Tag: North American Coastal Plain

Deep History

Prairie Erth by William Least Heat-Moon. Houghton-Mifflin Co. 1991.

This book is deep history of a single locality, Chase County Kansas, a thinly populated, largely rural part of the Flint Hills and the great North American grasslands. The book’s coverage extends far into the geologic past and up to the early 1990s. By then, as in much of rural America a peak of population and development had been passed, and its farms, ranches, villages and towns were becoming depopulated. Heat-Moon spent many months driving and walking about the county, systematically taking up one by one the grid of USGS topographic maps (twelve central ones and thirteen more that cover the edges) that include Chase County. He talked with a great many of the residents and others with connections to the land, the people and the history. He also read extensively, prefacing each of the twelve sections (one for each central topo map) with a series of excerpts from his commonplace book, relating to the themes he follows in that section. The quotations come from hundreds of books, newspapers, journals.

Geology, botany, zoology occupy almost as much of the six hundred pages as the people. A Native American himself, he devotes much space to the aboriginal people, the Kaw, also sometimes called the Kansa (among a host of other names that he cites) By the time he wrote, the few remaining members of that tribe resided on Oklahoma, to which they had been “removed” in the 1870s.

Summarizing this remarkable work of observation, listening and reflection is not possible. I was deeply impressed both by how fascinating a seemingly backwater place can be and by how deeply Heat-Moon engaged with the land and people. Despite often being seen as an eccentric outsider, he showed great respect for the locals and was able to win the confidence of many. His self reflections are often profound and often extremely amusing. The best travel writers often are like that: I think of Bill Bryson.

What I realized reading Prairie Erth was how much I am interested in the deep history of the places I have lived. I think that’s why I am captivated by books that lay out the events that shaped the landscapes I am most familiar with. If you have seen my earlier posts, New World History, Forgotten but not Gone, Ecosystem Lost and Found?, The Journeys of Holling C. Holling, and even Amphibious Reflections, you will have encountered my interest.

I live in the Pine Barrens region of southern New Jersey, on land once part of Gloucester Plantation, which was centered on Gloucester Furnace, an iron foundry. It can be fairly said that the Pine Barrens were one of the industrial centers of the early United States, although now, many people describe them as a “pristine wilderness.” This sort of blindness to the past seems endemic among us, as amply demonstrated in Forgotten Grasslands of the South and Looking for Longleaf.

Fortunately, there have always been some more inquiring minds, who have sought out the past and tried to preserve or at least document it. For my area, there are many books, like Forgotten Towns of Southern New Jersey, that record these past landscapes and communities. Many individuals like Jean Soderland, are researching the history of indigenous people. There is now a periodical devoted to all aspects of the regions history, SoJourn.

I have had at least five colleagues who dedicated their research to understanding the geological and cultural history of the region: a hydrologist, a geographer, a historian, an archaeologist and a geologist. The geologist started out in horticulture, but became so interested in the natural landscapes of the Pine Barrens that he took a PhD in geology to further his collaborations with a noted glacial geologist. He has contributed greatly to our knowledge of the ways that the Ice Ages shaped the topography of the Pine Barrens and indeed the entire North American coastal plain.

The North American Coastal Plain consists of marine of riverine sands and gravels accumulated on the edge of the ocean. From these soils develop that drain rapidly and are prone to severe drought. Fire has been a force in the landscape for millions of years, varying in frequency and intensity with climate and, since a few thousand years ago, with human activity. Groundwater saturates these porous sediments, often nearly to or above the surface. Upland vegetation historically burned often, the extensive lowlands only in severe droughts. 

 The ice age climate was dry, cold and ferociously windy as frigid air flowed off the ice sheets only a short way north. The landscape that developed as the climate warmed included wide but very shallow river channels, with streams too small for their valleys. These were created by melting permafrost. There are numerous shallow ponds in depressions, some nearly circular, created by powerful winds during full glacial periods, others long, winding and narrow, created by blowing sand blocking stream courses. Low, sandy ridges are the remains of ancient fields of dunes created by the same winds that blew out the depressions. 

Early European settlers cut the trees, dammed the streams and began creating mills, cranberry bogs and crop fields. They started many iron plantations in the late eighteenth to early nineteenth centuries, utilizing the local bog iron, the pine forests (for charcoal) and the shell maddens left by the aboriginal inhabitants, the Lenape, to produce iron. As iron industry moved west, paper and glassmaking took over the old water powered mill sites.

Today, the former Gloucester Plantation tract has been through several phases of settlement and resettlement. The land was promoted in a real estate endeavor that became Egg Harbor City. A town was laid out, at first facing Landing Creek and the Mullica River, then reoriented to the railroad that was built in the 1850s from Philadelphia to Atlantic City. The hinterlands were sold as farms, mainly to German-speaking immigrants, most of whom left eastern cities to escape the anti-immigrant Know-nothings (see Before the Storm and Politics and War) Egg Harbor City thrived as an agricultural and small manufacturing town and then gradually faded until the advent of the FAA Technical Center, Stockton College (now University) and the Atlantic City Casinos. These brought in new residents, but not much new commerce, which developed mostly in the central and eastern parts of Atlantic County. The establishment of the Pinelands National Reserve in 1979 restricted commercial and industrial development and even residential development over much of the Gloucester tract.

