Daily British Whig (1850), 26 Dec 1923, p. 4

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To Sfop A Cold in One Day Pherae cu rm ~ +" the sea. Yon have saved it bh long enough! ONE A ANT AD Y'S AGENCY FOR ALL OCEAN AMSHIP- LINES } al attention given your family going to or returning from Country. arranged for, ' TRENT ONCE A BIG RNER Niagara Has Been the Main Channel for the Last Ottawa, Dec. 26.--Chicago's fight for a drainage canal and Canada's fight for the maintenance of the "| present levels of the Great Lakes raise the interesting geological ques- tion of the history of the Great | Lakes and the changes that have taken place under natural condi- tions during the past few thousand years, since the disappearance of the glaciers of the Ice Age, says a state- ment by the Geological Survey, De- partment of Mines, Ottdwsa. Btudies of the raised or abandon- ed beaches which occur at many places around the marging of the Great Lakes and the old cutlet chan- nels connected with these beaches show that there _have been many changes in the size of the lakes and that the principal outlet has been shifted from one place to another, though the main outlet of Erie and the upper lakes has remained at Ni. agara, throughout the greater part of the time (probably 20,000 to 30,- 000 years) since the disappearance of the ice sheet from the southern part of the Great Lakes region. , The ice sheet which once covered the whole of the Great Lakes region gradually melted back toward the north and for a time blocked the upper part of the St. Lawrence val- ley, thus ponding the waters in the T.ake Ontario basin. The overflow, during this early stage of the Great Lakes--which, however, were much smaller than at present, because a large part of the Hudson valley -to The flow at Niagara during this stage is estimated to have been only 25 per cent. of the present flow. When the ice sheet melted back far- ther toward the north the Trent val- ley outlet was uncovered by the ice and as the land in this region was at that time lower than the Port Huron outlet the main drainage of the up- per Great Lakes was diverfed down the Trent Vallev to the Ontario basin and thence to the sea. . ) Down Ottawa Valley, At a somewhat later stage a part of the drainage escaped by way of the Chicago outlet to the Mississipp! Valley and at a still later stage near- 1y all the drainage of the upper lakes went by way of North Bay and down the Ottawa valley to the Champlain Sea, which then occupied the lower parts of the Ottawa and St. Law- rence valleys. During the times of outflow at the Trent outlet and later at the North Bay outlet the flow at Niagara is estimated to have been only 15 per cent. of the present flow, The outflow at Chicago was probably very small. The shifting of the main outlet from one place to another was due partly to the uncovering by the jce--as it melted back---of outlet channels lower than the more south- | erly outlets and partly to uplift or tilting of the land, the amount of up- lift being greater in the north than in the south, Uplift went on as the ice sheet gradually melted and is : Pattioui~rs apply or write "generally held to have been due to p. 3 Y. oP. &T ' N. R" Canadian Naticant Sin Johnson and Ontario Rifas "oon, t. Pho 99 and 1433. ERAN AN ANADIAN CIFIC removal of the burden of the ice y | sheet from the land surface. Some" parts of thé Niagara gorge are quite different in general char- 7 | ter and size from other parts. The narrow parts are probably due to the small outflows during the times of diversion of the flow of the upper lake by way of the Trent and North Bay outlets, The upper great gorge, two and one-half miles long, was formed during the time that the present flow has been maintained and since the diversion of the flow from the North Bay outlet back to the Port Huron outlet. Judging by the rate of recession of Niagara Falls since 1827 it has taken between 3,000 and 3,500 years to form the upper gorge. ------ A Falls to Stay. One of the most interesting prob- lems in connection with a study of the Great Lakes is the question whe. "ther the uplift which ected the region since the disappearance of the, glaciers of the Ice Age has continued time. One of ~ 4 THE DAILY BRITISH WHIG that the data used were probably faulty. It seems likely that the up+ lift which formerly, affected the re- gion and is still going on in more northerly regions has entirely ceas- ed in the Great Lakes region, so that there is little danger even in the. distant. {ntape- ofa chifting of the outlet from Niagara, at least through natural causes. NEWS BIDGET FRON PICTON Mayor Newman to Entertain Veterans and Families at Regent Theatre. Picton, Dec. 25.