Henry C. Adams

Capitolo 32

it is to contend effortless that it won't be then more impure than
water of storm that is permitted to be low in hinterland
brooks during heavy rain, the aforesaid sentimentalists
you/he/she can implore on a lot of possibilities of serious results. As far as
possible the files should point out the course taken from afloat
starting from the outfall to tall water and to every regular,
now later on the tide of decline, as to low water and
every time on the tide of flood. However it is not from some means,
necessary that they should be I taken in this or some particular
orders, because as the height of the tide every day varies a
observation taken to tall water that one day directly is not
comparable with one taken a hour later tall water the next one
day, and while perhaps relatively the greatest amount of
information can be gleaned by a series of observations taken
to the same state of the tide, but on tides to differ
heights, every observation still tells its his/her own history and
services an useful purpose.

Deep and afloat crafts of surface should be used concomitantly
you show the effect of the wind, the direction and strength of what
you/he/she should be noticed. If it seems that with a wind of on-beach
afloat particles would go adrift to the beach, while to protect will be
necessary before sewage is low. The crafts should be
succession until possible, but at least up to that the turn of
the tide--that is to say, a craft put in to or near tall
water should be followed until the tide you/he/she has turned to or
low and near water, and one put in to low water you/he/she should be followed
up to that after tall water. In all the water references low the
height of the tide dates it is that of the tall water and precedent.

The time to that the current turns relative to tall and low
you sprinkle to some place you/he/she will be found to vary with the height of the
tide, and all the information got on this point you/he/she should be
drawn on square paper as shown on Fig tree. 10 that they represent
the result of observations taken near the estuary of a great