Tag Archives: environment

It’s open water year round these days on the Fox River

Drive south on Ill. Route 25 along the Fox River from the Kane County line during the coldest winter months and you won’t help but notice that the farther you travel into Kendall County the more the amount of ice on the river increases.

Granted, the river from the Montgomery dam south to Oswego is generally swift moving and dotted with small rapids, but swift-flowing water isn’t the reason the Fox doesn’t freeze over, because it used to just a few decades ago.

So what’s the reason for the open water until you nearly reach Yorkville?

The main answer seems to be that the largest tributaries of the Fox River these days are not those creeks, springs, and wetlands created by the last Ice Age. Instead, we are the river’s largest tributaries—the men, women, and children who live in the Fox Valley.

When the 18th Century ended, it was less than three decades until the first permanent white settlers arrived in the Fox Valley. As 1799 turned into 1800, the river’s largest tributaries were the creeks that drained thousands of acres of wetlands that dotted the river valley from Wisconsin to the mouth of the Fox on the Illinois River. In Kendall County, the largest of these subsidiary streams were, from north to south, Waubonsie Creek, Morgan Creek, Blackberry Creek, and Big Rock Creek.

Most of these creeks were the main outlets for large wetlands. Waubonsie Creek, for instance, drained the Wabausia Swamp on the Kane-Kendall County border, a wetland that covered nearly a square mile. Morgan Creek, too, drained extensive wetlands that were the remains of a former glacial lake.

Both north and south, other smaller and larger streams and springs added their flows to the river.

During the winter months, the water that seeped and flowed into the river from its bordering wetlands and tributary creeks was cold, having been pre-cooled as it slowly made its way to the river.

1915 abt Drainage

One of the many rural drainage projects was this 24″ tile draining wetlands along Wolf’s Crossing Road into Waubonsie Creek about 1911. This particular project was dug by hand. (Little White School Museum collection)

As soon as the settlers arrived, they began to wage war on the Fox Valley’s expansive wetlands. Over a 50-year period, they aggressively drained marshland and channelized streams, the former to create more farmland and the latter to drain stormwater into the river as quickly as possible to stop nearby farmland from flooding. Their efforts were extremely effective, even given that all the earliest drainage work was completed by animal power and hand labor. By the start of the 20th Century, drainage efforts continued, now assisted by steam-powered dredges.

The result was the addition of additional tillable land, and the elimination of wetlands that were homes to hordes of disease-carrying insects. Drying up the county’s numerous marshes and sloughs led to a precipitous decline in the occurrence of malaria—called “the ague” by the settlers.

But a major unintended consequence of all those drainage efforts was that they not only sharply decreased the summer and winter flows of the river, but they also led to more frequent flooding. That’s because the stormwater “banks” created by the county’s wetlands and meandering streams were eliminated. Instead of runoff trapped in sloughs and marshes slowly soaking in to recharge ground water supplies and be slowly discharged over a period of weeks following rainstorms or snow melt, the runoff was rapidly channeled into the Fox River where it flowed downstream to the Illinois River. When dry months arrived, there was no water “bank” to add to the river’s flows, and it nearly dried up during some dry periods.

In addition, the velocity of the water from the Fox’s tributaries greatly increased due to the elimination of meanders in the streams—channelization—and the disappearance of the wetlands that once slowed the speed of stormwater runoff. That resulted in farmland drying out much more quickly after precipitation fell, but it also resulted in more erosion, with the area’s incredibly rich topsoil washing into the fast-flowing channelized streams. The fast-flowing muddy water caused major flooding far more frequently.

Fox Metro plant

The Fox Metro Water Reclamation District’s sprawling wastewater treatment plant between Montgomery and Oswego is today a major Fox River tributary.

And then, as the 19th Century ended, a new sort of tributary started adding to the river’s flows, this one far from the crystal clear water that was once generated by wetlands and meandering creeks. In the early decades of the 20th Century, it finally became apparent, that simply dumping raw sewage, from human waste to industrial products, didn’t get rid of the problem; it just moved it downstream. The human, animal, and industrial waste pumped directly into the river began to be treated to greater or lesser degrees as recognition of the dangers of pollution became clearer, and as wastewater treatment technology advanced.

With the Fox Valley’s population growth, the increasing volume of body temperature sewage began raising the river’s temperature, but at first there wasn’t enough inflow volume to noticeably affect it. As late as the late 1960s, the river regularly froze over all the way from Aurora south to Yorkville. When I was in high school in the early 1960s, we regularly ice skated on the river from Oswego north to Boulder Hill, a distance of three or so miles.

Ice skating on Fox

In about 1920, when this photo was snapped on the frozen Fox River immediately upstream from the Oswego bridge, the river regularly froze over and offered a fine site for community ice skating. (Little White School Museum collection)

But shortly after that, as my friend, Dr. Paul Baumann, pointed out in his 1976 monograph, A Bicentennial History of the Fox River, by the time we celebrated the United States’ 200th birthday, about one-third of the water in the Fox River had already been used at least once by humans or businesses by the time it reached Kendall County.

And then came the Fox Valley’s explosive growth from the 1970s into the first decade of the 21st Century. With that growth, it’s likely the river’s single largest tributary has become the sanitary sewage treatment plants linking the river’s banks. And the relative warmth of that water (it’s slightly warmer, but no less pure than water already in the river thanks to modern wastewater treatment technology) means that nowadays the river seldom freezes between the Fox Valley Water Reclamation District’s huge wastewater treatment plant, located across the river from Boulder Hill, and the pool created behind the Yorkville dam.

