Former Bike Rider Reminisces

As a former bike rider, I still remember how to balance a two-wheeler and sometimes venture out into the world to remind myself what it feels like to roll along the local pavements.

This morning I had an appointment over on Solano Avenue, a couple miles from home. I rode over. Then afterward, I rode up Solano and wound my way into the hills. Just to remind myself what that uphill trudge feels like.

I got to the top of Los Angeles Avenue, which is short and no big deal though it has a semi-steep pitch at the end. I was taking it very easy and riding in my lowest low gear.

Turning uphill on Spruce, perhaps the most popular way into the hills on the north end of Berkeley, another rider appeared alongside me. He was going faster than I and was visibly fitter, too. We said hi and wished each other a good ride, and within a few seconds he was pulling away. As I got ready to turn uphill on Keith Avenue, a quiet and steepish side street, the Other Cyclist was maybe 100 feet ahead of me.

I stayed in my low gear up Keith and crossed Euclid Avenue. Then I started a sort of side-step up the ridge toward Grizzly Peak Boulevard. From Keith, which has a gentle grade east of Euclid, I turned on to Bret Harte Way, which probably has a 16 or 17 percent grade (and grade is a measure of a road’s slope: 10 percent means a 10-unit vertical change for every 100 linear units; 10 feet in 100 feet, or 10 meters in 100 meters. Given my out-of-shape linebacker physique, which my legs have to carry up these hills, I regard 10 percent as pretty steep. In Berkeley, Marin Avenue climbs into the hills with gradients of roughly 20 to 30 percent, and the steepest street I’ve heard of in town is said to be 31 percent. That’s another way of saying darn near impossible for mere mortals and former bike riders).

At each corner, I tried to turn uphill. The way it worked out, I alternated between steep eastbound pitches like Bret Harte Way and flatter south-trending pieces like Cragmont. And so it went, up Bret Harte Road (steep again, and different from B.H. Way), Keeler Avenue (flattish), Twain Avenue (steep), Sterling (gentle), Whitaker (steep), Miller (easy), and Stevenson, a short street that I knew topped out at Grizzly Peak. And that was as far up as I intended to go.

I finished the climb and turned left on Grizzly Peak. As it happened, I was about 100 feet or so in front of the guy who had just passed me down below. We waved at each other, and I called out that he could have taken the short cut, and he laughed. It was a lovely piece of symmetry in a short ride into the hills, but the neatness of the coincidence made me want to try to account for it.

So here’s some arithmetic. The corner of Keith Avenue, roughly where the Other Cyclist passed me, is at an elevation of 499 feet if online sources are to be believed. The corner where we met again is at 1,082 feet. So both of us climbed 583 feet. Now, how far did we ride in linear distance? Again using an online tool–Gmaps Pedometer, which you ought to try if you haven’t already–my ride was 1.21 miles. His: 2.47. That’s another neat coincidence: His route being twice as long and the net climb being the same, his net grade (4.5 percent) is half of mine (9.2 percent). He also had to maintain an average speed roughly double mine, which would have been no problem since I was probably poking along at about 5 mph or less when the road got steep.

So those are the numbers. Interesting, but they don’t quite sum up that moment of delight when I saw the Other Rider again.

News from the Road: Chase County, Kansas

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On the recent Chicago-Berkeley peregrination, we stopped in Cottonwood Falls, Kansas. One draw is the nearby Tallgrass Prairie National Preserve, in the Kansas Flint Hills. It’s beautiful country. The town itself has a reputation as a well-preserved prairie village. It’s the county seat, and the courthouse is said to be the oldest still in use in Kansas (or west of the Mississippi, depending on who you believe). Broadway, the main street stretching north from the courthouse, is brick-paved. It is bordered by some handsome old buildings, including a hotel said to have a decent restaurant. We stopped for lunch at the Emma Chase Cafe and had burgers and fries; sweet-potato fries, in my case; never had them before.  

