se, t test lengtersected

    test breadtly at t of greatest depth,

    notanding t tline of

    treme length were

    got by measuring into to myself,

    t  to t part of the ocean as well as

    of a pond or puddle?  Is not t of

    mountains, regarded as te of valleys?  e kno a hill

    is not  at its narro part.

    Of five coves, three, or all which had been sounded, were

    observed to e across ter

    tended to be an expansion of er hin

    t only ally but vertically, and to form a basin

    or independent pond, tion of two capes she

    course of t, also, s bar

    at its entrance.  In proportion as the cove was wider

    compared s lengter over the bar was deeper compared

    in the

    cove, and ter of the surrounding shore, and you have

    almost elements enougo make out a formula for all cases.

    In order to see his experience,

    at t point in a pond, by observing tlines of a

    surface and ter of its shores alone, I made a plan of

    e Pond,  forty-one acres, and, like this,

    , nor any visible inlet or outlet; and as the

    line of greatest breadt breadth,

    e capes approace bays

    receded, I ventured to mark a point a s distance from tter

    line, but still on test lengt.  the

    deepest part o be  of till

    fartion to which I had inclined, and was only one

    foot deeper, namely, sixty feet.  Of course, a stream running

    the problem much more