Ice Houses

This view of Esch Brothers & Rabe’s ice houses north of Oswego, taken about 1890, gives an idea of the size of the company’s ice harvesting operation. (Little White School Museum collection)

As shallow as it is now and historically has been, the Fox River was never a main transportation route, but its dams did provide power for mills, its waters were rich in clams harvested for freshwater pearls and shells for buttons, and in winter its ice was harvested for use in both the home and industry. In fact, huge ice harvesting operations were conducted at each of the dams across the river, including at Yorkville and Oswego. How huge? In 1880, the Esch Brothers & Rabe ice company shipped 581 railcars of ice from Oswego. Of that number, they shipped 124 railcars full of ice from Oswego in August alone. By 1884, the ice company was shipping nearly 1,100 railcars of ice annually.

It’s fortunate cooling technology advanced so far that we don’t require that ice today, because through the impact on the environment of our mere presence here in the Fox Valley, we’ve managed to raise the river’s average temperature so much that it seldom freezes along much of its length in northern Kendall and southern Kane counties.

 

 

 

 

Advertisements

Leave a comment

Filed under Business, Environment, Fox River, History, Kendall County, Local History, Montgomery, Oswego, Science stuff

When the Fox River was known for its pearls—and pearl buttons…

Last week, the good folks over at the Aurora, IL Then and Now page on Facebook got to discussing Fox River clams and their uses, and it got me to thinking about the topic in its historical context.

We look on the Fox River nowadays as a major recreational resource for anglers and boaters—as we should—but it was much more than that during the 19th and early 20th centuries.

The Fox Valley’s pioneer millwrights lost no time in throwing dams across the river up and down its length to power mills that did everything from grind grain into flour to saw wood. The river water itself was harvested during the winter months as ice, which was marketed by commercial firms in those days before mechanical refrigeration.

Another of those little-known, but both interesting and lucrative, industries on the Fox involved harvesting clams. In the days before plastic became a practical alternative, buttons were made of metal as well as natural materials, including bone, wood, and mother of pearl from the inside of clam shells.

Seeking shells for buttons, the clamming industry got its start on the Mississippi River and its tributaries in the late 1800s. By the early 1900s, clamming had become a fairly big business on the Fox River, too.

One of Muscatine, Iowa’s button factories in the early 1900s.

One of the mother of pear button factories in Muscatine, Iowa that made the city the button capital of the U.S. for several years.

At first, clams had been harvested for the occasional pearls found in them. But when it financially worth while to ship clamshells off to button factories along the Mississippi near Muscatine, Iowa, the clamming industry on the Fox really got going.

By 1907, hunting for pearls from clams in the river had become a popular social activity for both men and women. On weekends, couples and groups would head off to the river, with the men wading in the stream collecting clams and women riding in boats accompanying them, opening the shells looking for pearls.

And occasionally, the hunters struck pay dirt. Natural pearls were extremely valuable during those years before the development of cultured pearls, and some dandy examples were taken from the Fox. Pearls selling for $200—about $4,500 in today’s dollars—and up were not uncommon.

Fox River pearls

Freshwater pearls my great-grandparents and other relatives found in clams on the Fox River at Oswego.

“Now what do you know about that?” marveled Lorenzo Rank, the Kendall County Record’s Oswego correspondent, in September 1909. “There has been more or less pearl hunting near here for several months, but since the lucky find made by Raymond Ness on Saturday—woe be unto the few remaining in clams. Saturday afternoon, Ness opened a small shell and out rolled a pearl that weighed 32 grains. It is nearly round and a pink pearl. Monday, William Strokmeier of Muscatine, Iowa came to town and gave Ness $725 for it. Trask & Plain and other Aurora jewelers had given offers on it but not so much as the Iowa buyer gave.”

That pearl really was a dandy, too, and would be worth more than $17,000 in today’s dollars—still a tidy sum indeed.

A 1911 article in the Record reported that some $2 million in freshwater pearls were being harvested in Illinois annually. And in July 1913, a doctor from Sheridan struck the freshwater pearl mother lode. According to the July 9, 1913 Record:

Muscatine buttons

Drilled clam shells, button blanks, and finished buttons from a Muscatine, Iowa factory.

“The most valuable pearl ever found on the American continent was brought into Chicago Wednesday to be appraised, says the Inter Ocean. It was valued at $8,700. The pearl was found several days ago by Dr. Jesse Carr of Sheridan on the banks of the Fox river. It weights 62 grains, and is a perfect specimen.”

But while pearls were an interesting and lucrative product of the Fox River, buttons made from the shells of the clams that created the pearls were an even bigger business.

The July 14, 1909 Record reported from Yorkville that:

“Fox river is being raked in the neighborhood and is giving up its wealth of clam shells to the manufacturers of the pearl button. About a month ago two young men, Milo Smith and Harry Rogers of Muscatine, Iowa, came to Yorkville and began to prospect for clams. Last week they shipped their first carload of shells and already there are two more parties of men interested. The river is rich in shells of the class that is required for the industry. Smith and Rogers, were about some time before they began active operations, but are now employing five or six men in the business. The raker goes out in a boat and scoops the clams out of the water and throws them in a pile. They are then taken to the shore where the raker is paid for them by the hundred pounds. Then they are steamed until the shells are opened and the clam is taken out and the shell is ready for shipment to the factory. Here they are cut into the size of the button required and finished, the polish being one of the delicate parts of the operation. Lawrence Hafenrichter has been working with them for some weeks and he has added much to his stock of river pearls. Friday of last week the men loaded a [railroad] car and shipped it to the factory at Muscatine. It is possible, should the supply of clams continue, that this nucleus may grow into a full fledged button factory in Yorkville.”