We picked up the local paper, the Chase County Leader-News, which ran the following story at the bottom of the front page on April 9. The story never says so–the locals must just know it–but the R3 Energy plant at the center of this incident is using chicken fat (among other things) as a raw material for biodiesel fuel. I had never thought of chicken fat that way before (a story earlier this week in the Arkansas Daily Gazette mentions that Tyson Foods, a big chicken processor, has a renewable energy group and is building a plant in Louisiana “to make high-grade biodiesel and jet fuels from Tyson-produced nonfoodgrade animal fats such as beef tallow, pork lard, chicken fat and greases.” I am way behind on my alternative energy news).

Six months before the incident, the Emporia Gazette ran a rather long article on the new biofuels plant in Cottonwood Falls. It was put up by a local family looking to get into a new business. It was a win for everyone–until the chicken fat spill.

R3 cleaning up spill

City Utility Supervisor
informs council of
chicken fat spill at R3

Jerry Schwilling
Chase County Leader-News

City Utility Supervisor Ron Lake informed the Cottonwood Falls City Council at its Monday, April 6, meeting that he had discovered a large amount of chicken fat at the city’s sewer lagoons Friday, April 3.

The chicken fat had run through the sewer line from R3 Energy to a lift station and from there onto the ground around the lift station.

Lake said when he discovered the chicken fat he asked R3’s Mike Swartz about it and Swartz said it was chicken fat that had been spilled at R3.

Swartz said Tuesday, April 7, that the spill had occurred when a truck was off-loading at the plant. The truck’s equipment, Swartz said, had malfunctioned spilling the chicken fat on the ground in the plans off-loading catchment area.

That area is designed to catch any spill and divert it either to the plant’s lagoon or the city’s lagoon. The decision was made to divert the spill to the city’s lagoon, Swartz said.

However, the lift station on the sewer line malfunctioned and the chicken fat spread on the ground around the lift station instead of going into the lagoon.

Swartz said the chicken fat was biodegradable and posed no ecological threat.

Lake told the council that he was required by the state to report the spill and to have it cleaned up.

Lake said that Swartz told him the spill had occurred on March 26. R3 did not report the spill to the city, Lake said.

Swartz said he reported the spill to two city employees the day it occurred and was told that Lake was not available.

R3, Swartz said, was having the lift station steam cleaned Tuesday, April 7, and had contracted a skid loader to pick up and dispose of the chicken fat on the ground at the city’s lagoons. He said he expected the clean up to be completed by the end of the day, Tuesday, April 7.

The council directed [city attorney?] North to send R3 a letter asking R3 to clean up the spill in the next seven days or the city would contract to have it cleaned up and bill R3.

The council also asked North to look into the creation of an ordinance to deal with any future spill.

Bike Crashes, Mapped

Russell Neches, a blogger in Davis, California, produced a beautiful and compelling map of bike crashes in the city over four years, 2004 through 2008. He also mapped data from all traffic accidents in the city, including those that did not involve bicycles. The map represents high-accident areas in red, as hot zones. Areas with a lower incidence of accidents are depicted in cooler yellow, green, and blue. The purpose of the exercise is more than a flat informational report. Neches says in an accompanying blog post:

“In particular, this is map is intended to examine bicycle accidents. I hope people will look at this map, and think about how they behave on the roads, weather on foot, on a bicycle, or in a car. How you behave on the road has direct, and sometimes dire, consequences for you and for other people.”

Watching Water

I’ve become preoccupied the last two or three months with the level of water in California’s reservoirs. If you’re inclined to, here’s where you can join in the fun: The state Department of Water Resources’ California Data Exchange Center. The cliche to describe a collection of information like this is “treasure trove.” For example, here’s one report that I’ve taken to taking a look at just about every morning: The Sacramento/San Joaquin Daily Reservoir Storage Summary. It’s a quick look at about three dozen state’s biggest storage facilities: how much water they’re holding, how many acre feet have flowed in or out in the past day, and–especially interesting–how much water they hold compared both to the average for this date and to the amount held a year ago.