--The Salvation Army has been receiving comtribu- tions in front of the post office for the past week. The money was used for Christmas cheer for poor children of the town. Mrs. Walter Adams, Lake street, has gone to Hotel Dien hospital for treatment. Captain D. B. Christie has return. ed home for the winter months. Peter Collier wag re-elected director for this district at the Eastern On- tario District Dairy meeting. Harold Collier of the Bank of Montreal, Ste Catharines, is spending over Christmas with his.parents, Mr. and Mrs, 8. J. Collier. Harold Hack- ing, Vancouver, B.C., arrived in town on Monday to spend over the holiday season with his uncle and aunt, Mr. and Mrs. H, S. Miller. y The funeral of the late John R Goode, who died in the hospital of appendicitis, took place on Wednes- day afternoon to Glenwood cemetery. The deceased was a veteran of the Great War and was accorded a mili- tary funeral, He is survived by his wife, Bertha M. McCoy, and three small children. John P. Hudgin a life long resi- dent of Prince Edward county, died at the home of his son-indaw, Rev. J. G. Osborne, at 9 Library St. Mys- tie, Connecticut. Mr. Hunter, with his wife, had gone from Picton to make his home with his only remain- ing daughter, Mrs. Oshorne. © was seventy-nine years of age. Inferment was in Elm Grove cemetery, Connec- ticut. Mayor Newman has issued an in- vitation to all veterans and military, their families and dependants to be his guests at the Regent theatre, Fri. day evening, Dec. 28th. Miss Margaret Ward, Toronto, is spending the holiday season at the home of her mother, Mrs. Patrick Ward, Paul street. Sidney Holmes, Toronto, is spend. ing the Christmas holidays with his parents, Mr. and Mrs. J. H. Holmes. Mr. and Mrs. T, J. Fleury left on Monday to spend Christmas at the home of Mr and Mrs. John Fleury, Lindsay. Miss Annie Haight, Hagers- town and Mr. and Mrs. Jack Haight, St. Catharines, are spending Christ- mas with their parents, Mr. and Mrs. Philip Haight. Dr. and Mre. Morley Branscombe are holidaying with Mrs. J. M. Platt, Mr. and Mrs. W. H Williamson, Mrs. H. A Hamilton and son, Master Jack, are spending the week with Mr. and Mrs. George Williams, Prescott. Mr, and Mrs. D. F. Robertson and daughters, Misses Rose and Eliza- beth, are holiday guests of Mr. and Mra. D. J. Barker, Old Grange. Mrs, G. 'M. Farrington has gone to Wel- land to visit her daughter Mrs. Howard Brake. Mr. and Mrs. W. W, Porte, Brighton, are with Mr. and Mrs. Alex. Wright. Mr. and Mrs, Stamford Warrington and small son, Teddy, are holidaying with Mr. and Mrs. E. M, Young, Claifamount. Miss Chapman, Usbridge, is a holiday guest with Ther sister, Mrs. J. A. Wear, Main street Miss Valera P. Brough, principal and social worker in one of Detroit's parochial schools, arrived on Monday to spend the holiflays at the home of her parents, Nr. and Mrs. J. W. Brough. po About twenty tons of poultry were bought and shipped from Picten last week. These were mainly turkeys and the price paid averaged twenty cents per pound, rough dressed. Part of them were takem to Toronto by motor truck. A. G. Wagorn has tendered his resignation as Chairman of the pub- lie school board owing to his removal ¢ to Toronto to attend a large 3 ly gathering at his father's home tmas Day. After the Feasts and Excitements of Christmas, then comes ENO'S invariably! ENO'S is so indispensable times for the in the home 'round Christmas time, HRISTMAS is the festival of happiness. But it brings from C diet. It is a time of excusable th linge departuy our regular habits of old--for the young that those who know it would not be without the guardianship of this world-famed laxative health-drink, Remember, too, that Summer vitality, wane after Christmas, and the custom of "fresh air and exercise" winter months. The result is greater susceptibility to many the power of Nature to Nat; resist disease, is on the is difficult to maintain in the long minor ailments which impair health. ENO'S "Fruit Salt" by its cleansing, purifying effect on the digestive organs and the blood, prevents these disorders. - To gaard the health of your family this winter--establish in your household the custom of starting the day right with FRUIT SALT ENO'S Druggists everywhere sell Eno's "Fruit Salt" in TWO sizes now, HANDY SIZE Ideal for travelling, office use, club locker, etc. HOUSEHOLD SIZE More suitable for regular family use, Sales for America F. RI TCHIE £100. LTD. 10-18 McCaul Sts; Toronto . C. ENO Limited Prepared only by J to get through that year satistactor. ily. The third year may prove the hardest one of all. . He is becoming discouraged, his creditors are be- ginning to push him, and new lines of credit are curtailed. He must show a good profit in that third year, or his creditors will get disgusted and close him out. When everything is considered, it is not surprising that so many busi- ness men fail in their third year. A CHRISTMAS REVERIE. (Crawt C. Black.) _ Don't you wish there was a rallway and that you could get a train Which would take you back to child- hood and Christmas there again? Say! Wouldn't you like to go back there to the hours of divine, For Christmas day and experience that joy so genuine, That Joy so everlasting which to think of is a charm, When we were 'round the parent knee back at the village farm? Do you ever long to mingle with your there again, man? Would you like to hang your stock- Christmas And forget the woes and worries of | ordinary DRS CHARLES PF. BROOKS Becre » American Meteorological ¥, Tells How. Stionger, The cpldest weather of winter is by no means in the period of short- est days. It comes as January is be- ginning to decline and in February. There are three reasons for this. One 1s that the ground continues to give out more heat: than it receives from the sun many days after the winter solstice. In fact, it is not until late and the United States, Therefore, in apite of the iis pot until the. last of J lor much of the United States that the mercury begins to average higher. It is truly sald st mid-winter that when the days grow longer, the cold grows stronger. a -- The hen may scratch for tem as well as for one, but she doesn't get #0 much to eat herself, ' You don't siways have to go to the suckers.

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