1910 clammer at Beloit

A clammer and his catch on the Rock River near Beloit, Wisconsin about 1910.

The Record’s prediction proved accurate, and it wasn’t long before enough clamming was going on in Kendall County to attract that button factory to Yorkville, thanks to a bit of early 20th century community economic development. In the summer of 1911, the Record reported that: “The Rehbehn brothers of Muscatine, Iowa, were the first to establish a factory for boring out button blanks in this vicinity, starting a small concern about a mile down the river from Yorkville. As the work grew on them they desired better quarters and an association was organized here by a number of the citizens who bought the old City Hotel property on the river bank from the Cassem estate and gave the use of it to the Rehbehns. It has been fitted with necessary machinery and about 15 or 20 men and boys are employed about the premises, boring blanks, which are shipped to Muscatine, where the product is finished into buttons for various uses. The residue of the shells makes a big pile at the east end of the factory.”

Shells drilled for buttons

Clam shells drilled for button blanks at the Rehbehn factory in Yorkville, Illinois. Recovered from the Fox River at Yorkville by by friend Mark Harrington.

Which brought to the fore the problem of what to do with all those clamshells. Over in Somonauk, the city fathers had a great idea: Use the piles of shells from the Somonauk button factory on the village’s gravel streets. Several loads of clamshells were dumped on the streets and leveled, the idea being that street traffic would quickly grind the shells into small pieces. But, alas, it was not to be. A note in the Somonauk Reveille (which, by the way is one of my favorite newspaper names) reported the problem: “Owing to the fact that as soon as the shells become partly broken they will be very hard on horses’ hoofs, travel over them will be exceedingly light, as they will be avoided whenever possible. Consequently it will be a long time before they will become desirable roads.”

So, for the most part, they were disposed of the way just about everything else was during that era: They were dumped in the river, where some of them can still be found, holes made by the button blank drills nicely intact.

As for the clam meat cooked during the opening process, it was either discarded or, which happened most often, was either given or sold to a nearby farmer to be used for hog or chicken food. As Eugene Matlock recalled of clamming on the river at his family’s farm south of Yorkville: “That cooked clam was taken back to our farmstead where it was a most welcome diet for the pig crop we seemed always to have.”

Misner Shop

The historic old Misner Wagon and Machine Shop in Millington, Illinois housed a button blank factory as late as the 1930s.

Despite those problems, the button blank business was apparently fairly successful until October 1914, when the button factory was destroyed by fire. By that time, though, the river had become badly polluted, and that, combined with growing pollution and over-harvesting had severely decreased the clam population. In addition, techniques had finally been developed to create inexpensive plastic buttons in colors other than black. As a result of that combination of factors, the Rehbehn brothers never rebuilt their factory.

Clamming wasn’t entirely dead, however. In 1937, Fred Leonard was operating a button blank factory in Millington’s historic old Meisner wagon and machine shop, but he had to partially rely on imported clamshells as well as those locally harvested.

Today, the catastrophic pollution that helped destroy the clamming industry has almost disappeared from the Fox River—thanks to those pesky clean water regulations so disliked by certain political factions—and its clam population is healthy and booming once again. But the days of clamming, button factories, and those lucky pearl hunters are gone, receding into the Fox Valley’s rich past.

 

 

Leave a comment

Filed under Aurora, Environment, Fox River, History, Illinois History, Kendall County, Oswego, People in History, Technology

When sledding was good in the Fox Valley

Time was, we could joke about northern Illinois climate consisting of winter and six weeks of bad sledding. But in recent years, the favorite lament of Midwesterners—until 2017 wrapped up, at least—has been the general lack of an old-fashioned winter.

Historically, that’s been a common complaint. For instance, on Dec. 27, 1916, Kendall County Record Editor H.R. Marshall was pleased to report that, at last, Kendall County was enjoying a fine old-fashioned winter, although modern life was intruding into the enjoyment a bit:

“No one can complain of the good old-fashioned Christmas weather for 1916. Snow on the ground and the thermometer hovering around zero makes one think of the earlier days. But the thing that is missing is the tinkle of sleigh bells. Once in a while you see a sleigh or a bob [sled} go by but little of the jingle that makes one feel that there is some pleasure in the world. The raucous toot of the auto horn and the sound of the open muffler have taken the place of ‘Old Dobbin.’”

A century plus a year later, things are different still. We have occasional cold snaps, as my dad used to call them, but then the weather usually warms, the snow and ice melts. And in recent years it never really returned during late winter.

1922 Trolley & ice skaters @Oswego

Ice skating on the Fox River at the Oswego Bridge about 1922 as the interurban trolley car crosses southbound on its way to Yorkville. In those days, the river froze solid most winters. (Little White School Museum collection)

This winter’s cold snap, however, is proving persistent. The Fox River hardly ever freezes solid between Aurora and Yorkville any more—this year, even as cold as it’s been, is no exception—because it is so warm, and not necessarily due to global warming, either. The major tributaries of today’s Fox River are the municipal sanitary plants that line its banks, pumping out their streams of warm treated wastewater. You can see the results of that by driving along Ill. Route 25 opposite the Fox Metro Water Reclamation District’s plant in Oswego Township on a cold winter day. Just note the vapor rising from the treated water as it enters the river.

This year, however, not only have we had unusual cold, but we’ve also had a bit of snow as well. The cold arrived earlier in December, followed by a good covering of snow. And then as the New Year arrived, we began experiencing one of those old-fashioned cold snaps that almost made it seem like old times.

Which sort of leads us back to the point about sledding. If sledding was bad during some parts of the year, when was it good?

