Delta Slate Tour

SLATE - THE DELTA STORY

A HERITAGE TO BE PRESERVED

Tribute to the Delta Area Residents

The book "The River and the Ridge - 300 Years of Local History" can be obtained through the Old Line Museum, P. O. Box 35, Delta, PA 17314. Cost of the book is $35.00 plus $2.10 tax and $5.00 for shipping the thick book. Congratulations on the 150th anniversary of historic Delta!! The book is well worth the money with 300 pages, plenty of photographs and easy reading.

"Welsh Settlers of Delta, PA./Cardiff, MD" by Jack Jones and published by the Historical Society of Harford County, Inc. can be purchased for $5.00 from:

Jack Jones
243 Equine Cove
Red Lion, PA 17356
Tele. (717) 246-7100
Email: jjones1902@aol.com

(Click on an image to enlarge it)

Jeri Jones presented a paper at the 2005 Geological Society of America's Northeastern Section meeting in March on the history and heritage. Below is the abstract and reference.

Northeastern Section - 40th Annual Meeting (March 14–16, 2005)

Paper No. 14-2

Presentation Time: 8:30 AM-8:55 AM

THE PEACH BOTTOM SLATE IN SOUTHEASTERN PENNSYLVANIA - ONCE THE BEST BUILDING SLATE IN THE WORLD

JONES, Jeri L, Jones Geol Svcs, 276 North Main Street, Spring Grove, PA 17362, JLJ276@aol.com.

The Peach Bottom Slate (PBS) is found within a complex metamorphic terrain in Lancaster and York counties, Pennsylvania, extending into northern Harford County, Maryland. The formation is considered to be Ordovician in age, but its structure is still not completely understood. The earliest known quarrying of the slate goes back to Welshman John J. Roberts in the 1730’s. The first commercial slate quarry in the United States was opened in this area in 1785. In 1843, a large Welsh migration brought experienced miners into the area. With the introduction of the Welsh, a new technique of straight-walled deep surface mining was introduced. Approximately 34 quarries once operated within the PBS on “Slate Ridge.” At the 1850 World Expo in London, England, the PBS was voted the “best building slate in the world.” Uses for the slate included grave markers, shingles, sidewalks, windowsills, fence posts and stove plates. The slate has been used in many federal and state buildings as well as the Biltmore Mansion in Asheville, North Carolina. The final use of the slate in the 1930’s and early 1940’s was roofing granules at the Funkhauser‘s Quarry. Due to it’s higher than normal content of silica and aluminum, the PBS keeps its original color and does not weather. A local church has had a PBS roof on it for 200 years without any leakage.

