Old Forest in Franconia Notch State Park - New Hampshire Division ...
Old Forest in Franconia Notch State Park - New Hampshire Division ...
Old Forest in Franconia Notch State Park - New Hampshire Division ...
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DIRECTIONS<strong>Franconia</strong> <strong>Notch</strong> <strong>Park</strong>way (a part of I-93)runs through <strong>Franconia</strong> <strong>Notch</strong> <strong>in</strong> the WhiteMtns. A paved bike path parallels the parkway.The park<strong>in</strong>g lots for the portion of thebike path described here are both on thesouthbound (west) side of the parkway. Forthis guide, follow the bike path north tosouth between Lafayette Campground andThe Bas<strong>in</strong>.NH DIVISION OF PARKS & RECREATIONThe mission of the NH <strong>Division</strong> of <strong>Park</strong>s and Recreation(www.nhparks.state.nh.us) is to protect and preserve recreation,historic, scenic and natural areas of the state, to cont<strong>in</strong>uallyprovide such additional park areas and facilities, to makethese accessible to the public for recreational, educational,scientific and other uses consistent with their protection andpreservation, and to encourage and support tourism and relatedeconomic activities with<strong>in</strong> the state.FRANCONIA NOTCH STATE PARK<strong>Franconia</strong> <strong>Notch</strong> <strong>State</strong> <strong>Park</strong> is located <strong>in</strong> the heart of thepopular White Mounta<strong>in</strong> region. The notch is a dramaticmounta<strong>in</strong> pass traversed by a unique parkway that extendsfor 8 miles between the high peaks of the K<strong>in</strong>sman and <strong>Franconia</strong>mounta<strong>in</strong> ranges, from the scenic Flume Gorge <strong>in</strong> thesouth end to Echo Lake at the north end. It conta<strong>in</strong>s the headwatersof the Pemigewasset River, the massive Cannon Cliffs(the largest cliff <strong>in</strong> northeastern U.S.), a great diversity offorests and alp<strong>in</strong>e tundra, and several other spectacular naturalfeatures.PARK USE GUIDELINESThis park is open to the public for recreation and education.Please, for the protection of the area and its <strong>in</strong>habitants, andfor everyone’s enjoyment, follow these rules:• BIKE PATH IS FOR MULTIPLE-USE. PLEASESHARE WITH CARE.• NO MOTORIZED WHEELED VEHICLES ON BIKEPATH OR TRAILS.• NO PETS ALLOWED.• CARRY OUT ALL TRASH.• NO CAMPING OR OPEN FIRES ALLOWED EX-CEPT IN THE CAMPGROUND.• PRACTICE LOW-IMPACT RECREATION. PLEASEDON’T PICK PLANTS OR FLOWERS.Note: As the bike path is heavily used, extra care must betaken when us<strong>in</strong>g this guide. Some bikers are rid<strong>in</strong>g fast.Please be alert and considerate of other users.OLD FOREST IN FRANCONIA NOTCH<strong>Old</strong> forests that have not been logged are rare throughoutNorth America. They are characterized by large, old trees,lots of dead and downed wood, and rich biological legaciesnot found <strong>in</strong> heavily managed forests. There are patches ofsuch uncut old forest <strong>in</strong> and around <strong>Franconia</strong> <strong>Notch</strong>. Althoughthe history of cutt<strong>in</strong>g throughout the notch is notprecisely known, we do know that there are remnants of oldforest such as the spruce-fir-northern hardwood forest alongthe bike path. This area is a good example of what a maturenorthern hardwood forest looks like. Some of the trees hereexceed 250 years of age.This forest has been impacted by several hurricanes and frequentw<strong>in</strong>ter storms. With such fierce weather, the notch is aharsh environment to grow <strong>in</strong>, and the architecture of theolder trees reflects it. Hardwood species such as yellowbirch, beech, and sugar maple typically have a dense scraggleof contorted branches at the top of thick, straight trunks thatare anchored by large root structures. The irregular canopy ofthis forest is a result of many years of limbs be<strong>in</strong>g snappedand broken off by strong w<strong>in</strong>ds, heavy ice, and deep snow.Softwoods like red spruce readily shed ice and snow, andolder specimens can frequently be seen emerg<strong>in</strong>g above thehardwood canopy.Of course, old forests consist of much more than just oldtrees. In fact, the old trees are fairly widely scattered andmixed <strong>in</strong> with younger trees and sapl<strong>in</strong>gs of various agesgrow<strong>in</strong>g <strong>in</strong> the open<strong>in</strong>gs created when older trees died. Deadtrees rema<strong>in</strong> as stand<strong>in</strong>g snags and blowdowns, and this decay<strong>in</strong>gwood provides both future organic soil for moreplants and trees, and important habitat for a wide diversity ofanimals, microorganisms, flower<strong>in</strong>g plants, and fungi. Inaddition, many lichen and moss species cover surfaces <strong>in</strong>these forests.