In those days of yore when I was young and the weather was colder more often, sledding possibilities were many and varied. When we lived out on the farm, we’d trudge what seemed to be miles to an abandoned gravel pit adjacent to our farm and ride our sleds down the nearly vertical slopes.

Besides that, my parents enjoyed having bobsled parties. My dad put his hayrack on a bobsled running gear every winter, hooked up the tractor, and everyone scrambled on board, sitting on bales of hay and straw. Away we went down country roads and farm lanes with everyone having a whale of a good time. The kids hooked their sleds onto the back of the bobsled with ropes and hung on for dear life as the party enjoyed themselves, after which hot chocolate and coffee and my mother’s great desserts capped the evening off.

The Hill horizontal S

The Second Street hill, looking west. The road makes a right-angle curve to the left at the bottom of the hill where Second joins North Adams Street. These days, the road is paved with asphalt.

When we moved to Oswego, bobsled parties were things of the past, but sledding opportunities grew. There was the road off Ill. Route 25 down to our street, for instance. Second Street is still a fairly steep climb today, although it’s paved with asphalt these days and village snowplow crews keep it cleared and well salted.

In the days of my childhood, however, Second Street was gravel, we were in the township, and we were lucky to see a plow for a while after the snow stopped. As a result, the hill’s gravel surface got snow-packed and slippery. All the locals knew you could drive down the hill with reasonable safety, but that most cars and trucks couldn’t make it up the slippery surface, especially since motorists almost always needed to stop at the Route 25 intersection. So traffic on the hill was light when there was snow on the ground.

And us kids quickly realized it made for a great sledding opportunity. You could start at the top and speed down, and if skillful enough, make the sharp turn at the bottom to head south on North Adams Street. A quarter mile distance was not difficult to achieve.

Sledding course

The trick to ensure a long sled ride was making the curve at the bottom of the Second Street hill.

Occasionally, we’d help Mother Nature out a bit by sprinkling water on the street, especially near the top and near the old CB&Q tracks to give us a bit more speed. It wasn’t unheard of for us to build up a bit of a snow bank on the curve where Second met North Adams Street, to allow us to make the curve a bit easier. Very careful and skillful sledders could make the curve at the bottom and head south on North Adams, sometimes all the way to the driveway at my folks’ house.

Motorists, however, did not appreciate our work, and cinders were soon sprinkled to offer a bit of traction for motorists.

We weren’t the only ones who sledded on the streets, either. In an editorial during a snowy winter in December 1952, Oswego Ledger Editor Ford Lippold wrote:

“Several motorists have reported that they had close calls during the past few days with children coasting on the streets. It is hard for motorists to stop quickly even when moving at a snail’s pace on the icy streets of the village.”

One winter, we got a good snowfall, and then it warmed up enough so that a very wet snow covered it, after which it turned very cold once again. That left an icy crust that measured nearly an inch thick on top of the snow, and provided some of the best sledding ever. That winter, we marked out a course that ran from my best friend Glenn’s backyard diagonally all the way to Bill Crimmins’ house. It led to some remarkably speedy trips across the ice, although control was a bit problematical. The most dangerous stretch of the route passed under a grape arbor’s wires. All but one of us were careful to duck our heads as we sped down the course, but he lifted his head at just the wrong time to see if anyone was gaining on him. The resulting gash in his face, and its spectacular amount of blood, spelled the end of our sledding on that course for the rest of the winter.

1940 abt Hall, Levi House Main Street cropped

Nellie Wormley Herren stands outside her ornate home on South Main Street during the winter of 1940. Generations of local kids had great fun coasting on the hill behind her house, where the ground sloped steeply down towards the railroad tracks and the Fox River. (Little White School Museum collection)

There were other good sledding spots around town then, near Smith’s Pond, and in Mrs. Herren’s backyard off Main Street to name two off the top of my head.

Kids in Kendall County’s other towns enjoyed the same opportunities during those years of less traffic and fewer parental worries about whether their children were safe from the many challenges of modern life. I imagine almost anyone growing up in Plano or Yorkville or Newark during that era can name their favorite sledding spots, too. For instance, on Jan. 20, 1915, Marshall wrote in the Record about the good sledding on the Bridge Street hill—something that would be suicidal today with Bridge Street’s busy four lanes of traffic:

“While the coasting on the Bridge street hill has been fine and called out large crowds for several weeks, there were several accidents that lamed some of the young folks.”

So, yes, we really did have good sledding back in the day. Enough to establish a contrast so we knew when it was bad, anyway.

Leave a comment

Filed under entertainment, Environment, Fox River, History, Illinois History, Kendall County, Local History, Nostalgia, Oswego, Semi-Current Events, Uncategorized

Snowy winter days create their own sounds, smells, and memories

Despite the effects of climate change on our Illinois winters, it still gives me a warm feeling to sit here in my office, in the house my great-grandparents built as their retirement home, and watch the flakes drift down during an early winter snowfall.

Downtown, children and adults, all dressed in high-tech, down-filled, rip-stop winter clothing hurry along the sidewalks on their way to and from stores and doctors’ and dentist offices. Today’s clothing is lighter and more comfortable and autos and other pieces of necessary machinery are more dependable, but an Illinois winter’s cold, wind, and snow are constants that conjure up memories of winters and holidays past.

1914 Transition Wastington St. winter1914

You can almost hear the sleigh bells ring looking at this image of Washington Street in downtown Oswego about 1914 during an early winter snowfall. (Little White School Museum photo)

These days, I chiefly recall that era of decades past by its sounds and smells.

