preventing the establishment of seedlings and permanently converting palustrine forested areas to openshrub or herbaceous wetlands. However, not all of the wetlands contain stumps, and these may havehistorically been open wetlands.Understanding these wetlands is further complicated by questions about the role of peat formation andbeaver activity in their history. The acidic character of the wetlands and the fact that a few of the wetlandstoday contain somewhat substantial peat accumulation suggests the possibility that some may have beenpeatlands. Peatlands develop when dead plant matter, usually sphagnum moss or graminoid vegetation,does not decompose and accumulates over a long period of time to form a spongy mat. Without mineralenrichment from surrounding bedrock, the environment typically becomes extremely acidic and nutrientpoor. Few plant species can tolerate such conditions, and thus the community that develops consists ofhabitat specialists, many of which are rare species in <strong>Pennsylvania</strong> because there are very few suchhabitats. Climatic conditions are not highly favorable for peat formation. Also, beaver were historically apart of this landscape, and it is ambiguous what their role may have been to influence peatlanddevelopment. Before European settlement the beaver population is estimated to have been much higherthan it is today, and thus it is likely that beaver occupied these wetlands at least periodically if notcontinually, and that this disturbance is a natural part of their history and development. Beaver dams causea cycle of ponding and vegetative re-colonization that might interrupt the process of peat formation, andalso can convert forested wetlands to open wetlands. Today, several of the county’s natural wetlands arecurrently occupied by beaver and others appear to contain former beaver ponds now undergoingsuccession.Floodplain wetlandsFloodplain wetland communities occur along rivers and streams in low-lying areas. These locations areperiodically inundated by the floodwaters of spring rains and snow melt or seasonal intense storm events,but may be dry for much of the year. They are predominantly forested, but also may have more openportions dominated by shrubs or herbs, especially where flood activity is most frequent and intense.In central <strong>Pennsylvania</strong>, floodplain forests are characterized by a canopy containing some combination ofsilver maple (Acer saccharinum), eastern sycamore (Platanus occidentalis), tulip poplar (Liriodendrontulipifera), black willow (Salix nigra), green ash (Fraxinus pensylvanica), American elm (Ulmusamericana), or box-elder (Acer negundo). Shrubs and vines common to these forests include spicebush(Lindera benzoin), ninebark (Physocarpus opulifolius), silky dogwood (Cornus amomum), Virginia creeper(Parthenocissus quinquefolia), and poison ivy (Toxicodendron radicans). Floodplain forest communitiesreceive severe disturbances from floodwaters including erosion, scouring by ice and debris, and/ordeposition of considerable quantities of sediment and debris. Only species with adaptations or tolerance forthese kinds of conditions can survive here. However, conditions also tend to be relatively mesic andnutrient-rich, due to continual influx of organic material borne by floodwaters, and thus a unique anddiverse plant community is typically present. In Clearfield County, the best examples of floodplain forestare found along the West Branch Susquehanna River and along broad floodplain areas of the large creeks inthe southern portion of the county, such as Chest Creek and Clearfield Creek.Seepage wetlandsA final major category of wetlands highlighted in this report are seepage wetlands. These wetlands formwhere underground