Last August, I disappeared for a much anticipated week of bicycling, camping, and hiking. I hadn’t taken a bicycle trip longer than three nights in far too long, so it felt good to get back on Rocinante and pedal away from home with no phone or internet to distract me. Despite nagging high humidity and some heavy rain during the middle of the trip, it was a blissful time when I disconnected from everything but the immediate world around me (a privilege, yes I realize, but one I’ve worked to maintain).
In total, I didn’t ride my bike all that much. It was about 140 miles, so a reasonable fit person could cover my route in two days—and a younger version of me would’ve felt antsy when taking so much time to cover so little distance, but the point wasn’t to move quickly. Instead, I sought experiences best gathered through careful observation. Each day offered new discoveries, even if they were within the confines of the familiarity that accompanies travel near your home turf. Toward the end of the trip, for example, a day-long hike showcased groves of trees that had experienced a great deal of change, and offered a chance to consider how they might change in the near future.
Starting near Patten on a Friday afternoon, I headed west to the Matagamon Gate at the northeast corner of Baxter State Park where, long story short, I spent the next four nights. After a fifth night of camping closer to the small town of Millinocket and resupplying on food, I made my way north into Katahdin Woods and Waters National Monument.
I spent the remainder of my trip at Esker Camp in the national monument. On my next to last day, I ventured to the top of Deasey Mountain, one of the highest points in the park, on the International Appalachian Trail (IAT). While many hikers see the mountaintop and its historic fire lookout as the highlight, I find myself still thinking of the mountain’s trees.
Maine’s modern history is intertwined with logging. A lot of trees and a lot of water to transport logs and power sawmills made the state ideal for this industry. In the 1800s, Bangor earned a reputation as the lumber capital of the world. Lumberers looked first for the tall, straight-boled white pines that were so valuable for ship masts. When Henry David Thoreau journeyed to the Katahdin region in the late 1850s, he could not find a mature standing white pine. Trees for lumber were the next to go. Then once the paper-making industry arrived, almost every tree more than a foot in diameter at its base was on the market. Harvest rates increased through much of the 1900s until the paper industry began to decline and eventually collapsed in the state.
The timber industry isn’t what it used to be in Maine, but harvesting of trees remains heavy, and anything more than a quick glance on a drive in northern Maine reveals there’s a wide variety in logging strategies depending on the landowner’s wants and the harvest company’s practices. Overall though, most of the forests you’ll see in Maine are relatively young. In a lot of the cuts I’ve visited at random, many trees are harvested at the tender age of 50 years old and sometimes younger. The national monument’s forests are no exception. On satellite images, the landscape is a checkerboard of logging roads, many of which were blazed in the last 60 years to truck out logs.
Deasey Mountain’s modest height (1,942 feet in elevation) and its proximity to Wassataquoik Stream and the East Branch of Penobscot River—major river drive watersheds before road building reached the area’s forests—made its trees a prime target for logging crews. Dozens of dams, including one not far upstream of Esker Camp, were built in the Wassataquoik and East Branch watersheds to facilitate the river drives. Large, human-caused fires had also burned through the area in the late 1800s and early 1900s. With so much recent disturbance I expected to hike through a regenerating forest for most if not the whole way to the summit.
The first task was to ford Wassataquoik Stream at the IAT crossing, which was straightforward due to the river’s knee-deep water that day. After leaving the Wassataquoik’s immediate floodplain the IAT utilized an old road for a brief clip that roughly followed the route used by some of the first Katahdin climbers, then ox teams in early logging efforts, then the heavy equipment of 20th century industrial logging. On the old road north from the Wassataquoik I walked through relatively young, even-aged trees.
But to my surprise, the forest immediately changed after the trail left the old roads. Instead of spindly, closely spaced trees, i was surrounded by groves of large eastern hemlocks with plenty of big sugar maple, white ash, and spruce. Although the views from the mountain summit I experienced later that day were enjoyable, it was this section of forest which most captured my attention and curiosity.
Now, these weren’t the largest trees I’ve ever seen and if you’re used to hiking through the old-growth forests of the Cascades in Washington and Oregon or the Smokies of North Carolina and Tennessee, then I’ll excuse you if you consider these trees to be modest at best. While eastern hemlocks have the potential to live more than 500 hundred years and grow more than 150 feet tall, the natural disturbance regimes in eastern North America coupled with modern logging practices and invasive insects such as hemlock woolly adelgid rarely allow them to reach their maximum age or size.