The sound of a small boy walking along a snowy lane with corduroy pants and five-buckle boots seemed unnaturally loud during a quiet early morning snowfall. Each step produced a “whoop-clink!” as first one and then another corduroyed leg noisily brushed against its brother with a rough-soft sound punctuated by the boot buckles’ musical jingle.

If the weather was right and the snowflakes were too, the tiny crackle each one made as it landed could be heard—if a sharp young ear was close enough to a winter coat’s arm.

Trudging along a country road, down a deserted village lane, or across a lonely farmstead, a winter day stroller had plenty of time to get off the road when traffic came from behind. The tire chains everyone used for traction in snow and on ice in those days before snowtires and front-wheel drive heralded each car and truck well in advance, as the chained tires squeaked and jingled and jangled through the snow.

1943 Oswego Winter

Snow’s building up fast in this photo snapped at Main and Washington in Oswego at the end of World War II. (Little White School Museum photo)

During a snowstorm, all the regular daytime sounds were muffled by the dense whiteness as it cascaded to the ground, allowing a keen ear to pick out familiar noises only now and then. Here the scrape of a shovel on a concrete drive or walk, there the joyful cry of a sledder on the way down a steep hill. But mostly, it was quiet as even the noisy English Sparrows sat hunched with their feathers fluffed for warmth, waiting for clear flying weather.

A snowstorm, if you’re paying attention, has a smell all its own. It is a sharp, clean scent that puts a person in mind of those stiffly white, freshly freeze-dried bed sheets our grandmothers once gathered in off their clothes lines in deepest January; an aroma that, I am quite sure, certain businessmen would sell their very souls for, could it be bottled and lined up on store shelves.

Out in back of the chicken house, large icicles hung down from the roof, looking for all the world like stalactites hanging from the ceiling of a prehistoric cave. There is a certain unique beauty in a clear, sharply tapering icicle. And nothing seemed quite so warm and wonderful as, while still grasping that freshly-born crystal clear icicle, going in the door of the chicken house, with its heavy smell of feathers and nesting straw complimented by the sounds of chuckling hens.

Heading back to the house pulling a brand new sled, magnificent in its varnished wood and red painted runners, that just the day before were carefully polished with a bit of steel wool and then waxed with the nub of an old candle, it was easy to imagine Arctic explorers or Eskimo hunters or even Sgt. Preston of the Yukon trudging alongside, sharing the adventures and hardships of a long, frozen journey fraught with all manner of dangers. Do you suppose a polar bear smells anything like a tail-wagging dog after she’s had a happy roll in the snow?

1945 abt Dobbin & sled

The Matile family pony, Dobbin, seems resigned to making the best of things after my sisters harnessed him to their sled.

After stamping and sweeping the snow from boots and snow pants, that wonderful kitchen all grandmothers seemed to possess, with all its special wintertime aromas, provided the perfect welcome. The cheery cookstove, all shiny white porcelain and dull black cast iron, warmed the room and provided, back behind and next to the wall, the perfect haven for a slumbering cat curled up in a cardboard box. Huge fresh-baked sugar cookies and fluted-edged molasses cookies, each with three small half-circles indented (creating dark brown smiley faces way before emojis were a gleam in someone’s digital dreams) cooling on the kitchen counter added a sweet smell of sugar and spice all their own.

The scarf was unwound, the hat and mittens removed, the thick winter coat unbuckled and unzipped. Damp mittens were put on the back of the cookstove to dry, adding a moist wool smell to the room.

Somehow, remarkable designs had appeared overnight on the kitchen windows, with mysterious, enigmatic, beautiful scenes outlined in shining frost. Who was this wintertime Picasso and why did he seem to do his finest work on the windows at Grandmother’s house? Jack Frost did it, was the unsatisfactory explanation.

In this day and age, a snowstorm’s quiet is punctuated by the muffled mechanized roar of neighborhood snowblowers and pickup mounted snowplows, but the delighted squeals of snowbound children, sentenced to frolic with sleds and snow saucers for the day, is still also there, provided you’re willing to listen hard and patiently enough.

IMG_1188.JPG

A winter’s snowfall erases all of Mother Nature’s mistakes, as this image of the Matile house proves.

The musical chinking of tire chains is mostly absent these days—at least in this part of the country—and the distinctive sounds made by walkers clad in corduroy pants and five buckle boots have given way to the sleeker sounds of nylon trousers and boots apparently modeled on those worn by Moon-walking astronauts. Unfortunately, our modern double-glazed windows have robbed poor old Jack Frost of his best medium; he must be content these days with fewer and fewer suitable single-pane windows—hardly what the old master deserves.

The constant, even after all these years, is the snow itself, creating a thick, soft white blanket that covers carefully manicured lawns and scarred construction sites alike after our infrequent blizzards during this era of warmer winters. But when those infrequent storms hit and for all our modem, efficient snow clearing equipment, the dense white of modern winter storms still slow our bustling suburban lives to an unwanted– but often secretly enjoyed–walk. The trick is to slow down and enjoy it for what it is.

 

 

Leave a comment

Filed under Environment, Farming, History, Local History, Nostalgia, Oswego

Visitor from the past would find a confusing modern farmscape

While development has taken a substantial toll on agricultural land here in Kendall County, there are still plenty of planted fields left for farmers to harvest this time of year. From the county’s congested tier of three northern-most townships, just take a drive west on Galena Road, or south on Route 47 or southwest on Route 71, and it doesn’t take long to leave tract homes and strip centers behind, and find yourself surrounded by fields that grow corn and soybeans, just as they have for generations.