Delta, a small community in the southeastern corner of York County, Pennsylvania, is probably thought to be more closely associated with Baltimore, Maryland instead of York. It was within this community, in 1850, that a "backyard" mineral resource would take this small, sleepy town into the center of stardom for slate. At the London Expo in that year, the Peach Bottom Slate was judged as the best decorative slate in the world. Many eyes focused their future onto Delta, including the Welsh, which actually started their migration in the area in the mid 1840's. With their knowledge on deep, straight wall mining from Wales, the Welsh educated the Scotish-Irish residents on extracting the maximum tonnage of slate from the quarries.		High altitude view of Delta (lower center) and Peach Bottom Atomic Power Plant and Susquehanna River along right side.
The Peach Bottom Slate District is certainly one of world fame. Although the discovery of the slate in Delta are credited to Welshman John J. Roberts in the 1730's, the first commercial slate quarry in the United States was opened in this area in 1785 by William Docher. All of the slate quarries were situated on the original McCandless property and later owned by the Williamson estate. Slate Point, located just south of the Peach Bottom Atomic Power Plant, is believed to be the location of the first quarrying in the area. John Cooper was the original owner of the property, but sold to his grandson, Steve Thomas Cooper in the 1790's. Steve struck a deal with a John Kirk "to allowing the quarrying of slate for 99 years, at $.01/year until Kirk begins quarrying, $30/year for the first 7 years of quarrying, $60/year thereafter. Although the history of these pits is quite scarce, it is believed that the slate was hauled by wagon to Peach Bottom, now the site of the atomic power plant. From atop Slate Point, which is owned by Philadelphia Electric Company, a great view of the Susquehanna River is seen.
The role of a slate miner was a semi-skilled occupation. Wages were low for a ten-hour day and the work very hard and dangerous. Loosening the large slabs of slate from the vertical quarry walls while supported on a platform and removing to the sawer's shanty was risky. Not only was skill involved in being a miner, but a lot of luck, hoping that the machinery, tools or cables would not fail, causing a serious accident. Loosening the slate from the walls was not done by dynamite as suspected. Dynamite was too strong and would seriously fracture the rock. The lower-energy black powder was used to soften the blast, after which large wedge chisels were pounded into the fractures to slowly heave the slate block loose. The slabs removed were twelve feet by eight feet With the introduction of the Welsh in the 1840's, they brought with them the art of tunneling. Several advantages to tunneling was the fact that none of the overburden was disturbed and it took less work to find the commercial slate. Also, tunneling provided shelter when inclement weather occurred. A constant temperature of sixty degrees F. remained year-around in the tunnel, rather comfortable working conditions. Cables run across the quarry. From these ran trolleys and with other cable rigging, they were able to lift the slab out of the excavation. Splitting the slate was another talent only mastered by a few. In 1929, 263,668 squares of slate were produced (Ashley, 1931, A Syllabus of Pennsylvania geology and mineral resources, PA. Geologic Survey, 4th. series, Bulleting G1).		The Jones Quarry as photographed in 1999. Pit is about 800 feet long, 100 feet wide, and 70 feet deep to the water elevation. Water is about 70 feet deep. A waste pile at the Jones Quarry. Low quality slate and overburden was dumped here.
Slateville Presbyterian Church was organized in 1849 by a few members who separated from Slate Ridge Presbyterian Church. The cornerstone was laid on September 7, 1849, the date of the organization. Dedication occurred on June 8, 1850.In 1867, the congregation saw that the building was too small, and built a new structure at a cost of nearly $7,000. This building was improved and renovated in 1884. Within their cemetery, it is quite noticeable the difference between the granite, marble and slate grave markers. One problem that helped to lead to its demise was that the slate was too durable to the weather. Engraving on the slate dating back to the late 1700's looks "like new" today. The life of a Peach Bottom slate roof is often 150 years. The colonial interior includes the original stained glass windows, oak pews, and a Midner-Losch pipe organ which was installed in 1927. Carillon bells added in 1972 contribute music heard daily throughout the Delta countryside. The church celebrated their 150th anniversary in 1999. The church has been the "lunch stop" for the tours that Jeri Jones leads into the area, either through Jones Geological Services or the York County Parks.		Notice the slate sidewalk, steps and church tower roof. Slateville Presbyterian Church cemetery, a great place to inspect the Welsh language and slate engravings.
The Welsh families needed to settle someplace close to the quarries. Because the Welsh were a close-knit group, they basically did everything together. Along with their love to quarry slate, much of their social time was dedicated to two their loves: the church and music. The Welsh constructed vernacular style cottages in nearby settlements. The only standing settlement of three is Coulsontown, The cottages were replicas of the miner villages found in the mountainous Snowdonia region of northwest Wales. Main Street in Coulsontown is about 600 feet long and gravel paved. Main Street today consists of a few vacant lots, several modern homes, a two and one half story frame cottage and four stone quarrymen's cottages. Cornerstones are large, well-shaped quoins. Door and lintel blocks are one single block. The walls are composed of the Cardiff Conglomerate, found locally. Roofs are covered with slate. A distinctive feature is the four courses of cornice made of brick. Brick was considered a luxury item in Wales, thus the bricks here represent a symbol of the new economic status in America.		A cottage constructed with the Cardiff Conglomerate. Walls are about two feet thick. Notice the double chimneys