The pocket of older trees extended along at least a mile of trail. Despite looking, I didn’t find stumps from cut trees or long-abandoned roads or skidder trails, which would have been the obvious signs of harvest in this stand during the last 100 years. I also failed to find charcoaled stumps. By a stroke of luck, this patch of forest did not burn during the large wildfires in the late 1800s and early 1900s. Parts of the Wassataquoik watershed were made near barren after an intense fire in 1903, for example. Short-lived and fast growing trees that fill recently harvested and fire-burned areas such as aspen were also largely absent, which suggests this forest hadn’t seen a major disturbance from an axe, chainsaw, fire, or windstorm in a very long time—at least long enough for the relatively slow growing hemlocks to mature to their current stature.
I would be surprised if this pocket of forest had not experienced at least some harvest in the last 200 years. Before the modern era of roads and feller bunchers (machines that cut, trim, and stack trees), loggers used sluiceways, ox and horse teams, and sometimes Lombard Steam Haulers to transport timber to places where the logs could be left until the river drives of spring thaw. Even the headwaters of the Wassataquoik watershed, now occupying the wildest portions of Baxter State Park, saw intense logging in the late 1800s.
Although I couldn’t find evidence of recent logging and there’s no recorded history of agriculture on the mountain, I suspect this section of forest isn’t old growth, at least not yet. The definition of old growth remains a subject of debate among scientists, yet most seem to agree that old growth forests are complex. Rather than even-aged trees, old growth stands in the northeastern U.S. contain a wide spectrum of tree ages and sizes. Certainly they often contain very large trees but also lots of dead wood. The canopy is complex with trees of different heights and broken tops. If browsing by deer and moose isn’t too intense, the understory is filled with a diversity of shrubs, small trees, and ephemeral herbs.
Other than the large trees, I saw only modest representations of these features on Deasey. Large dead trees, either standing or on the ground, were not common (although there were some thrilling examples of standing dead snags), and the understory was thin in some places. Sometimes this is the result of heavy deer and moose browse, but here I wondered if it was more of the product of the deep shade cast by the hemlocks and spruce. When storms and insects cull the live trees the subsequent gaps flood the forest floor with light, which allows the shade suppressed plants to burst upward.
With much of Katahdin Woods and Waters in stages of early succession after 20th and early 21st century logging and fires, it’ll be many decades before large areas of the national monument’s forests grow into anything that partially resembles the structure they held before industry arrived in the region. Even then, it won’t be the same as before. Ignoring the fact that North America no longer harbors its large Pleistocene mammals which exerted great influence on plants, and the losses associated with Indigenous forestry across most of the landscape, such as burning which maintained open woodlands and prairies, the disturbance regimes now forced on the land in the last 200 years have created novel forest communities. Many forest types we consider “normal” such as stands of near-continually young birch and aspen have no past analogs.
Beyond that, if people never manipulate this forest through harvest or with fire (purposeful or accidental) again we’ve already set into motion a cascade of effects that will influence the forest for many thousands of years. Introduced disease has ravaged Maine’s American beech—a formerly large, long-lived, shade tolerant tree. Hemlock woolly adelgid and emerald ash borer continue to advance and will likely kill most of the ash and hemlock they encounter. Climate change will make the area less hospitable to spruce, balsam fir, and sugar maple while perhaps improving growing conditions for oaks. Species that live farther south currently such as tulip tree and hickories could become new additions to Maine’s forests as annual temperatures rise. High levels of atmospheric CO2 may accelerate tree growth, but at the same time new diseases, new insect infestations, and increased forest fire potential—all fueled by climate change—are likely to be greater threats to these forests than today. Whatever emerges as a result of these influences will be largely a forest of our own making, whether we want it to be that way or not.
Sometimes I wish I could live long enough to experience the distant future, mostly out of curiosity. I wonder if we have the collective foresight and the will to protect what’s left, to ensure that hemlock and ash trees aren’t reduced to functional extinction like the American chestnut. Could I return in 200 years and find hemlocks on Deasey Mountain? In 500 years?
