‘A Continuity Of Place And Blood” (December 1977 | Volume: 29, Issue: 1)

‘A Continuity Of Place And Blood”

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Authors: C. W. Gusewelle

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December 1977 | Volume 29, Issue 1

Sometime in the sleep of every year, between the browning of the oaks and the first greening of the spring wild grasses, that country flamed.

The rainless days would laze on in powdery file. The thin earth of hillside clearings turned to the plow would pale from brown to gray, and then begin to ride up on the wind. There was beauty in such days-a sense of reach and distance. But the rattle of dry leaves in doorway wood lots just at evening was terrible to hear, and anyone who neighbored with the timber did well, before retiring, to mark which quarter the wind blew from, and how strongly, and what it smelled of.

For when the fire burst finally up out of the creek bottoms and across the ridges, it came with a suddenness never quite remembered. Driving everything before it-deer, blind-flying birds, pigs gone feral in the greenbriar thickets, sometimes the people themselves. Raging barn-high up the dark flanks of the hills, turning rank meadows into white-hot lakes.

Men did not stop such a fire. And in absolute, admitted truth they did not care to stop it. The fire, they said, killed ticks, cleared the brushy undergrowth, and made spring grazing in the unfenced timber. And no matter that the ticks had been just as numerous and a man’s cattle as spare through all the remembered wildfires of a lifetime, this much was known and repeated like a catechism: the burning-off killed ticks, made pasture.

All across that country, long after the burning, could be found the remains of tortoises that the fire had overtaken on their way to somewhere. The olive, outer skin of the shells had peeled down to chalk-white empty helmets, wonderfully complicated in their jointing, that fell away in clicking segments when they were touched with the toe of a shoe. It was sad to find them so, pointing not away from the direction the fire had come, as might be thought, but toward their forgotten destinations.

Spring rains flushed off the ash, and the topsoil with it, into streams running milky gray out of their banks. The first fine grass came, then bird’s-foot violets. The healing seemed unfailing, the nearest thing to a miracle that could be claimed in those raw hills. But it was never complete. Always the ground was a little poorer, the game a little scarcer.

It is proper for lowland rivers to meander. But the streams of the Ozark highlands bend and recurve upon themselves in a way that upland rivers are not supposed to do.

Some 320,000,000 years ago, the seas that once covered much of this continent’s interior receded, leaving behind their heavy sedimentation of sandstone, shale, dolomite, and limestone, leaving also a network of estuarial rivers that wound tepidly through the emergent fern forests, sheltering the amphibians and watering the newer things that crept.

Over the next 100,000,000 years the humid forests flourished in the luxuriance of growth and the slow, slow burn