It’s easy to think that our forebears would find the landscape on Route 47 down near Lisbon Center or on Grove Road south of Route 126 familiar. It’s rural; many of the farm homes are products of the late 19th century and early 20th century. There are even a few (very few) gravel roads to reinforce the feeling of stepping back in time.

But assuming we could crank up the Wayback Machine, and send Mr. Peabody and Sherman back to, say, 1870, to bring a farmer back for a brief summer visit to his future, he might find some similarities, but mostly he’d be struck by profound differences.

First and foremost, even if plunked down in a completely rural area, out of sight of any buildings, our farmer of the past would undoubtedly be struck by the odd uniformity of the agricultural landscape. Familiar, though unusually large and densely planted corn fields would stretch in every direction, but what, he would wonder, are those other row crops that seem to have bean leaves? And where in the world are the familiar fields of wheat, oats, barley, and rye? What’s happened to the pastures and the hay fields?

And where have all the fences gotten to? How on earth do modern farmers keep the neighbors’ cattle and hogs from eating growing crops with no fences to keep them out of the fields?

1890 abt Otto Johnson farm

The Otto Johnston farmstead in 1890 had a barn, a corn crib, and a chicken house, but no machine shed–the simple farm equipment of the era was stored in the barn and crib. (Little White School Museum collection)

That nearby farmstead looks odd, with no barn, and only some cylindrical metal buildings with conical roofs and one very large shed that looks as if it, too, is made of metal. And such a huge door it has. No cattle shed; no corn crib; no chicken house; no hog houses. The farmhouse lawn seems trimmed so neatly it’s almost unnatural, but where is the orchard?

Unlike our visitor from the past, today’s farmers operate in an either-or environment. They’re either grain farmers or livestock farmers. Our visitor from the past came from an era when every farmer grew both grain and livestock. Moreover, both were integral to the economic heath of every farmstead.

Grain was not only grown for market, like it is today, but was also grown for use on the farm to feed hogs, cattle, and poultry. Hogs and cattle were driven to market, meaning less grain had to be hauled over the abominable roads of the era. Poultry was kept for the eggs produced–which were traded for groceries in town–and used for meat on the farm and also to trade in town.

1947 July prob Russell Rink bailing

Russell Rink had plenty of business for his custom baling operation in East Oswego Township in 1947 when this snapshot was taken, since alfalfa, timothy, and other hay crops were common on area farms. (Little White School Museum collection)

The manure produced as a byproduct of feeding hogs, cattle, and poultry was, in turn, used to fertilize the farmer’s grain fields.

A variety of crops were grown every year, and the fields in which they were grown were rotated each year, with pasture or hay land part of the rotation so the land could lay fallow for at least a year with no crops leaching nutrients out of the soil. The Anglo Saxon root of the word fallow refers to the colors of pale red or pale yellow—the color of fields tilled but not sown with seed.

Soybeans were not part of that rotation until they were popularized in the 1930s by the U.S. Department of Agriculture. County agricultural agents instructed farmers in the fine points of their cultivation and harvest, and soon they became a popular cash crop—one probably unfamiliar to our visitor from the past.

2017 fenceless landscape

DeKalb County’s fenceless landscape is common on northern Illinois farms these days, With no livestock on farms, there’s no need to waste productive land with fence rows.

What happened to the crops with which our visitor was familiar? Where are the oats, the wheat, the rye and barley? Farmers not only specialize these days, but so do regions of the country. Illinois’ humid climate is not conducive to growing wheat, so its cultivation has migrated west of the Mississippi to drier the Great Plains. Oats were once necessary to feed the millions of horses that powered the nation’s farms and cities, and for on-farm livestock feed, needs that have largely disappeared today. So too have modern times sharply reduced the use of rye and barley.

Pastureland—where are the county’s pastures? Most have been plowed for cropland in the absence of livestock. The same with the hay fields that once covered thousands of Kendall County farmland acres. The sight of rolling stands of clover, timothy, and alfalfa rippling in the wind of mid-summer is largely a thing of our past that faded away with the livestock that once required them for food. It makes a person wonder what Timothy Hansen would think, the Norwegian immigrant who imported the nutritious forage grass named Phleum pratense to his farm in Virginia in 1721. So well did he conduct his campaign in its favor that farmers nicknamed the grass “timothy” in his honor. Where once timothy grew on virtually every farm, today its presence has dwindled, another victim of changes in farming.

Farm orchards, too, have largely departed leaving only memories of stands of apple, plum, pear, and cherry trees once prized for their abundant fruit. As have the dirt roads with which our farmer of the past would have been familiar. When studies were done in the early 20th century, it was found farmers’ cars and trucks got much better gas mileage on gravel roads, road maintenance costs were less, and wear and tear on vehicles was far, far less. And asphalt roads were far, far better than gravel roads in terms of damage to vehicles, mileage, and maintenance costs. So dirt roads have disappeared. Gravel roads, at least in most of Kendall County, have disappeared, too, because they’re expensive to maintain.

As our visiting farmer leaves to head down-time to his home, he is probably happy to get back to where farming makes some sense and where the parts of the landscape make cultural and economic sense to him. As for us, it’s another late autumn of taking life the way we find it in Kendall County.

Leave a comment

Filed under Architecture, Farming, History, Illinois History, Kendall County, Local History, People in History, Technology

Unintended consequences…

For some reason, there seems to be a lot of controversy connected with global climate change.

Well over 90 percent of climatologists say it’s proven science that us humans have greatly contributed to the warming of the earth’s climate since 1900, and even the big oil companies’ scientists told their bosses what was happening decades ago. In fact, there’s an interesting investigation going on right now where the attorneys general of several states are trying to determine whether Exxon misled the company’s investors about the issue.