The largest quarry in the district is that of the Funkhauser's Quarry. Once three separate operations, the quarries were combined, now having a total length of about 1200 feet with vertical walls and water-filled. Site of the last slate operation in the area, shutting down in about 1944. The mining was extended northward by tunneling. The worst accident in the quarrying history of Delta occurred here in the early 1900's, when seven men were killed in a tunnel by a dynamite blast. The last products produced were that of roof granules, although high-grade roof shingles were also produced. The product was hauled to the mill by railroad. Remnants of the mill can still be seen on the north side of Atom Road. Because of its easy access into the bottom of the quarry, this location has been a popular swimming area. Although the property is heavily posted, Funkhauser's Quarry has been proclaimed by the U.S. Department of Labor, Mining Safety Division, as the second most-deadly quarry for drownings in the country.		View of the Funkhauser quarry looking southwest Funkhauser's Company of Hagerstown, Maryland operated the last slate business in this once-famous district.
One can't talk about the Delta area without including the Cardiff Marble Company, just south of Delta in Cardiff, Maryland. The site was famous for its own mineral resource, "Green Marble" or what geologists really term a serpentinite. The greenish rock is a metamorphic rock consisting wholly of serpentine minerals, commonly derived from the alteration of peridotite. In turn peridotite is a coarse-grained igneous rock formed very deep inside the Earth. The operation was originally a quarry being used road construction, but in 1913, a blast exposed a piece of the serpentinite. The quarry sent the rock to Baltimore for polishing, after which it was determined that a new resources has been discovered. After changing their equipment to concentrate on the beautiful rock, rapid expansion of the quarry started. At the completion of the operation in the early 1970's, the shaft extended to a depth o over 300 feet with numerous hallways at various levels. Huge blocks of the serpentinite were lifted out by horst and cable, similar to the slate operations and removed to the saws in nearby buildings. The rock was used for decorative stone, lamp bases, table tops, fireplaces, and desk ornaments. The rock was used as decorative stone in the Empire State Building in New York City, the Department of Highways Building in Harrisburg, along the bottom of the walls in City Hall in York, PA and in numerous federal buildings in Washington, D.C.		Horst and cable device to raise large slabs of the serpentinite out of the shaft as seen in 1999. Vertical shaft as it appeared in 1999.
So, what has happened to the heritage of the Peach Bottom slate industry and the Cardiff Marble? With the efforts of many of the residents who grew up in the community, the heritage is stronger than ever. As I found out when organizing my first fieldtrips there and continue to see, that area residents love to talk about the heritage. The Old Line Museum is downtown Delta is great way to discover the heritage. Filled with artifacts, photographs and clothing, a visitor can quickly find themselves living in the 19th century. The museum is also home of the world-famous "Slate Clock", a one-of-a-kind creation, made by Humprey O. Pritchard, a life-long slate miner. The clock stands seven feet and two inches tall and thirty inches wide and over one foot deep. Three different slates were used in the production of the clock: Peach Bottom deep blue slate, Bangor, PA silvery gray slate and red slate from Vermont. The museum is open Sunday afternoons, May through September from 1:00 - 5:00 pm and by appointment. Email them at oldlinemuseum@aol.com.		World famous slate clock
The geology of the Delta area is still one of those mystery areas. The first research conducted by George Stose and Anna Jonas in 1939 mapped the area as being a syncline, with the Peach Bottom Slate in the middle, while the Cardiff Conglomerate and the Peters Creek Formation scists laid on the limbs of the fold. Since the Cardiff Conglomerate is absent on the northern limb, Stose and Jonas placed a fault along the north side, between the slate and the Peters Creek Formation. Other researchers who mapped in the area saw evidence for an anticline and not a syncline (Michael Higgins from the U.S. Geological Survey among others). The most recent research was conducted by David Valentino, who at the time was employed by the Pennsylvania Geologic Survey, could not determine what type of folding was involved and proposed the name "Peach Bottom Structure" to the fold instead of the "Peach Bottom Syncline." With the complex geology and limited outcrops of bedrock (obviously most of the slate is exposed in vertical-walled quarries where one cannot look closely at the structure), this area is still debated by geologists. Because of the lack of fossils and the amount of folding in all of the formations within the Uplands Section of the Piedmont, the Peach Bottom Formation has been assigned an Early Paleozoic Era date.		Map of Stose and Jonas (1939) showing the Peach Bottom Formation (red).
Finally, it was discovered in the late 1970's by amateur mineral collector, Donald Schmerling, that gold occurred in several of the streams in the area. Today, about 15% of streams in York County contain gold. Although gold has not been found in place with bedrock, panning within several of slate quarries did produce gold. Other several good localities include the Delta Fish and Game Club along Peaks Peak Road, along the same streams further north where they intersect with Muddy Run near Castle Fin and in Robinson Run, al north of Delta. To the west of Delta, at Constitution, several small streams have produced gold and nice crystals of rutile. Largest gold found in this area is about 0.75 inch, apparently associated with the Peters Creek Formation schists.		Dark lines in left center (above "BO" in Bottom) and along the right top side of map represent streams that contain gold north of Delta.
G - Hughes Estate Quarry; H - Mills Quarry; J - Large Mills Quarry; K - Lloyd Quarry; L - Stewart Quarry; M - Electric Quarry; N - Edwards Evans Quarry; O - John Williams Quarry; P - John Humphrey Quarry; Q - McLaughlin Quarry; R - A small un-named opening; S - Faulk Jones Quarry; U - Johnson Quarry; V - R. L. Jones Quarry. Bold represents quarries that were combined to produce the Funkhauser Quarry. Belt extended into Maryland for a distance of 1.5 miles and into Lancaster County for about 5 miles. Entire slate area only about 0.25 mile wide. Dark line crossing the map from the lower left to the upper right represents the proposed fault between the Peach Bottom Formation and the Peters Creek Formation. Hashed boundary on south side of slate represents the approximate contact of the Peach Bottom Slate and Cardiff Conglomerate.