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It's not that boats didn't chance the big river ... they did, but many boats and cargoes were lost because the St. Lawrence is shallow in spots and river shallows have a tendency to move around a lot.From the source, Lake Ontario, 246 feet above sea level, the St. Lawrence wends it's way 186 miles to Montreal, 20 feet above sea level. The river drops 226 feet in 186 miles ... about one foot 2 and a half inches per mile ... on average. That's not to say there aren't placid areas where the deep places are smooth and slow ... but those areas make the drops longer and steeper.The Lakes vary in depth as much as 20 feet on a continuous 26 to 39 year cycle. The extra water goes on top ... some people ask why the bottom doesn't get deeper? The bottom stays where it's at ... the extra water goes on top. Well, except for glacial isostatic readjustment. That's so slow we really don't have a way to measure it. Trust me on this.OkOkOk ... the weight of glacial ice pressing down on the earth's. As it turned out, I noticed that Liz had also come in--she worked in the lab adjoining mine--to pick up a few papers she needed to read, I found out later. So, it seemed only natural for me to stop in and say hi.We ended up staying and talking for hours. Not about anything of real consequence or the typical exchange of common interests--just talking about past experiences, current problems, and future ambitions. It was as if we already knew each other well enough to skip all the formalities and requirements of 'getting to know each other.'That became the pattern for the next few weeks. I'd drop by once or twice after work (I rarely scheduled any experiments past six or seven; she had no such inhibitions), and chat with her while she was working in the lab. The conversations usually ran to how she was doing in her classes, commiserating on how few results both of us were getting in our experiments, but rarely anything intensely personal.During those weeks, it gradually occurred to me.
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