Tidal currents in a country like the UK, with a very high tidal range and a (for use of a better word) crinkly coast, are usually formed by a difference in tide heights around a peninsular or area of coast line - or when flow is constricted through narrows in marine topography. The tidal flow then runs to re-equilibriate that imbalance. So yes, in this country they can often be parallel to shore, or at least very close to it. But tidal streams also appear for other reasons, salinity gradients in the mid-Pacific for instance. The 'underwater windmill' is still the basic tenent of the tidal stream world (w.marineturbines.com or w.swanturbines.co.uk), simple and effective. But the power of the tide is not to be underestimated. There has been more than one prototype that has been deployed and effortlessly decimated by the next tide. Great power to be harnessed, but greater almost needed in the harnessing. GB