water reaches the surface. Rainwater not only runs off the soil surface to accumulate inobservable above-ground bodies of water, such as streams and lakes but drains through the soil toaccumulate in and flow through bedrock layers, following fissures and areas of low density rock. Wheregroundwater intersects the surface, a broad area of saturated soil called a “seep” will form if the volume islow, and a concentrated stream of water termed a spring will be formed if the volume is higher. Theseepage wetlands highlighted in this report form at the foot of slopes; precipitation received by the uplandareas sinks down through loose, permeable layers of sandstone bedrock, is re-directed laterally upon13
encountering a more dense layer of rock, and eventually emerges at the surface. Groundwater dissolvesminerals from the bedrock layers through which it flows, and thus may substantially influence the chemicalenvironment of a seepage wetland. Seeps in Clearfield County are expected to be fairly acidic, as thebedrock is predominantly sandstone, which contains few soluble minerals. They are typically shaded byforest canopy, and thus provide consistently cool and wet habitat conditions which certain plant and animalspecies thrive upon. Many species of salamanders use seeps, and typical plant species are jewelweed(Impatiens sp.), bee balm (Monarda sp.), slender manna-grass (Glyceria melicaria), golden ragwort(Senecio aureus), wood sorrel (Oxalis acetosella), scabrous sedge (Carex scabrata), northern awned sedge(Carex gynandra), mad-dog skullcap (Scutellaria lateriflora), marsh pennywort (Hydrocotyle americana),a sedge (Carex torta), marsh marigold (Caltha palustris), false nettle (Laportea canadensis), woodhorsetail (Equisetum sylvaticum) and golden saxifrage (Chrysosplenium americanum).Wetlands and MiningWhere mining has occurred in the upland areas above any wetland that receives seepage inputs, drainagethrough the disrupted bedrock layers will typically contaminate these groundwater flows with dissolvedmetals (mainly iron, aluminum, and manganese) and acids. Upon reaching the surface and encounteringoxygen in the air, some of the metal compounds convert to solid form, thus accumulating in seepage areasas the orange (iron), bluish-white (aluminum), or black (manganese)-colored sediment characteristicallyassociated with mining drainage. Aluminum, manganese, and high acidity are all toxic to aquatic life; ironis less toxic. However, the accumulation of sediments of any of the metals degrades aquatic habitats byblocking light needed by aquatic plants and microorganisms, and clogging the tissues of aquatic animals.The impacts of abandoned mine discharges (AMD) on a particular wetland will depend on theconcentration of the contaminants in the discharge and the volume of the discharge, relative to the overallvolume of the wetland.14
- Page 2 and 3: CLEARFIELD COUNTYNATURAL HERITAGE I
- Page 4 and 5: Over the history of these studies,
- Page 6 and 7: TABLE OF CONTENTSPreface………
- Page 8 and 9: EXECUTIVE SUMMARYIntroductionA heal
- Page 10 and 11: Ground SurveyAreas identified as po
- Page 12 and 13: Table 1. Natural Heritage Areas cat
- Page 14 and 15: outcrops occur in conjunction with
- Page 16 and 17: INTRODUCTIONA healthy natural lands
- Page 18 and 19: Natural Resilience, Human Activitie
- Page 20 and 21: Natural Heritage Inventory MappingG
- Page 23: Natural History Overview of Clearfi
- Page 26 and 27: SoilsSoil character exerts a strong
- Page 30 and 31: METHODSThe methods used in the Clea
- Page 32 and 33: fragmenting feature data to generat
- Page 34: *Defined as: 2,000 waterfowl (at on
- Page 38 and 39: RESULTSContiguous Forest Blocks in
- Page 40 and 41: Table 5. ContinuedSize% Roadless Ac
