Serpentine Rock From Serpentine Barrens

Barrens

Even in pre-revolutionary Colonial days, it was recognized that patchy areas of Chester and Lancaster counties were covered with twenty-foot stunted evergreens instead of two-hundred foot oaks. They were "barrens", resembling the pine barrens of central New Jersey. In time, these barrens were particularized as Serpentine barrens, out of recognition that this stunting of vegetation was somehow associated with greenish stone in the bedrock. So, the serpentine barrens in time became serpentine rock quarries, but they seem somehow less barren now that surrounding deciduous forests have been cut down to make nice farmland. The greenish stone was a novelty, especially because it was usually (but not invariably) soft sandstone and easy to quarry, and the bedrock was only an inch or so under the topsoil, or even appeared on the ground surface as outcropping. These qualities made serpentine a popular building material, but in retrospect it should have been more apparent that sandstone crumbles easily, and what can stunt tree growth probably wasn't very good for you.

Serpentine Rock

Well, the green color comes from chromium salts. Sometimes the greenish color is diffused throughout volcanic rock, but more commonly concentrated in green veins "snaking" through sandstone. Diffuse is better for building, because the greenish intrusions create fracture lines in response to acid rain. In modern times, we mostly think of chromium as imparting a shiny look to plated auto bumpers. Some auto maker was once quoted as saying he sold more cars using $10 worth of chrome than with $100 worth of engineering. That's metallic chrome, because central to the definition of a metal is that it looks shiny. Even high school chemistry scholars can tell you it is a "salt" of chromium, the chromic ion, which imparts a greenish tinge when dissolved in water. So, chromic salts dissolved in the local water are what dwarf the vegetation of a serpentine barren, not chromate (which is yellow), and not metallic chromium (as in auto trim). So, although one might suppose otherwise, a few years ago when local builders started up modern quarries of the serpentine rock, the environmentalists of Chester County were up in arms. Demonstrations were held, editorials written, politicians hectored. The Serpentine Barrens were a local treasure, requiring legal protection; protective ordinances were demanded.

Although building construction with serpentine rock had a considerable flurry in the late 19th Century, the crumbly nature of sandstone caused the disappearance of all but a few examples. A building in boathouse row on the Schuylkill, a pre-revolutionary house on the Brandywine battlefield, College Hall on the campus of the University of Pennsylvania, pretty much comprise the notable surviving examples. But in a certain way, the Serpentine buildings do sort of define Victorian Philadelphia.

California is not within the intended scope of Philadelphia Reflections. However, it probably should be mentioned that Serpentinite is the official California rock, as would be natural for a substance which composes about 2000 square miles of its bedrock. It's green in color, but has a high magnesium content, and seems to originate with the grinding of techtonic plates as they throw up mountain ranges, with attendant earthquakes. California also has serpentine barrens, but local geologists blame that harmful vegetation effect on magnesium competing with soil calcium (rather than the less notable chromic ions in West Coast serpentine). We're getting into some pretty fine distinctions, here. Pennsylvanians will probably be content to know we found ours first, that it had a flurry in Victorian architecture, and it's just a bit quaint. And, that it doesn't pose a significant risk for asbestos poisoning. A California geologist, in defending their state rock honor, recently proclaimed there was greater statistical risk of dying from their state animal (the grizzly bear) than from their state rock.

(1834)