-------This brochure was created by the <strong>New</strong> <strong>Hampshire</strong> NaturalHeritage Bureau as part of a series designed to educate thepublic about the state’s special plants and natural communities.More site guides and profiles are available on the Visit<strong>in</strong>g<strong>New</strong> <strong>Hampshire</strong>’s Biodiversity program page at:www.nhnaturalheritage.org<strong>New</strong> <strong>Hampshire</strong>Natural HeritageBureauNH <strong>Division</strong> of <strong>Forest</strong>s & Lands - DRED172 Pembroke Road - PO Box 1856Concord, NH 03301-1856Tel: (603) 271-2215The DFL is an equal opportunity employer and educator.NH Natural Heritage BureauVisit<strong>in</strong>g <strong>New</strong> <strong>Hampshire</strong>’s Biodiversity<strong>Old</strong> <strong>Forest</strong> <strong>in</strong><strong>Franconia</strong> <strong>Notch</strong><strong>State</strong> <strong>Park</strong>a property managed by<strong>New</strong> <strong>Hampshire</strong> Department ofResources & Economic Development<strong>Division</strong> of <strong>Park</strong>s & RecreationThis brochure was paid for with funds fromthe NH Conservation License Platewww.mooseplate.com
TRAIL DESCRIPTION:Along this stretch of the bike path you will pass throughpatches of old forest. The paved path travels over easy tomoderate terra<strong>in</strong> with some hills. The surface is smooth, butit can be slick when wet, and the weather <strong>in</strong> the <strong>Notch</strong> canchange quickly at any time of the year.Start<strong>in</strong>g at the park<strong>in</strong>g lot near Lafayette Campground, takethe bike path south <strong>in</strong>to the woods. When not obscured byleaves, Mt. L<strong>in</strong>coln and <strong>Franconia</strong> Ridge are visible abovethe parkway to the left. On your right is the PemigewassetRiver, which is really just a small cobbly brook this close toits orig<strong>in</strong>. On either side of the path (1), notice a mix ofyoung and old trees such as sugar maple, yellow birch,beech, and red spruce. Part of this forest has apparently beencut <strong>in</strong> the past, and a severe hurricane <strong>in</strong> 1938 blew downmany trees, leav<strong>in</strong>g large gaps for younger trees to fill. Scatteredthroughout, however, are trees that survived the hurricaneand are much older. This mix of young and old treesclosely mimics the ecology of our orig<strong>in</strong>al natural northeasternforest, where w<strong>in</strong>d and fire have historically acted asnatural disturbance agents. Several particularly large yellowbirch trees can be seen beside the path about 50-100 feetfrom the start. One of these trees has a diameter of 33 <strong>in</strong>chesat chest height (quite big for a tree <strong>in</strong> an eastern mounta<strong>in</strong>forest). In addition to their characteristic gnarly upperbranches where decades of severe weather have taken a toll,some of the older trees have scars spiral<strong>in</strong>g up the trunk <strong>in</strong>the bark. These scars are healed cracks, orig<strong>in</strong>ally caused bylightn<strong>in</strong>g, frost-wedg<strong>in</strong>g, or trees twist<strong>in</strong>g dur<strong>in</strong>g high w<strong>in</strong>ds;the cracks often occur <strong>in</strong> the direction of prevail<strong>in</strong>g w<strong>in</strong>ds.As you cross Walker Brook (often dry <strong>in</strong> late summer) on awooden bridge with iron rails (2), you’ll see large rott<strong>in</strong>glogs to either side, along with other woody debris likedowned branches. Large and small woody debris <strong>in</strong> variousstages of decomposition are <strong>in</strong>dicative of older forests andthe natural process of forest decay