- Page 44 and 45: Landscape Conservation AreasThe Lan
- Page 46 and 47: SGL #120 LCAThis LCA is a contiguou
- Page 48 and 49: Moravian Run - Alder Run LCAThis LC
- Page 50 and 51: Threats and StressesIn some portion
- Page 52 and 53: Gifford Run Valley, west slope37
- Page 54: Beccaria Township, Coalport Borough
- Page 57: Bell Township, Mahaffey Borough, &
- Page 60 and 61: Featherbells(Stenanthium gramineum)
- Page 62 and 63: Supporting Natural Landscape—To m
- Page 64: Bigler TownshipPNDI Rank Legal Stat
- Page 67: Bloom TownshipPNDI Rank Legal Statu
- Page 70: What It Looks Like:Appalachian Game
- Page 74 and 75: BOGGS TOWNSHIPThe landscape of the
- Page 77 and 78: BRADFORD TOWNSHIPThe landscape of B
- Page 80 and 81:
BRADY TOWNSHIPBrady Township falls
- Page 83 and 84:
BURNSIDE TOWNSHIPThe West Branch Su
- Page 85 and 86:
BURNSIDE BOROUGHThe landscape of Bu
- Page 88 and 89:
CHEST TOWNSHIPChest Township is 71%
- Page 90 and 91:
Heron Rookery at Chest Creek Floodp
- Page 93 and 94:
COOPER TOWNSHIPCooper Township lies
- Page 96 and 97:
COVINGTON TOWNSHIPThe northern half
- Page 98 and 99:
Creeping Snowberry(Gaultheria hispi
- Page 100 and 101:
should be avoided within the core a
- Page 103 and 104:
DECATUR TOWNSHIPMost of Decatur Tow
- Page 106 and 107:
FERGUSON TOWNSHIPThe southwestern p
- Page 111 and 112:
GIRARD TOWNSHIPThe northern two-thi
- Page 113 and 114:
The Supporting Natural Landscape is
- Page 115 and 116:
RecommendationsCore Habitat Area—
- Page 120 and 121:
GOSHEN TOWNSHIPMost of Goshen Towns
- Page 122 and 123:
Gifford Run Wetlands (pg. 81)Steepl
- Page 125 and 126:
GRAHAM TOWNSHIPThe landscape of Gra
- Page 128 and 129:
GREENWOOD TOWNSHIPGreenwood Townshi
- Page 131:
Gulich Township & Ramey BoroughPNDI
- Page 134 and 135:
herbaceous layer is somewhat sparse
- Page 136:
Huston TownshipPNDI Rank Legal Stat
- Page 139 and 140:
Supporting Natural Landscape— Any
- Page 141 and 142:
Along the stream channel connecting
- Page 143 and 144:
Supporting Natural Landscape—Use
- Page 145:
Jordan TownshipPNDI Rank Legal Stat
- Page 148:
Karthaus TownshipPNDI Rank Legal St
- Page 151:
Knox TownshipPNDI Rank Legal Status
- Page 154:
Lawrence Township & Clearfield Boro
- Page 158 and 159:
documented in Pennsylvania. It hibe
- Page 160 and 161:
allegheniensis) dominant in the can
- Page 162:
Morris TownshipPNDI Rank Legal Stat
- Page 165:
Penn Township, Grampian Borough,& L
- Page 168:
Pike Township & Curwensville Boroug
- Page 171:
Pine TownshipPNDI Rank Legal Status
- Page 174 and 175:
pine species (Lycopodium dendroideu
- Page 176 and 177:
Threats and StressesFoot traffic on
- Page 178 and 179:
wetlands to determine its uniquenes
- Page 180:
Sandy Township, Dubois City, & Fall
- Page 183 and 184:
eeding season, and they will be sen
- Page 185:
Union TownshipPNDI RankGlobal State
- Page 188:
Woodward Township, Brisbin Borough,
- Page 191 and 192:
RECOMMENDATIONSThe following are ge
- Page 193 and 194:
situations, the site is effectively
- Page 195 and 196:
GLOSSARYAlluvium: detrital deposits
- Page 197 and 198:
LITERATURE CITEDAnonymous. 1985. A
- Page 199 and 200:
Naeem., S. (Chair), F.S. Chapin III
- Page 201 and 202:
GIS DATA SOURCESBedrock geologic un
- Page 203 and 204:
APPENDIX IIPENNSYLVANIA NATURAL HER
- Page 205 and 206:
Evidence of Disturbance (logging, g
- Page 207 and 208:
GLOBAL STATECOMMUNITY NAME RANK RAN
- Page 209 and 210:
GLOBAL STATECOMMUNITY NAME RANK RAN
- Page 211 and 212:
GLOBAL STATECOMMUNITY NAME RANK RAN
- Page 213 and 214:
APPENDIX V bPENNSYLVANIA STATUSNati
- Page 215 and 216:
small numbers throughout their rang
- Page 217 and 218:
State Element RanksS1 = Critically
- Page 219 and 220:
Photo: Lisa SmithHairy rock-cress (
- Page 221:
The Sustainable Forestry Initiative