Most of the Preserve's distinctive topography is a consequence of water erosion by
Jordan Creek and its tributaries through the uplands of the Schochary Ridge.
Geology The park's boundaries are on the far-east terminus of the Schochary Ridge; It marks the boundary of the "Game Preserve" fault line which separates the New Tripoli formation of the Schochary Ridge and the Martinsburg formations. The Schochary Ridge is an outcropping of rock which formed during the last stages of the
Taconic orogeny. The long east–west-oriented ridge is several miles south of
Kittatinny Ridge (within the otherwise flat and fertile
Lehigh Valley) and is bisected, within the park, by
Jordan Creek. The non-Schochary geology of the Nature Preserve is of the Martinsburg Formation, predominately made up of New Tripoli Member. The Martinsburg Formation developed during the Ordovician period (490 to 443 million years ago), and is characterized by dark grey
shale and thin beds of
siltstone and
sandstone, with depths up to 12,000 feet. The New Tripoli group, the dominant geologic member in the preserve, is composed of shale and calcareous
turbidites with sedimentary characteristics. Shale is largely impervious to water producing high surface runoff, but its weak structure is highly erodible, resulting in gentle slopes.
Hydrology Jordan Creek and its minor tributaries, including Mill Creek, Hegel's Run, Elk Ridge Run, Macintosh Run, and Thicket Run, give the preserve a distinctive hill and valley character. The preserve is the easternmost extent of Schochary Ridge, which arises from the relatively flat surfaces of the
Lehigh Valley. Mill Creek is a major perennial tributary; its watershed drains large portions of agricultural land in the
Lowhill Township, southern
Heidelberg, and
Washington Townships. Mill Creek does not enter the preserve but forms its geographic western boundary and joins with the Jordan Creek just short of the preserve. The creek, whose swift waters eroded the valley in which it flows, separates the preserve from the more westerly State Game Lands 205. Mill Creek also provides a perennial source of water which helps to maintain the thicket of
deciduous trees, which are principally
oak and
maple and grow on the preserve's north-western boundary. After the confluence of the Jordan and Mill Creeks, the Jordan enters the preserve and heads north-north-east. To its west, the Jordan is bounded by the imposing Mill Hill (along which the Theyken Ridge Trail runs). Further downstream, Mill Hill recedes straight north as the Jordan turns east—Mill Hill's proximity to the Jordan is further distanced by a valley cut by Hegel's Run. Hegel's Run is a perennial minor tributary of Jordan Creek, originating within
skunk cabbage wetlands in the interior of the preserve. Flowing north to south, Hegel's Run continues out of the wetlands and parallel to the Fireman's trail where, along its course, it is fed by two smaller unnamed tributaries originating from springs on the sloping Mill Hill which are blanketed by a heavy canopy of
autumn-olive and by a minor tributary originating to the northeast in the grassy Schantz valley. Hegel's Run flows further south where, after being crossed by the firemen's trail forms a confluence with Jordan Creek immediately upstream of
Schlicher's Covered Bridge. After passing under Schlicher's Covered Bridge and a pedestrian footbridge, the Jordan Creek makes a hairpin curve, ultimately turning to flow straight south. To the east of the creek, in this section, arises Elk Ridge, which is the last and easterly most rise of the Schochary Ridge. Elk Ridge Run, Macintosh Run and Thicket Run are all seasonally intermittent minor tributaries of the Jordan. Just before the ford, the Jordan is joined by Elk Ridge Run. This south flowing watercourse begins near the bison paddocks and drains the eastern slope of Elk Ridge and the western slope of the environmental center grasslands. After the ford, the Jordan Creek continues south until forming a confluence with Macintosh Run. Since the early 2010s, the Northern Range has also been developed by the Valley Mountain Bikers. They have developed
mountain biking trails through dense thickets of autumn-olive. The trails are open to the public and can be accessed via the North Range Utility Road and parking lot. The central Range is the largest of the three ranges; it also contains the greatest variation of topography. It is bounded on the north by the Jordan Creek and Hegel's Run and on the south by Old Packhouse Road—a portion of the southern end is occupied by the Lehigh County composting facility. The Central Range is subdivided into eastern and western sections by the Jordan Creek. The Eastern Central Range begins south of Hegel's Run and is centered around the dramatic Elk Ridge, which is the highest point in the preserve and also forms the extreme easterly extent of the Schochary Ridge. Elk Ridge is home to the preserve's
bison and
elk herds. The extreme eastern boundary which borders
Lehigh Carbon County Community College is marked by a deciduous tree-line of
walnut, oak, and maple receding into grasslands interspersed with autumn-olive. The center is on one of the highest parts of the preserve and features straight lines, a low profile, and muted colors which merge the building into dramatically rolling grasslands. It also has a rooftop observation area, a community room for environmental education programs and meetings, and restroom facilities for park visitors. The building also houses satellite offices for the Lehigh County Parks Department and the
Pennsylvania Bureau of Forestry. The Western Central Range begins south of Jordan Creek and is centered around the
Lehigh Valley Zoo. Because of the presence of the zoo, and the road connectivity, including the Jordan Ford, it is the most visited section of the preserve. This section has views of west-facing
Lowhill Township grasslands. The lowland sections provide views of eastern Pennsylvania river valleys, and fishing opportunities. The Trexler Border Trail, as it descends off the western veld and down into the Jordan Creek Valley, is surrounded in spring and summer by fecund native wildflower, which draw abundant native butterfly and birds. The Trexler nature trail, which follows Jordan Creek from the ford has views of the river, as well as mixed deciduous and conifer forest and exposed shale formations which are often covered in damp mosses. There are bird blinds in this area for ornithologists. The Northern boundary of the Southern Range is Old Packhouse Road and its Southern the boundary of a commercial orchard. This range is the least visited and most ecologically precarious of the three with only a single trail leading into this area—the Trexler border trail. At one time, large parts of this range were in production as an apple orchard. Stands of old apple trees interspersed with autumn-olive dot this landscape. At the far south of the park is a large glade of
Eastern Hemlock and other conifers which provides a distinctly different forest environment from elsewhere in the preserve. The confluence of Thicket Run and the Jordan Creek also create a moist lowland ideal for the growth of wildflowers and
cattails. == Flora and fauna ==