But a lot of people still don’t buy the facts that have been laid out, mostly because those folks at Exxon didn’t only hide the facts their own scientists dug up from their own investors, but they also apparently bankrolled climate change denier individuals and organizations, muddying the waters for lots of us.

It’s not that hard to figure out what’s happening, though. Each recent year sets a new record as being the hottest on record, and individual months are regularly setting temperature records, too. But it’s not hard to find someone to dispute the fact of global climate change—although there aren’t a lot of them, the professional deniers are a pretty loud and determined bunch, once again proving muckraker Upon Sinclair’s dictum that “It is difficult to get a man to understand something, when his salary depends on his not understanding it.”

If you’re a seed catalog saver, you can get an easily understood look into what’s happening. Just look at how those hardiness zone maps keep changing. The zones where certain plants can grow keep steadily moving north, indicating average temperatures are continuing to rise.

Walleye

Walleye, one of Wisconsin’s most sought-after gamefish, are becoming rare in some of the state’s most popular resort areas, at least partly due to global climate change.

Up in northern Wisconsin, the change in the climate means some of the fisheries up there are changing, too. In the Minocqua area, largemouth bass, which is generally considered a warmer weather species, have begun to take over some of the lakes in that region. The Wisconsin DNR figures that the growing largemouth population is feeding on walleye fry, thus leading to a decrease in walleyes. And that’s bad for the resort industry up there because walleyes are a big, big draw for anglers. To try to do something about the situation, the DNR has banned keeping any walleyes caught for a five-year period, supposedly to give the species a chance to rebound against largemouth predation.

I’m pretty sure it won’t work. Those largemouth that are suddenly so prevalent aren’t there by happenstance; they’re there because the water’s warmer there now on average, making it a friendlier habitat for bass. Helping the walleye population by increasing their numbers through lack of angler harvest isn’t going to do a thing to cool off the water in Minocqua area lakes. But since the DNR is now prohibited from discussing climate change’s effects on Wisconsin wildlife, it’s going to be interesting to see how the subject is handled going forward. Because you can bet this is just the tip of this particular rhetorical iceberg.

When you think about unintended consequences, global climate change is this era’s prime example. When the Industrial Age got really going, I doubt anyone thought that burning all that coal and, later, oil was going to have a negative impact on the entire earth. Just like adding lead to gasoline, which was designed to make internal combustion engines run smoother and more efficiently, the ultimate impact was to inflict lead poisoning on several generations of Americans. The outcome of that was likely the spike in crime rates in the 1970s, according to some who’ve studied the topic. Banning leaded gasoline may well be the reason violent crime has been declining since the 1970s.

It’s when we fiddle with the earth’s ecology that those unintended consequences seem to have their biggest effects. The folks in Wisconsin are trying their best to do something about a process over which they have little control by doing something over which they do have at least a little influence, although it’s probably futile. It probably won’t comfort them to know that we’ve been messing with fish populations for generations, sometimes with negative implications that didn’t show up for decades.

German carp

German carp thrived after being stocked in the Fox River by the U.S. Fish Commission in the 19th Century.

The lowly carp is prime example number one of that. We take these ubiquitous rough, annoying fish for granted these days. But they only got in our rivers and creeks because the U.S. Government put them there in the first place, hoping to provide a useful, marketable species to benefit everyone.

So they imported a bunch of them from Germany with plans to stock them in streams the next year. They were considered so valuable that they used the reflecting pool on the Mall in Washington, D.C. to house them over the winter. Then in the spring they stocked them all over the place.

I’ve already written about the general reaction to this bit of ecological sabotage, noting the reaction was far from unanimously positive. But, as luck would have it, carp were stocked at about the same time streams in long-settled parts of the country were being stressed beyond their limits with almost unbelievable amounts of pollution, from raw human and animal waste to manufacturing byproducts, from coking mill waste to waste from coal gas plants. The effect of chemical poisons on streams was amplified by increasing amounts of agricultural runoff that was containing more and more silt as unwise farming practices created erosion.

As their gravel-bottomed spawning grounds were covered with silt the oxygen content of water in polluted streams drastically declined due to huge increases in chemical and human waste, game fish populations catastrophically declined.

Enter those carp. They were far more adaptable to filthy water conditions and positively thrived on the muddy stream bottoms that were being manufactured by a near-total lack of any controls on pollution. And because they liked the conditions they were introduced in, they thrived—and therefore were blamed for creating the conditions rather than being lauded for making use of them, much like those largemouth bass up in northern Wisconsin are being blamed today for decreasing walleye populations.

A classic example of blaming the messenger—carp—for stream quality happened on the Rock River in southern Wisconsin back in the 1970s. The Rock has several dams up there creating lots of recreational fishing at Beloit, Janesville, and other towns along the river’s course. By the ‘70s, some of those impoundments had gathered a lot of sediment and silt from agriculture runoff, and while carp were flourishing, gamefish were not. So the Wisconsin Department of Natural Resources decided to try poisoning the all the fish in one of those impoundments, the idea being that without carp rooting around the bottom and creating silt-laden water that gamefish didn’t like.

So that’s what they did. And it worked. The impoundment was cleanses of carp—and all the other fish as well, and that had the effect of clearing the water right up. Residents living there were ecstatic—you could actually see the bottom again!

