive meteor hit Mexico, forming a crater more than 100 miles across. This one is believed to have caused the mass extinction of the dinosaurs at the end of the Cretaceous Period.

Despite the fact that North Dakota’s Red Wing Crater is more than five miles across, it unfortunately has filled in over the millennia and can’t be seen from either land or air. Unlike craters formed by volcanoes that leave a rim above ground level, the Red Wing Crater, as well as another smaller on in Renville County called the Newporte, are both below ground and were accidental discoveries recently made by oil drillers.

Dakota Datebook written by Merry Helm

This text and audio may not be copied without securing prior permission from Prairie Public.

Dakota Datebook is a project of Prairie Public, in partnership with the State Historical Society of North Dakota, with funding from the North Dakota Humanities Council.

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