Page 49 - Annuaire Statistique Québec - 1918
P. 49

PH YSIOGHAPHY                               23

                              TEE l\.foNTEREGIANs:-In the western portion of the St. Lawrence
                         Lowlands, which "vill be referred to beIow, is ta be found the third
                         group of the hills or mountains of the Province.    The general name is
                         derived from Mount Royal at ~VIontreal. From the top of Mount
                         RayaI al! of these hiIls can be seen in the plain ta the east.  They are
                         Mount Royal (769 feet), 11'1ontarville or St. Bruno (715 feet), Belœil
                         (1,437 feet), Rougemont (1,250 feet), Yamaska (1,470 feet), Shefford
                         (1,725 feet), Brome (1,755 feet) and l\'1ount Johnson or Monnoir (875
                         feet).  The heights given are above sea-Ievel.  They are 0,11 of igneous
                         origin.

                              THE S·l'. LAWHENCE LowLANDs:-Between the Laurentian highlancls
                         on the north, and the Appalachian highlands on the south, is the great
                         plain which is described as the St. Lawrence lowlands. It widens west-
                         ward fl~om the city of Quebec, and is the seat of the greater part of the
                         population of the Province.    In the western portion this large area is
                         chiefly underlain by horizontal sedimentary rocks of Palaeozoic age.

                              HYDROGRAPHy:-The great artery of the Province is the St.
                         Lawrence river.   Hs source is in the State of :\finnesota.   From the
                         head of that source----:-the river St. Louis-down through the Great Lakes,
                         and the river proper, ta Cape Gaspé, the distance is 2,100 miles.   The
                         St. Lawrence i8 tidal as far up as the city of Three Rivers, and at Quebec
                         the "spring" tides rise 18 feet.   The mean width of the river from
                         Montreal ta Sorel (46 miles) is 1% miles.      Below Sorel the stream
                         widens into the stretch known as Lake St. Peter.     It has a length of
                         20 miles and a \vidth of 9 miles.  The narrowest part of the river is at
                         Cape Diamond at Quebec, namely three quartel's of a mile.        At the
                         lowel' end of the Island of Orleans (below Quebec), the river widens
                         ta eleven miles, while at the accepted estual'Y, at Cape Gaspé, it is
                         100 miles wide.

                              PmSIOGRAPHy:-M:odern science takes account of the influence
                         of the physical features of a country upon civilization. The physical
                         structure of the Province of Quebec is val'ied. :lVIountains, hills, valleys,
                         plain12, lakes and Iivers are \Videly distributed. The mountains are never
                         of Alpine elevation, but the water stretches of alllcinds are of command-
                         ing size and beauty.    The greater part of the population resides in
                         the St. Lawrence Lowlands, but as has been already stated, a consider-
                         able proportion is spread over the r\.ppalachian and Laurentian high-
                         lands.  The vast reserves of watel' in these highlands, and particularly
                         in the Laurentians, constitute a factor of great importance ta the
                         industrial development of the Province.     In their descent ta the St.
                         Lawrence they furnish an almost inexhaustible store of power for
                         electrical transmission.
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