 Farming continues, mainly commercial blueberries (a crop developed in the Pine Barrens) and, more recently, community supported agriculture. Much of the land, however, reverted to forest. Not the open woodlands of the years before fire suppression became the policy in New Jersey, but dense, closed canopy oak and pine forests, with thick understory of huckleberries. This lowered the groundwater table, drying up ponds and headwater streams. It also caused the native herbaceous plants to become much less frequent and with them their associated insects, especially butterflies and moths. Many are now only found in a few well managed preserves and, ironically, in utility line corridors and airports, which are kept open by mowing in the dormant season.  

The region’s roadsides, once a haven for native herbs, have been converted by mowing and addition of cool season grass, to monotonous and sterile strips. Unpaved roads, trails and open areas are now the domain of off-road vehicle enthusiasts, who flood the Pine Barrens on weekends, destroying habitat. The worst are the “mudders,” who have wiped out hundreds of localities for rare and endangered wetland plants. Species not native to the Pine Barrens are increasingly taking over, especially on recently abandoned cleared land. I am in continual struggle with autumn olive, multiflora rose, Asian barberry, and Eurasian bittersweet.

I pin my hopes on the position of the New Jersey Coastal Plain as the northernmost (excepting Long Island and Cape Cod) part of the great North American Coastal Plain biodiversity hotspot.  As climate change pushes populations northward and sea level rise shrinks the Coastal Plain, southern New Jersey may be a critical refuge for southern species. But who can tell? It could just as well succumb to rampant deregulation and competing interests, like the infernal off-roaders. 

Change over millions of years shaped the landscape and the evolution of the Pine Barrens’ characteristic flora and fauna. I tried to impress this on my students in the years I taught ecology. The processes that operate in the lithosphere, hydrosphere, atmosphere and biosphere – energy flow, nutrient cycling, population dynamics, evolution and cultural change – shape what we see around us. And every development leaves traces on the land and in the living organisms that inhabit it. Without an understanding of the history of the place you are in, you cannot understand its present or future.

Ecosystem lost and found?

Looking for Longleaf. The Fall and Rise of an American Forest by Lawrence S. Earley (2004) Chapel Hill. University of North Carolina Press. 322pp.

When I was a teenager, my grandfather recalled for me how the longleaf pine forests in eastern North Carolina looked when he was young, some seventy to eighty years before. It was like being in a cathedral, he said, with the trunks of the trees like columns and the forest floor clear as far as you could see. This book gives an introduction to the character and extent of the longleaf pine ecosystem, once dominant over a vast region of the Atlantic and Gulf Coastal Plain, introducing the plant, Pinus palustris, the diversity of associated plants (sometimes hundreds of species in a square kilometer and as many as 40-60 in a square meter) and several of the more distinctive animals, like gopher tortoise and red-cockaded woodpecker.

Earley explains the critical role of fire and soil in establishing the diversity of types within the overall longleaf ecosystem.

The middle part of the book is a historical account of the European encounter with the forest, its exploitation by the naval stores industry and its eventual destruction by that industry and the railroad based loggers. Some of these descriptions fit closely with what I heard from my grandfather and from a friend in North Carolina (whom Earley interviewed for the section on turpentining). He talks about rafting logs down the coastal rivers (as my grandfather, born in 1869, did as a boy) and shipping naval stores (my grandfather also described how the cooper made the barrels for turpentine). He explains that what preserved so much of the forest were the limitation of cutting timber to areas close to usable streams, that is until the railroads came. My father (born 1913) recalled how the railroad was brought in to log some of the most remore and inaccessible places when he was growing up. Some time around 1970, before the railroad was finally abandoned, I saw carloads of longleaf pine stumps waiting to be hauled off to extract the valuable resins or to make fatwood kindling, sold by L.L. Bean, among others. Earley also mentions the continued interest in salvaging sunken logs and getting lumber from old buildings.

The final chapters are on the development of forest management ideas, from failed attempts at replanting to replacement by loblolly and slash pine and the gradual development of methods to regenerate longleaf, first as even aged stands but now moving towards uneven age management and overall ecosystem restoration. Red-cockaded woodpecker played a key role in several changes in policy, driven by court decisions under the Endangered Species Act. Many of the agencies involved, like the US forest Service have serious problems dealing with the steady increase in scientific and ecological understanding of the forests. Institutional change is difficult, especially when institutional memory is impaired by frequent reassignment of key people and political pressures. The US Forest Service has had an especially hard time admitting it has been wrong about fire suppression and even-aged management.

He talks about the role of national and state forests and of large and small private landholders (currently there is increasing longleaf acgeage on federal and maybe state land and on large private conservation holdings, but continued losses on timber company lands and small private holdings) and what the trends may mean for the future of the ecosystem and many of its species. New incentives under the Conservation Reserve Program may be changing the minds of some private owners. It is possible to derive a pretty steady income from restored longleaf, partly through sale of raked needles in the 10th to 15th years after replanting. Poles are much in demand, using middle aged trees. The author seems most impressed by adaptive management approaches using small group-selection cuts and frequent growing season fire. Several interesting examples are described in the next to last chapter on restoration. Some of these areas sound like they would be worth seeing, and there are some groups that can help with restoration, a topic that is on my mind lately, as I and my brothers and sisters still hold a small remnant of thousands of acres of longleaf land owned by my great-great grandfather in the early 1800s. We will soon be clearing the stand of loblolly pine, planted decades ago, to make way for longleaf again.