But getting rid of the carp didn’t get rid of the sediment, which was extremely rich in nutrients thanks to runoff from all the farm fields through which the river ran. And as soon as the water clarified, sunlight finally got down to the bottom, creating a veritable algae explosion. The stuff grew inches thick on the surface, died, and sank to the bottom where it decomposed, sucking whatever oxygen still remained out of the water, creating a smelly, slimy mess. Which made residents far from ecstatic. It took a frantic DNR quite a while to get the situation stabilized and to try to reverse it because the agriculture interests were not interested in doing what needed to be done to reduce runoff from their fields.

The main point the ecology movement tried to get across to people when it got started is that almost everything in the natural world is connected one way or another. And sometimes, because much of the time we neither understand nor recognize them in the first place, those connections come back to bite us when we mess with one part or another without careful consideration first.

Leave a comment

Filed under Business, Environment, Frustration, Government, History, Science stuff, Semi-Current Events, Technology, Uncategorized

A tale of two towns…

Just got back from our annual early October trip up to the Northwoods to close our fishing cabin for another season.

My buddy, Paul and I, have known each other for more than 60 years, having met in third grade when my family moved off the farm and into town. Paul, I, and my wife Sue pooled our resources back in 1972 and bought five acres of wild land along the South Fork of the Flambeau River up in Price County, Wisconsin. Camping got old after six or seven years, so in 1980 we bought a fishing cabin a couple miles north of Park Falls—then, as now, Price County’s largest municipality—on Butternut Lake.

2017 10-10 Paul fishing

The sunset on Butternut Lake on Oct. 10 proved to be a spectacular one as we attempted to invite a few walleyes for supper.

We open the cabin each spring so as to be ready for opening day for walleye season on the first Saturday in May. And since it’s a three-season fishing cabin, we close it down for the winter each autumn, generally around Columbus Day.

As I sat out fishing with Paul as our annual autumn trip drew to a close, I started thinking about the big changes we’ve seen in northern Wisconsin, as well as the changes in my hometown of Oswego here in Illinois’ Fox River Valley. In both cases, those changes have been profound, generally in a good way for Oswego but not so much for Park Falls.

Park Falls, like most of the municipalities in Price County, was established during the lumbering boom of the late 19th Century, growing faster than its neighboring villages when a paper mill was built there. It was not only the industrial center of the surrounding hinterland, but was also the agriculture market center for nearby farms, which were mostly dairy operations. Today, the paper mill is still busy, turning pulpwood harvested from the surrounding managed forests into paper.

The town’s businesses and industry led to construction of a large stock of housing, smaller worker’s cottages for industrial workers and retail employees, with larger homes built by executives and successful merchants.

Paper Mill

The Flambeau River Papers mill still dominates Park Falls’ downtown while providing jobs for residents.

But like so many small towns in overwhelmingly rural areas like northern Wisconsin, Park Falls has seen its population decline sharply over the years. When we bought our fishing cabin back in 1980, Park Falls’ population stood at its historic peak, 3,192. The town’s downtown sported a stock of substantial brick storefronts that housed two grocery stores and a fair variety of retail businesses.

That same year, Oswego’s population was reported by the U.S. Census Bureau at just slightly below Park Falls’, 3,021. Oswego was still the market town for the surrounding agricultural hinterland, but was rapidly changing into a suburban bedroom community. Residential and commercial development took a breather during the 1980s, but then in the 1990s it began again, surging strongly into the early 2000s. In fact, during that era, Kendall County, in which Oswego is situated, became (in percentage terms) the fastest growing county in the entire nation.

Meanwhile, Park Falls and Price County were steadily losing population. Young people graduating from high school found decreasing opportunities for economic advancement, leading to a population drain.

2017 10-6 Fall color at the lake.jpg

Autumn color was hitting the peak on Oct. 6 when I snapped this shot down towards Butternut Lake.

The paper mill continued to provide jobs, but increasing automation meant there were fewer of those available. Then in 2006, the factory closed, shocking the entire community. But with private and governmental economic cooperation, it reopened after a few months, and has continued operating since. In addition, St. Croix Rods opened a manufacturing plant in Park Falls for high-end fishing equipment, and later, the Weathershield company opened a state-of-the-art window factory in town, providing more relatively good-paying jobs.

Even so, the community’s population continued to decline. The 2016 population estimate for Park Falls was just 2,292, a decrease of nearly 30 percent since 1980.

In comparison, Oswego’s population surged during that same period, growth fueled by northern Illinois’ powerful economic engine. In 1990, Oswego’s population had grown, but not sharply, to 3,879. But then the frenetic growth of the 1990s and early 2000s hit and by the new millennium Oswego’s population had grown to 13,326. The growth explosion continued through the 2000s, despite the Great Recession of 2008. By 2010, the village’s population stood at an astonishing 30,355. Between then and 2016, population went up another 10 percent or so to an estimated 34,571.

2008 Oswego look E from W bank

These days, there are more traffic signals on Oswego, Illinois’ Washington Street than in all of Park Falls, Wisconsin—one of the prices residents pay for the community’s growth.

Not sure what all this proves, other than the old cliché that the three most important factors contributing to real estate values is location, location, and location.

Park Falls’ population declined by nearly 30 percent during the same period when Oswego’s population grew by 10 times, mostly, but not entirely, based on where the two towns were situated, Park Falls largely isolated in Wisconsin’s Northwoods, Oswego adjacent to the Chicago suburban economic powerhouse.

Those of us who have lived through Oswego’s growing pains often grumble about the area’s extreme changes. But all things considered, it’s been a lot better watching a community grow and prosper rather than slowly evaporate as its young people leave for places where there are opportunities to make a successful family life.

 

 

 

1 Comment

Filed under Business, Environment, Fox River, History, Illinois History, Kendall County, Local History, Oswego, Semi-Current Events