Nestled between a couple of the tightly-folded Appalachian foothills, about 50 miles downstream from where the Allegheny and Monongahela Rivers merge to form the Ohio River at Pittsburgh, PA, lies Irondale, Ohio, where I grew up. Irondale is a village of about 300 people, having shrunk from a mighty 600 when I was there in the 70s and early 80s.
It was founded in the late 18th century when salt deposits were discovered at the confluence of what are now called Salt Run and Little Yellow Creek. Salt mining became its first industry, but was supplanted over the years by tin milling, clay mining and brick making. Today, the only real industry is a small recycling company where the main brickyard used to be.
That company is actually located in one of the suburbs of Irondale, called Salisbury. Now it might seem odd to speak of suburbs of a village, but that's sort of how we thought of it. Anyway, in older days, when my father was growing up there, Salisbury was the home of the clay mine, brick yard, and (clay) sewage pipe production that fueled the local economy. In still older days, the tin mill (America's first, the sign at Irondale's frontier states) was down in Irondale proper, although still on the 'other side of the tracks'.
Rail was the preferred mode of transport for moving the raw materials and finished products around in those days, and the tracks connected Salisbury, Irondale and Cream City (the other suburb, where I spent the first 9 years of my life) with the rest of the world. My teenage home in Irondale proper was very near those tracks, with just a small road and Little Yellow Creek separating us. There was a level crossing a quarter mile away, where 'Main Street' (now called East Avenue) crossed the tracks, so we would get a loud whistle anytime a train came through.
Now I'm told that in its heyday, Irondale had a cinema, several bars, a general store, a barber shop, a post office and several traffic lights. Much of that had atrophied by the time I hit the scene, and today only the hair salon survives.
My Dad graduated from Irondale High School, but my Mom, seven years younger, graduated from the new Stanton High School. Stanton drew from several communities, not just Irondale. The Irondale school was relegated to grade school status. I spent a couple of years there and a couple of years at Hammondsville grade school (because that was closest to my grandmother's house, where I was dropped off in the mornings when both of my parents worked at Ohio Brass making electricity pole insulators). In time, I duly went to and graduated from Stanton too. Now it has been relegated to the world of middle schools, and local high school students are bused even farther away to attend Edison High, where my old rival Jefferson Union High School used to be.
Back to Irondale... Downstream from our house, past the bridge that led to 'Main Street', a large flood wall was built (during the Great Depression, I think, as part of a job creation scheme). This was one of the two best places to fish, although you usually only got bottom feeders who hung around where a sewer emptied into the creek. The other main fishing hole was the reservoir, in the other direction, up Salt Run about a mile from the village centre. The water level in the reservoir seems to be tied to the population of the village. It gets lower every time I see it, and I think that the village now gets water from the county system rather than the reservoir.
Next to the creek down at the flood wall was the large park that had a playground, baseball diamond and basketball court. It was also the site of the annual Irondale carnival, where dodgy rides were constructed and, thankfully, never disintegrated with people on board. I remember being told that reserves of some sort of hydrocarbon, probably coal, caught fire underground there in 'the old days'. How I don't know. Anyway, the park also had a small war memorial with WWII vintage small cannon for us kids to sit on or smoke cigarettes behind.
There are several roads into Irondale. The main one runs along Little Yellow Creek two miles down to Hammondsville (home of Stanton High School), where it hits a state road that roughly follows (Big) Yellow Creek down to the Ohio River and a four-lane highway. All others head upwards, as Irondale lies in a cup-shaped valley (or dale!). Irondale and Hammondsville sit at about 700 feet above sea level. About 500 feet above them lie the long ridges including Pine Grove and Chestnut Grove.
In this part of the States, you can see the hand-off from the landscape and economy of the east to those of the midwest. In the valleys, you see the rusting remnants of industry - coal, steel, clay, brick. On the ridges, you find open farmland, primarily dedicated to feed corn and dairy cattle (I think). Head east, and you get more of the valley-type feel. Head west, and the hills flatten out into the wheat and corn fields of the plains.
Ruling the local landscape is the Ohio River itself. Big, wide and slow, it separates my home state from the West Virginia panhandle and Pennsylvania, each less than ten miles away. The river always had huge coal barges moving up and down it, through the locks at the New Cumberland dam - built for flood control, not electricity generation. Coincidentally, right next to the dam is a huge generation plant - powered by coal rather than water. I believe it has the distinction of being the fourth largest polluter in the entire US!
When I was growing up, it lay within Stanton's tax domain, so the local tax revenues (and the children from Stratton and Empire, where it sits) flowed to my school. This gave us a great swimming pool, athletics track, tennis courts, auditorium and all other amenities that schools these days so rarely have. A fair trade-off for the toxins I grew up breathing?