adient of 250 feet to the city boundary at
Eustace bridge, upper Leeson street, though from prolonged summer drouth
and daily supply of 12 1/2 million gallons the water had fallen below
the sill of the overflow weir for which reason the borough surveyor and
waterworks engineer, Mr Spencer Harty, C. E., on the instructions of
the waterworks committee had prohibited the use of municipal water for
purposes other than those of consumption (envisaging the possibility of
recourse being had to the impotable water of the Grand and Royal canals
as in 1893) particularly as the South Dublin Guardians, notwithstanding
their ration of 15 gallons per day per pauper supplied through a 6 inch
meter, had been convicted of a wastage of 20,000 gallons per night by
a reading of their meter on the affirmation of the law agent of
the corporation, Mr Ignatius Rice, solicitor, thereby acting to the
detriment of another section of the public, selfsupporting taxpayers,
solvent, sound.

What in water did Bloom, waterlover, drawer of water, watercarrier,
returning to the range, admire?

Its universality: its democratic equality and constancy to its nature
in seeking its own level: its vastness in the ocean of Mercator's
projection: its unplumbed profundity in the Sundam trench of the Pacific
exceeding 8000 fathoms: the restlessness of its waves and surface
particles visiting in turn all points of its seaboard: the independence
of its units: the variability of states of sea: its hydrostatic
quiescence in calm: its hydrokinetic turgidity in neap and spring tides:
its subsidence after devastation: its sterility in the circumpolar
icecaps, arctic and antarctic: its climatic and commercial significance:
its preponderance of 3 to 1 over the dry land of the globe: its
indisputable hegemony extending in square leagues over all the region
below the subequatorial tropic of Capricorn: the multisecular stability
of its primeval basin: its luteofulvous bed: its capacity to dissolve
and hold in solution all soluble substances including millions of
tons of the most precious metals: its slow erosions of peninsulas and
islands, its persistent formation of homothetic islands, peninsulas
and downwardtending promontories: its alluvial deposits: its weight and
volume and density: its imperturbability in lagoons and highland tarns:
its gradation of colours in the torrid and temperate and frigid zones:
its vehicular ramifications in continental lakecontained streams an