Yes, a crank was all it needed to start.

I averted my eyes while my friend typed in her password.

This was a day almost fifty years since the time I was supposed to run in the 4 by 100-meter Olympic relay. I was standing on the track in the imposing, empty Olympic Stadium in Berlin. […] I walked down into the well of the vast, brooding stadium, and then along the backstretch of the red clay running oval.

Mr. Ralph Abercromby has made special observations on the upper wind currents over the equator in the Atlantic Ocean. … With respect to the general circulation of the atmosphere we know that the surface trades either die out at the doldrums or unite into one moderate east current; that the low and middle currents over the doldrums are very variable, but that the winds at these low and middle levels, 2,000 to 20,000 feet, come usually from the southeast over the northeast trade, and from the northeast over the southeast trade, and that the highest currents—over 20,000 feet—move from east over the doldrums, from southwest over the northeast trade, and from northwest over the southeast trade.