Ontario Sessional Papers, 1913, . 20 Sandy Oct 14 ;).5 The figures in the columns headed Ranges show the riseand fall of the tide on thedays of greatest and least range in the month. - * Range of tides following a soutli wind with a velocity of Id to 20 miles an Approximate ranges. 1913 INVESTIGATIOXS AT JAMES BAY 42a TIDES AND OF TIDAL OBSERVATIONS IN THE ESTUARY OF MOOSE RIVER, 1913. Site of Gauge. Spring Tides. Neap Tides. Date. Ranges. Mean. Date. Ranges. Mean. Shears Beacou Moose Factory Apr. 24 May 13 Ma
Ontario Sessional Papers, 1913, . 20 Sandy Oct 14 ;).5 The figures in the columns headed Ranges show the riseand fall of the tide on thedays of greatest and least range in the month. - * Range of tides following a soutli wind with a velocity of Id to 20 miles an Approximate ranges. 1913 INVESTIGATIOXS AT JAMES BAY 42a TIDES AND OF TIDAL OBSERVATIONS IN THE ESTUARY OF MOOSE RIVER, 1913. Site of Gauge. Spring Tides. Neap Tides. Date. Ranges. Mean. Date. Ranges. Mean. Shears Beacou Moose Factory Apr. 24 May 13 May 22 .Tune 6 June 20 ,Iuly 6 .July 19 Apr. 14 May 17 May 29 June 12 June 29 July 16 July 31 \i INTERVALS FOR THE ESTABLISHMENT OF THE PORT, Date Locality. F. & * The interval between the moons crossing the meridian and the time of highwater at full and change, , on the days of new and full moon. This is, on these days,approximately the same interval after midday. t If not an error, this is three hours after the normal time. 42b REPOET OF T. & X. (). EAILWAY Xo. 71 Tlie average interval for the vicinity of Moose Factory is three hours ten average for the vicinity of Ship Sands is 2 hours 25 min. The interval isabout one hour on the coast near Cockispenny. Spring tides usually occur atMoose Factory two days after the new and full moon. This is expressed by thelocal saying, The spring tides come with the 5 oclock tides. The tides first strike the south shore of James Bay at Cockispenny Point, andtravel both west and south-east from there. High water occurs at Moose Factoryjust about an even two hours later than on the coast. Practically the same differ-ence in time is obtained whether the time
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