On my way to visit Hibernia County Park in Chester County, I was finally able to photograph this barn and the adjacent house near Coatesville that I had long wanted to get a picture of.
I also finally made a trip to the Coatesville Reservoir, another place I had never visited before.
Here are some other interesting sights in the area of Wagontown, Chester County.
It now feels more like Spring in Chester County, although the calendar still says it’s Winter. The weather, however, can’t seem to make up its mind. We start with a few scenes around Kimberton.
Heading south from Blue Knob, I visited several covered bridges in Bedford County. First up is the Osterburg Bowser Covered Bridge, a wooden covered bridge at East St. Clair Township. It is a 90-foot-long (27 m), Burr Truss bridge with a shallow gable roof. It crosses Bobs Creek, and it is one of 15 historic covered bridges in Bedford County. The bridge was listed on the National Register of Historic Places in 1980. It is an example of the bridges in this area that do not have complete sides.
I next made my way to Snooks Covered Bridge, a historic wooden covered bridge also located in East St. Clair Township Township. Built in 1883, it is a 75-foot-long (23 m), Burr Truss bridge with a shallow gable roof. It crosses Dunning Creek. It was listed on the National Register of Historic Places in (you guessed) 1980.
The Ryot Covered Bridge is wooden covered bridge that is located in West St. Clair Township. It was listed on the National Register of Historic Places in 1980. This bridge is a low to medium Burr Truss bridge with a shallow gable roof. It was damaged by fire in 2002, and reconstructed. The bridge was listed on the National Register of Historic Places in 1980.
A request to remove the bridge from the National Register was submitted after it was badly damaged by a fire in 2002. The bridge was set on fire by teenage arsonists in 2002. Most of the wooden parts of the bridge were badly damaged. The Ryot Bridge was rehabilitated only seven years earlier, so most of the added steel supports remained intact, along with the stone abutments. The bridge was restored by P. Joseph Lehman, Inc., at a total cost of $300,000.
The Cuppett’s Covered Bridge, which was built by Cuppett brothers William & Philip on September 14, 1882, is a historic covered bridge that is located in Napier Township. Privately owned by the Cuppett family from the day it was built, the bridge took just five months to build for a total cost of $780. John Wayde did the masonry work, and Jeremiah Thompson completed the carpentry. Crossing Dunnings Creek, the 70-foot-long (21 m) bridge is a unique design with unusually low arches and low side walls which highlight the patented Burr Arch Truss system. The Cuppett’s Covered Bridge was listed on the U.S. National Register of Historic Places in 1980 by the United States Department of the Interior. The bridge was quite a popular spot for family photos when I was there.
The Knisley Covered Bridge is a historic wooden covered bridge located at West St. Clair Township. It is an 80-foot-long (24 m), medium Burr Truss bridge with a shallow gable roof. It crosses Dunning Creek. The bridge was listed on the National Register of Historic Places in 1980.
Here are some photos of a recent trip to State Game Lands 110 and 211. SGL 110 is northwest of Hamburg. This game land runs along the top of a ridgeline on Blue Mountain. The Appalachian Trail also travels through this area. The leaves were starting to change color when I was there:
I next travelled into Dauphin and Lebanon Counties to visit State Game Land 211, the home of the Stony Valley trail, a former railroad bed belonging to the Dauphin and Susquehanna Railroad. This area was formerly the site of small towns supported by mining, timbering, ice harvesting and spring water bottling. The eastern end of the trail runs along side a well-known beaver pond.
Mount Davis (3,213 ft or 979 m) is the highest point in Pennsylvania. Located in the 5,685-acre (2,301 ha) Forbes State Forest near the hamlet of Markleton in Elk Lick Township, Somerset County, it lies on a gentle crest of a 30-mile (50 km) ridge line extending from central Somerset County southward into Garrett County, Maryland. The high point was named for John Nelson Davis, an early settler, American Civil War veteran, surveyor, and naturalist known for his studies of the mountain’s flora and fauna. During the Civil War, Davis served in Company E, 102nd Pennsylvania Infantry.
The summit of Mt. Davis may be ascended by car or a number of hiking trails. Its surroundings are noted for their patterns of unusual circular stone formed by periglacial action. A metal observation tower with a relief map of the region stands near the true high point.
I found this location surprising. It was not what I was picturing in my mind for many years. The area immediately surrounding the summit is state forest, however you can be a five minute drive from the summit and still be going through farmland, which doesn’t make the peak seem that prominent or that high. I guess the surrounding area is at a pretty high elevation.
Ryerson Station State Park is in Greene County in the southwestern corner of Pennsylvania, near the West Virginia border. It seems to sit off by itself down in that corner. It is near Moundsville, WV, a place I have been to, but that is a story for another day. The 1,164-acre park features the fanciest state park swimming pool I have ever seen, campground, hiking, fishing, picnicking, and winter activities.
Next we have an interesting feature – the remains of an old reservoir. I don’t think I’ve ever seen one quite like this. You can see where the hole was created in the dam to allow the stream to run again. The lake appears to have been fairly shallow.
Our next stop in the swing through western Pennsylvania is McConnells Mills State Park. The signature of this park is a 19th century gristmill and adjacent covered bridge. It occupies 2,546 acres of the spectacular Slippery Rock Creek Gorge, which is a National Natural Landmark. Created by the draining of glacial lakes thousands of years ago, the gorge has steep sides while the valley floor is littered with huge boulders. Scenic overlooks and waterfalls are popular natural attractions.
The park has distinctive geology. The bedrock formed more than 300 million years ago as layers of sand, mud, and peat built up in what was a coastal area. After becoming rock, these different layers were lifted to the surface in several mountain-building events. The different strengths of these rocks cause them to erode differently, helping to make the varied landscape of the park. The gorge and the dramatic topography of the park were created by glaciers during the past two million years.
The Cleland Rock Scenic Vista – unfortunately this has become a bit overgrown.