Welcome, dear trees, to the Anthropocene. It might be a rough ride, but I hope we’ll help you get through it.
Some people who know me well poke fun at my penchant for exploring mucky places. At one national park where I worked as a ranger, it took a few years of turnover among the seasonal staff before their friendly prodding about a short lecture I once gave on the differences between bogs, fens, and muskegs died away.
I suppose my fascination with wetlands began on camping trips when I was young (probably no older than eight or nine years). In those good ol’ days of the 1980s my cousins, me, and any temporary campground friends we found spent hours alone exploring a “swamp.” It was little more than a shallow, cattail-filled ditch at the end of one of the state park campground’s cul-de-sacs, but armed with dip nets, fishing nets, and plastic buckets, we pulled more than a few frogs, tadpoles, and crayfish out of it, and sometimes a leech or two off of us.
Although I couldn’t articulate it at the time, I now understand that I was drawn to that place because it seemed so alive. I’ve never outgrown the urge to slog into habitats where I feel like other life forms envelope my whole being. A trial-and-error bushwhack is a small burden to pay so that I can experience that feeling again, which is how I found myself shoving through tangles of spruce and larch last June.
In a broad lowland a few miles south of Patten, Maine lives a most impressive bog. The difficulties I experienced getting into the bog were far surpassed by the beauty one experiences in a rarely trammeled landscape. Crystal Bog is the most spectacular bog I’ve ever seen.
Getting into Crystal Bog (also known as the Thousand-Acre Bog) is not an easy task—a fact I discovered when I first explored it in 2020. No trails enter the bog proper, and the adjacent ATV trails only skirt the extensive swampy thickets that surround it. Choosing the wrong route is easy in such habitat, especially on overcast days when clouds obscure the sun and any hint of which direction might be north or south.
I don’t carry a GPS device or a smart phone, so I navigate via compass when vegetation is too thick and landmarks too obscure to provide orientation. During my attempt to access Crystal Bog in 2020 I rode my bicycle a little too far on the ATV trail that cups the north side of the wetland, started south at the wrong place, didn’t utilize my compass often enough, and bushwhacked much farther than expected or necessary. With those lessons learned, however, I felt better prepared to avoid the thickest muskeg and swampiest areas to reach the open bog more easily.
I locked Rocinante to a sturdy tree once I located a good starting point…
…and set off through the trees.
Crystal Bog is part of a large wetland complex. On every side of it, streams meander through forested swamps and sedge-filled fens. The sphagnum peat lands at the center of this complex was my destination, though.
After 20 minutes of travel (a remarkably short time span compared to the two hours of bushwhacking I needed the previous year), the forest began to transition into a more open woodland. Sphagnum moss and low-growing ericaceous shrubs became common and spindly black spruce and eastern larch were the only trees.
Shortly after, I reached the open expanses of the bog proper.
As I moved from swamp to muskeg to sphagnum bog, I moved progressively into harsher habitats, at least from a botanical perspective.
Bogs are a type of peat-land that generally get water from aerial precipitation rather than flowing surface or ground water. Sphagnum thrives here. The tannins and acids released by sphagnum lower soil pH to levels inhospitable for most plants. While a bog’s edges might be richer in minerals and productivity due to ground or surface water flow, the sphagnum-dominated areas in and around its center offer very different conditions. The pH at Orono Bog near Bangor, for example, progresses from 6.6 (a pH you find in milk) at the forested edge to 3.8 (a pH approaching that of grapefruit juice) at its sphagnum-dominated center. Since the pH scale is logarithmic, rather than linear, this difference represents almost a 1,000-fold change in acidity.
As more sphagnum grows on the surface, it buries and compacts previous generations to form peat. Decomposition is also hindered by the low oxygen conditions found in the bog’s supersaturated soils. But, sphagnum is really good at growing on top of itself. In this manner, sphagnum begets sphagnum. Under the right climatic conditions, sphagnum bogs can sustain themselves for thousands of years and peat accumulations can grow many meters thick. Peat also preserves a botanical record of the plants that lived in the bog and the pollen that settled on it, a paleontological record on present and extinct animals that died within them, and even an archeological record of the people who utilized these places.
