Free Appointment in Samarra by John O'Hara Page B

I can’t break,” said Al, who had no date. “I had a sort of a date, but it can wait if you want me to do anything.”
    “Well, I hate to ask you, but this is what I want you should do. Drive up to the Stage Coach and stay there till they close up and keep an eye on things, see what I mean? And tell Helene I’ll be there if I can make it, but you stay there anyhow, will you kid? There’s fifty bucks in it for you on account of lousing up your date. Okay?”
    “Kay,” said Al. “Only too glad, Ed.”
    “Okay,” said Ed. “Just stick around and keep an eye on everything.” He hung up.
    Al knew what he meant. Helene was not a teetotaler by any means. In fact Ed encouraged her to drink. She was more fun when she drank. But she was liable to get drunk tonight, because it was Christmas, and Ed didn’t want her to become reckless with the spirit of giving.

3
    Anyone in Gibbsville who had any important money made it in coal; anthracite. Gibbsville people, when they went away, always had trouble explaining where they lived. They would say: “I live in the coal regions,” and people would say, “Oh, yes, near Pittsburgh.” Then Gibbsvillians would have to go into detail. People outside of Pennsylvania do not know that there is all the difference in the world between the two kinds of coal, and in the conditions under which anthracite and bituminous are mined. The anthracite region lies roughly between Scranton on the north and Gibbsville on the south. In fact Point Mountain, upon which Gibbsville’s earliest settlement was made, is the delight of geologists, who come from as far away as Germany to examine Gibbsville Conglomerate, a stone formation found nowhere else in the world. When that geological squeeze, or whatever it was that produced veins of coal, occurred, it did not go south of Point Mountain, and coal is found on the north slope of Point Mountain, but not on the south side, and at the eastern face of Point Mountain is found Gibbsville Conglomerate. The richest veins of anthracite in the world are within a thirty-mile sector from Gibbsville, and when those veins are being worked, Gibbsville prospers. When the mines are idle, Gibbsville puts on a long face and begins to think in terms of soup kitchens.
    The anthracite region, unlike the bituminous, is a stronghold of union labor. The United Mine Workers of America is the strongest single force in the anthracite region, and under it the anthracite miner lives a civilized life compared with that of the miner in the soft coal regions about Pittsburgh, WestVirginia, and the western states. The “coal and iron” police in the anthracite region have been so unimportant since the unionization of the mines that they seldom are mentioned. A candidate for governor of Pennsylvania cannot be elected without the support of the U.M.W.A., and the Pennsylvania State Police never are called “black cossacks” in the anthracite region. A candidate for any political office in the anthracite counties would not think of having anything printed without getting the typesetters’ union label on his cards and billboards. The union is responsible for the Pennsylvania mining laws, which are the best in the world (although not yet the best there could be), and labor conditions, so far as labor strife was concerned, were all right in 1930, and had been all right since the disastrous strike of 1925. At that time the union called a strike which lasted 110 days, the longest strike in anthracite history. There was no violence beyond the small squabble, and there was no starvation among the miners. But anthracite markets disappeared. Domestic sales were hurt permanently; the oil burner was installed in thousands of homes. Anthracite is practically smokeless, and was satisfactory to home owners, but they could not get anthracite during the strike, and when the oil burner was installed there was no point in going back to coal. And so, as a result of the 1925 strike, the anthracite