Water resources of the Penobscot River basin, Maine . /i ^ / ^ ^ p West BranchMattawamkeagEast Branch. >Mat 1 r^ ^Wa f A /^ ^-^- 1 // J^ A ^ r lattawann, ea, /: _^^ / ^ ;/ 7 /^ Malta wamkeagEast BranchWest Branch i l/. y A h ^w. b -^ ^ ? DIAGRAM SHOWING STORAGE MASS OF SEVERAL TRIBUTARIES OF PENOBSCOT Rl\discharge for West Branch of the Penobscot has been corrected for storage; other figures are as obsi EFFECT OF PRESENT STOEAGE OK PLOW. 201 unit discharge of the Piscataquis at Foxcroft is greater than that ofthe other tributaries of the Penobscot here considered, it is probablethat th
Water resources of the Penobscot River basin, Maine . /i ^ / ^ ^ p West BranchMattawamkeagEast Branch. >Mat 1 r^ ^Wa f A /^ ^-^- 1 // J^ A ^ r lattawann, ea, /: _^^ / ^ ;/ 7 /^ Malta wamkeagEast BranchWest Branch i l/. y A h ^w. b -^ ^ ? DIAGRAM SHOWING STORAGE MASS OF SEVERAL TRIBUTARIES OF PENOBSCOT Rl\discharge for West Branch of the Penobscot has been corrected for storage; other figures are as obsi EFFECT OF PRESENT STOEAGE OK PLOW. 201 unit discharge of the Piscataquis at Foxcroft is greater than that ofthe other tributaries of the Penobscot here considered, it is probablethat the results shown by the mass curves (PL XI) are somewhattoo large. The July to March curves for the three seasons considered onPlate XI indicate that the discharge in 1907-8 was considerablyabove the normal, the other two seasons being characterized asdrier. During July of each year the flow of the East Branch isliable to be somewhat affected by storage, but it will be noted thatafter July the East and West branches show very similar dischargeuntil the following April. The discharge of the Mattaw
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Keywords: ., bookcentury1900, bookdecade, booksubjectwatersupply, bookyear1912