There’s a story in the numbers, though I’m still puzzling out what it is. For instance, the state’s current drought is not a drought everywhere. Although rainfall and the mountain snowpack are generally below average, some reservoirs hold more than average for this time of year and much more than they did a year ago (which was an even worse year, precipitation-wise). But the numbers are just one dimension of a complicated picture. All that water has a lot of work to do. We count on it not just for irrigating the Central Valley farms and bringing drinking and lawn water to the citiies and suburbs, but for providing electricity, too. And in recent decades, the state and federal water managers have even been made conscious of another function the water might perform: preserving wildlife–especially the once-magnificent salmon runs in the Sacramento and San Joaquin watersheds.

The I-5 Trivia Files: Self-Interview

Q. So what’s the topic?

A. I was thinking about driving up Interstate 5 and all those passes you cross.

Q. Yeah?

A. It’s a flat valley drive until you get to Redding. That’s 200 miles from the front door. Then there’s some climbing and lots of twisty parts around Lake Shasta. And then you go up some more, past Dunsmuir.

Q. Dunsmuir?

A. Dunsmuir’s about 50, 55 miles north of Redding. LIttle town on the upper part of the Sacramento River. Popular place during trout season. Elevation up there is about 2,500 feet.

Q. What then?

A. Mount Shasta. You can see the mountain way down in the Valley. Once we saw it clear down by Dunnigan, which is 180 miles down the road from the peak. But when you get into the hilly country around Redding, you lose sight of the mountain until you’re much closer. And then, bang, there it is.

Q. Big.

A. Very big. Very impressive. A 14,000-foot peak standing out there pretty much by itself. Anyway, the highway goes up past the town of Mount Shasta, which sits on the eastern base of the mountain. At about 3,500 feet. Then I-5 goes up crosses Black Butte Summit. About 3,900 feet. That’s the first real pass, maybe 50 miles south of the Oregon border.

Q. Black Butte?

A. It’s a volcanic cone of some kind. Next to Mount Shasta, it’s the most remarkable sight along that part of the road.

Q. OK. You’re still going north. What’s the next pass?

A. Well, the road loses some elevation first. You go through Weed, which is mentioned in passing in “Of Mice and Men,” the Steinbeck story. It’s a place Lenny and George had to leave before they landed in the Salinas Valley, where the story takes place. Then you go through Yreka, which ought to have a bakery because it it did you’d have a good palindrome. The road goes right up after you pass Yreka, up Anderson Grade. There’s a nice view of Shasta to the south, and somebody put a dragon sculpture along the highway there. You climb up to Anderson Grade Summit. Maybe 3,100 feet.

Q. Not a big deal?

A. Well, it’s steep coming up from Yreka, and the road winds, and there are plenty of slower trucks up there, and then the road plunges down toward the Klamath River. There’s an exit right along the Klamath with a rest area. Good place to stop, though I only remember doing it once.

Q. Still in California.

A. For a little while, maybe 10-15 miles. The road goes up and down for a while, you pass a weigh station, and then you start climbing again. The last town in California is called Hilt. Milepost 796, I think. And then you’re on the Oregon border.

Q. How far from home?

A. About 320 miles. That climb that starts in California is the Siskiyou Summit climb. That’s two syllables — SISK-you.The summit is the highest point on I-5, 4,300-some feet. Doesn’t sound that high — all the well-known passes in the Sierra Nevada are in the low 7,000 to 10,000-foot range. But Siskiyou is far enough north and gets enough wet weather in the winter to make it a barrier. I know plenty of people who’ve gotten stopped there during snowstorms. Or at least a couple.

Q. How about you?

A. Never. We always had great luck driving through there in winter. The road always seemed to be dry and clear when we went through on our way up to Eugene.

Q. Where’s the road go next.

A. There’s a steep drop with a couple runaway-truck ramps down to the town of Ashland, where the Shakespeare Festival is. Elevation there is probably 1,500 or 1,800 feet. Then you’re in a valley through Medford, the big town in the region. Then you noodle around through Grants Pass before you come to the three summits.