and regeneration. Justbeyond the bridge to the left (3), observe several large treesand a dead stand<strong>in</strong>g snag. Then, at a turn to the right (4), notethe presence of a large amount of hobblebush (Viburnumalnifolium) <strong>in</strong> the understory. This bush, with its suede-likebuds and ve<strong>in</strong>y leaves, is often browsed by moose and isvery common <strong>in</strong> this type of forest.Next, you pass through a dense patch of spruce and fir trees(5) where there is deep shade year-round and it is relativelycool. The moist ground beneath these conifers is littered withtheir acidic needles, where few species of understory plantscan thrive save a green carpet of mosses and clover-likenorthern wood sorrel (Oxalis acetosella). A nice example ofa high-energy cobble/sand bar, constantly modified by therush<strong>in</strong>g water, can be seen <strong>in</strong> the river just off to the right (6).The forest soon opens up aga<strong>in</strong> as it transitions from thickspruce – fir back to mixed northern hardwoods (7). You willsee more large, old trees scattered throughout, some withmoss grow<strong>in</strong>g on their more shaded north sides. Understoryplant diversity <strong>in</strong>creases here, with woodferns (Dryopterisspp.), hobblebush, and tree sapl<strong>in</strong>gs be<strong>in</strong>g most prom<strong>in</strong>ent.You can also see many fallen logs, trunks, and branches <strong>in</strong>various stages of decomposition. Near the second picnictable pullout (8) there is a huge snag, with thick shelf fungusand <strong>in</strong>terest<strong>in</strong>g flaky bark patterns. An overgrown path withgrasses and wild strawberries (Fragaria virg<strong>in</strong>iana) <strong>in</strong> itcomes <strong>in</strong> from the left (9). The forest floor soon becomesquite bouldery off to the left, on a slightly steeper slope withwood ferns and birch trees. Off to the right there is a fairlylarge wet depression known as a forest seep (10), wheregroundwater emerges near the surface. Plant species foundhere <strong>in</strong>clude peat moss (Sphagnum), foamflower (Tiarellacordifolia), and northeastern manna-grass (Glyceria melicaria).Such seeps are frequent throughout this forest.Where the path crosses Dry Brook on the second woodenbridge (11), you can see another nice cobble bar below. Afew tenacious plants and moss species are able to take hold<strong>in</strong> the loose, gravelly soil of this seasonally dry dra<strong>in</strong>age. Afew hundred feet beyond, conifers beg<strong>in</strong> to reappear.Beyond a few more curves <strong>in</strong> the trail, you’ll see an evenagedstand of deciduous trees on the left (12), and a big lean<strong>in</strong>gyellow birch just to the right. Many ephemeral dra<strong>in</strong>agesw<strong>in</strong>d throughout this forest, caus<strong>in</strong>g small rolls and undulations<strong>in</strong> the otherwise flat ground. Soon, look for a yellowbirch tree on the left with its roots above ground and lots ofhobblebush nearby (13). This “barber chair” tree likely grewup around a fallen trunk that has long-s<strong>in</strong>ce rotted away.Another grassy woods road soon comes <strong>in</strong> on the left (14),this time with wild raspberries. Shortly after this, a densepatch of sugar maple sapl<strong>in</strong>gs can be seen off to the left, andseveral thick-trunked spruce trees tower over 100 feet abovethe path (15).A third wooden bridge crosses a smaller, unnamed brook(16). You are quite close to the parkway here, but <strong>in</strong> betweenand right next to the path you will pass by another smallforest seep (17). Soon the path sw<strong>in</strong>gs close to the riveraga<strong>in</strong>. Down the steep embankment you can see a cobble bar<strong>in</strong> the middle of the river, along with fallen tree trunks (18).Large spruce, fir, and hemlock trees frame the path along thef<strong>in</strong>al set of turns before it emerges from the woods at a park<strong>in</strong>glot.Well worth a visit, The Bas<strong>in</strong> (19) is a picturesque pothole<strong>in</strong> the river where a waterfall cascades over a small ledge.Afterwards, either return the way you came, explore fartheron the bike path, or take the Pemi Trail (no bikes allowed)back along the west side of the Pemigewasset River.