On top of this wealth of partial decay exists a living veneer. Minute gradations in topography and drainage create micro-habitats for the plants that are adapted to the bog’s stressful conditions. The higher above the bog’s water table, the more oxygen can diffuse into the soil and the more O2 is available for plant roots that need oxygen. Relatively few plant species survive in bogs compared to nearby forests. Yet those that do are often abundant.
Larch and black spruce in bogs receive ample sunlight, have access to plenty of water, and experience little competition from other tall plants, but the peat enveloping their root systems offers little to sustain their growth. Small-statured trees in a bog may be many decades old, while growing little more than the height of an average adult person. At the Orono Bog, some 7-foot tall spruce trees were found to be about 100 years old. (FWIW a tree, I think, cares not for its appearance, only its ability to reproduce.)
These small-statured black spruce (Picea mariana) may be many decades old.
Ericaecous shrubs such as Labrador tea, bog rosemary, and laurels survive in bogs only where their shallow roots remain perched above the flooded peats and sphagnum. Yet, although bogs are classified as wetlands, summertime drought can cause drastic lowering of the water table. The thick, leathery leaves of these plants might help them retain moisture under those conditions.
Labrador tea (Rhododendron groenlandicum)
Sheep laurel (Kalmia angustifolia)
Orchids tap mycorrhizal fungi to overcome the lack of nutrients, a trick utilized by the ericaceous plants as well.
Grass pink (Calopogon tuberosus)
Other bog plants evolved means to capture nutrients from animals. Bladderworts capture prey in small sacs attached to their thread-like underwater leaves. When a tiny zooplankton contacts sensitive hairs on the outside of the bladder, it triggers the bladder to inflate. The sudden action sucks in water and the hapless prey. The plant then absorbs its nutrients.
Bladderwort (Utricularia sp.)
Sundews ensnare small insects using sticky secretions on the ends of glandular hairs on their leaves. An insect alights on the leaf and becomes stuck. The hairs and the leaf margins then slowly fold over and envelope the insect. The leaf hairs also release an anesthetic to stupefy the prey as well as enzymes to dissolve its soft tissues.
Round-leaved sundew (Drosera rotundifolia). An unlucky insect is trapped on the leaf in the right photo.
Pitcher plants use specialized leaves to create a basin of water. Insects that fall into the basin, aided by downward pointing hairs on the inside of the leaf’s rim and numbing secretions, are slowly decomposed by bacteria and possibly plant enzymes that live in the water. Specialized cells at the bottom of the pitcher absorb the insects nitrogen and other nutrients.
Pitcher plant (Sarracenia purpurea)
I paused often as I wandered through the bog to marvel at the tenacity and beauty of the life around me. I also marveled at the lack of a human presence. The ability to experience a landscape that wasn’t overtly altered by people was a special treat, even in one of the least populated U.S. states.
Maine is lushly vegetated. Forest covers a greater percentage of its land than any other state. That forest, though, is heavily manipulated by people—by a timber industry that often harvests trees before they reach age 50, by a warming climate, by tens of thousands of miles of roads, and by invasive species. But human-caused changes are not limited to the land. Off the coast, the Gulf of Maine is one of the fastest warming bodies of water in the world. There is virtually no Atlantic cod fishery because cod haven’t recovered from the devastation of overfishing in the 20th century. Ditto for Atlantic salmon, which hang on by a thread. Places where evidence of humanity’s heavy hand is absent or at least minimized are difficult to find even in parks such as Acadia, Baxter, and Katahdin Woods and Waters.
Bogs are often overlooked at best or viewed as wastelands to be “reclaimed” for agriculture or mined for peat at worst, but they rank among the worlds most important habitats, especially when we consider their ability to capture and sequester atmospheric carbon. Like old-growth forests, peat is a non-renewable resource since we humans lack the patience and self-restraint to harvest it at sustainable levels (please buy peat-free soil products for this reason).
While the area surrounding Crystal Bog is full of roads, early successional timberland, potato fields, homes, and small towns, this bog remains remarkably unmarred. It is one of the few places in modern day Maine that would be recognizable to a Wabanaki traveler from the 15th century. In the middle of Crystal Bog, it’s easy to let your mind drift to a place where the world is well. This is an illusion, I realize, but one we all must escape into every once in a while.