Q. Three summits?

A. Well, you hit them one right after another. I always tried to keep the order straight. Northbound, I think you hit Sexton Mountain first. Then … Stage Road, I think. And last … Smith Hill. I think the last is the highest, about 2,000 feet. Then there’s a little break crossing a valley, and then you hit a fourth pass, Canyon Creek, which is also not very high but has a long, long descent to Canyonville and then the Seven Feathers Casino.

Q. How many times have you done this drive?

A. Over the last four or five years maybe 20, 25 times. Enough to get to know it. That’s the last named pass that I know of, Canyon Creek. Though there are rivers.

Q. That’s a different species of geographic phenomenon. Which ones?

A. Well, from the south, you’ve got the Sacramento, which you cross and recross half a dozen times from Red Bluff up to Dunsmuir. Then the Shasta, which is a tiny thing, and maybe the Little Shasta. The Klamath. Bear Creek between Ashland and Medford; has enough water running to be called a river. The Rogue. The South Umpqua and the North Umpqua. The Coast Fork of the Willamette, and the southern end of the mainstem Willamette just as you get into Eugene. Maybe other rivers. But a whole bunch of creeks, too. One name that comes to mind: Jumpoff Joe Creek, north of Grants Pass before you go up Sexton Mountain.

Q. Creek names are a whole other subject.

A. True. We’ll get to them later.

Top of Mariposa

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At Mariposa and Utah streets, west flank of Potrero Hill. On clear nights, I always want to try and capture the glow that lingers over the peaks to the west after sunset. It’s not to be captured, or not by me, at any rate. The profusion of wires at the corner was a consolation prize and the best I can do by way of marking the day.  

Pandemic, the Game

If you happen to spend time with your adult-age kids, as we occasionally do, they may share some of their enthusiasms with you. Our older son, Eamon, and his wife, Sakura, have become avid fans of the San Jose Earthquakes and taken us to several games. I realize that I like non-American football. I’d be up for seeing some rugby and footy, too.

Our younger son, Thom, is into what I’ll call new-wave board games. Ticket to Ride, a railroad-building game. Carcasonne, a sort of territory-acquisition game. Power Grid, the game of electrical utility domination.

He also introduced us to Pandemic. It’s different from most board games in that players cooperate to head off a series of global disease threats. The game requires consideration of what threats deserve immediate attention and a lot of planning for how to respond. We played the game once. Sadly, we were unable to prevent the world from being overrun by multiple deadly disease outbreaks.

Snow Again

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Here’s what that Friday morning snow in Mount Shasta looked like. Not sure when it started, but it was over by 10 a.m. By noon, it was turning into a nice day. I spent the afternoon on a ranch north and east of town, and it was dry and warm there.

Snow

Drove up to Mount Shasta last night and didn’t get in until very late. I’m up here to do a radio story on a recent Nature Conservancy land purchase that aims to restore some valuable salmon spawning streams up here. But the news right now, as I look out my window onto Mount Shasta Boulevard, is that there’s a steady and from a lowlander’s perspective pretty heavy snow falling. I don’t think it will last long, but I didn’t really expect to see it. It’s beautiful, and I’m hoping that it won’t get in the way too much of my handling a tape recorder and microphone. Pictures later.

Mixed Marriage, Revisited

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I’ve written about this grave before. About five years ago, my dad and I spotted it while visiting the Mother Jones Memorial in a union miners’ cemetery just outside Mount Olive, Illinois. The Cardinals and Cubs logos got our attention, of course. Last week, I stopped there again with my brother Chris and son Liam. After we got done gazing upon Mother Jones’s final resting place, we went across the road to the Kalvin grave. Chris noticed a metal capsule on the back of the stone, which happens to be the side facing the road. It has a hinged cover. Beneath the cover is what I take to be a picture of Steven and Verona, some time during their long marriage and lifelong residence in Mount Olive. A date is noted below: their wedding day. For a little historical baseball perspective, Steven Kalvin was born three years before Wrigley Field opened (and five years before the Cubs made it their home); Verona Kalvin was born the same year the last Yankee Stadium opened. They were married three seasons after the Cubs’ last pennant.

Verona, here’s hoping you don’t have to wait too much longer.

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