Wayland Country Club, on the Sudbury River, courtesy of Google.Glacial vocabulary is seductive and mysterious, at least for the non-geologist. Eskers, moraines, drumlins, kames, pitted outwash plains—none of these terms appear in everyday usage. Even the word “kettle” becomes somehow less homey and more uncanny when it is used to define how ponds come to be formed on a glacial plain. First, an enormous chunk of ice breaks off from a glacier, like an iceberg almost, but stranded without an ocean around it. Then the ice is covered by accumulating sand and gravel until it appears as a hill. Underneath the hill, the ice melts and the sediment collapses into a kettle-like indentation in the landscape. If these kettles have filled with water, we now know them as lakes or ponds.
Walden Pond is a kettle, as are many of the ponds to be found in the Sudbury area. Thoreau tells a story of its naming:
…that anciently the Indians were holding a pow-wow upon a hill here, which rose as high into the heavens as the pond now sinks deep into the earth, and they used much profanity, as the story goes, though this vice is one of which the Indians were never guilty, and while they were thus engaged the hill shook and suddenly sank, and only one old squaw, named Walden, escaped, and from her the pond was named. It has been conjectured that when the hill shook these stones rolled down its side and became the present shore. It is very certain, at any rate, that once there was no pond here, and now there is one… [1]
Such a story, while not to be mistaken for “science” corresponds pretty well with the geological narrative that also explains how “once there was no pond here, and now there is one.” It also asks us to reconsider the prejudices of our own definitions of historical and prehistorical periods, suggesting a capacity for human recollection that reaches back much further than the moment of European contact, to a time when what is now known as Walden Pond was a mountain of sediment-covered ice that melted, if not within the span of one human’s memory than at least within the scope of ritual remembering held within one society’s oral culture.
Oral traditions are not very strong in modern culture. They’ve been crowded out by the isolating distractions of the mass media; a preference for the disjointed “truths” of real-time news-feeds has largely supplanted the kind of local knowledge that is taken in with the senses and passed from person to person, family to family, community to community, in the slower, transformational time of story-telling. But there are other, unspoken and maybe even unconscious ways of remembering and reproducing “what was” in the landscape. A number of country clubs line the Sudbury River, their golf courses a popular attraction for residents and visitors alike. The modern game of golf was invented in Scotland, a land whose topography is also much marked by glacial activity. The geologist Anita Harris has observed that “all over the world, when people make golf courses they are copying glacial landscapes,” sculpting an undulating terrain of greens, fairways, roughs, bunkers, gullies and water features to provide tactical challenges and the pleasures of a distinctively glacial “natural” beauty for the players. [2] Given its own glacial history, it’s perhaps not surprising that golf seems especially at home on the eastern seaboard.
What can we learn by looking at golf courses as ready-made monuments to our glacial past? Maybe it’s precisely the sensation of a past that seems so long ago as to be out of reach (the deep past of geological time) doubling into the familiar, physical shapes of the present ground where we are now standing. Of course, golf courses produce a different sort of “flow” than glaciers. Although their movement across the landscape is not literal, their impact within a watershed can be considerable—the runoff of fertilizers and pesticides from golf greens is an ongoing challenge for river ecology. Seeing golf courses as part of an unwritten history of glaciers perhaps allows us a different way of understanding how our human interventions, their movement and reach, can equally affect the land, their consequences reaching into a more immediate future that may be no less earth-shaking even as it does not afford us the luxury of unfolding over more glacial, geological “eras” and “epochs.” And the shock of realizing the ways in which human time has displaced geological time in the magnitude of its effects may come upon us no less suddenly than it seemed to the cursing “Indians” who felt the “ground” of what would become Walden Pond unexpectedly give way beneath their feet.
“A lot can happen in 1 billion years—supercontinents can collide and then rift apart several times—and mountains the size of the Swiss Alps can form and then erode away. Scientists devised the geologic timescale to help sort out these momentous events.”
James Skehan, Roadside Geology of Massachusetts, 1
[1] Henry David Thoreau, Walden, or a Life in the Woods, (The Ponds), 468.
[2] John McPhee, In Suspect Terrain, 10.
[The Bureau apologizes to its readers for the lapse in time from the last post to this one. It was not quite a billion years, but it may have seemed like it. During February we were called away to complete another experiment in time travel on Lovers Lane in the Presidio of San Francisco National Park. Some documentation from that experiment can be found on the Bureau’s Facebook page, and the original files conveyed by our Field Agent to our home office can be accessed on the Presidio Trust website. We promise to do better in the future, at least at the moments when we find ourselves there.]


