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  • Aug. 1, 1876
  • Page 49
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The Masonic Magazine, Aug. 1, 1876: Page 49

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    Article NOTES ON LITERATURE, SCIENCE, AND ART. ← Page 5 of 6 →
Page 49

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Notes On Literature, Science, And Art.

and the foundations , so to speak , of the river systems of the country were fairly inau gurated . For a considerable time the Trent Valley of this period was , even far south of the district under consideration , subjected to tidal action ; and its estuarine conditionsin common with those of the

, other great river-valleys of the country , extended many miles further inland than at present . Consequent , however , upon the continued elevation of the land , accompanied by an increase in the rate of temperaturethe sea gradually retreatedand the

, , Valley became the bed of one broad river , between whose banks rolled its watersfed largely by periodically melting ice and snow—riddling , washing , and carrying away to sea by far the greater portion of the clay and other finer material , and by

this means allowing to settle down , upon the red marls beneath and between its two banks , to the reduced thickness of from fifteen to thirty-five feet , the sand , gravel , and boulders which composed the remaining portion of the deposits with which the Valley was originally infilled . A yet further change took place . The river , by the continued elevation of the land , became

gradually contracted in its dimensions , and by degrees small tracts of gravel-beds appeared at the surface ; and as they rose the lessening waters worked out therefrom new channels , and they lay in the broad river a series of small islands , which , in the course

of time , become covered with vegetation . The outlines of the islands of this period , which are generally oval , and do not exceed six feet above the present level of the Trent , are easily traceable , and it is upon one of these that the town of

Burton-on-Trent was ori ginally founded . A further elevation and silting up of about two feet , however , brought about a considerable change , and converted the area between the two banks from an island-dotted river into a Valley cut up and about equall

y ap portioned between land and water . In the course of time a yet further increase in the laud-area of the Valley took place—possibly the result , to a certain extent , of its elevation , but principally of silting—by which means its conditionas presented under

, the aspect of an ordinary flood , was established . The last change represents the present aspect of the Valley under ordinary circumstances . There have ,

therefore , been no less than four different levels of river-action in the Valley , each represented by a distinctive series of deposits , and occupying definite and well-defined areas . The first is , of course , when the whole of the Valley was under water , and

the terrace-gravels of Drakelow , Stapenhill , on the one side , and of Horninglow and Stretton on the other , formed the river banks ; the second when the first range of gravel-islands or banks appeared . Of these , the largest commences about 200

yards north of Branstone Cottage , [ the author ' s residence , ] and extends to the bottom of Anderstaff-lane , being thus occupied by the High-street , and all the old parts of the towrr of Burton . " And in an equally plain manner does Mr . Molyneux

point out to his neighbours the gradual formation of the land they live on , and the materials of which it is composed , as well as the best means of preventing inundations for the future . If Mr . Molyneux ' s larger work be half as interesting as his sixpenny

pam phlet—and it ought to be more so—it must be most agreeable reading ; anyhow , he deserves hi gh praise for the able treatise he has published on "The Old River Courses and the Recent Floods of the Trent Valley at Burtou-on-Trent . "

On the 1 lth of May last , Lady Smith , of Lowestoft , in Suffolk , completed her hundred and third year , on which occasion she received by post the following beautiful verses by Eta Mawr , with the' writer ' s photograrili : —

" fake—honour'd Lady—jiaid with joy and pride , This cordial tribute , on your natal day ! To kindred minds , though space and time divide , Th' electric spark of friendship finds its way .

Accept the humble offering which I send ; Your portrait I possess — enclosed is mine ; A feeling , though a somewhat failing , friend—For I too have arrived at life ' s decline ! And life seems but a dream , though full of years , When back we look upon the lapse of time ;

“The Masonic Magazine: 1876-08-01, Page 49” Masonic Periodicals Online, Library and Museum of Freemasonry, 30 May 2025, django:8000/periodicals/mmg/issues/mmg_01081876/page/49/.
  • List
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Title Category Page
Untitled Article 1
Untitled Article 2
Untitled Article 2
Monthly Masonic Summary. Article 3
THE DAFFODIL. Article 3
THE EARLY INDICIAE OF FREEMASONRY. Article 4
AN EARLY MASONIC BOOK. Article 5
SONNET. Article 9
MAY MASON. Article 9
SOCIAL PROBLEMS AND THEIR PEACEFUL SOLUTION. Article 14
SONNET. Article 19
AN OLD, OLD STORY. Article 19
THE WOMEN OF OUR TIME. Article 21
MASONIC AMATEUR PERFORMANCES AT PLYMOUTH. Article 23
NOTES ON THE OLD MINUTES OF BRITISH UNION LODGE, IPSWICH. Article 26
AMERICAN KNIGHTS TEMPLARS Article 27
ZOROASTRIANISM AND FREEMASONRY. Article 30
THE FALLING SNOW. Article 33
FAIRY TALES UTILISED FOR THE NEW GENERATION. Article 33
THE ORIGIN AND REFERENCES OF THE HERMESIAN SPURIOUS FREEMASONRY. Article 34
Our Archaological Corner. Article 37
MASONIC ARCHAEOLOGICAL NOTES AND QUERIES. Article 39
SERMON Article 41
REVIEW. Article 43
SOMEHOW OR OTHER. Article 45
NOTES ON LITERATURE, SCIENCE, AND ART. Article 45
HYMN. Article 50
Untitled Article 51
Untitled Article 52
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Note: This text has been automatically extracted via Optical Character Recognition (OCR) software.

Notes On Literature, Science, And Art.

and the foundations , so to speak , of the river systems of the country were fairly inau gurated . For a considerable time the Trent Valley of this period was , even far south of the district under consideration , subjected to tidal action ; and its estuarine conditionsin common with those of the

, other great river-valleys of the country , extended many miles further inland than at present . Consequent , however , upon the continued elevation of the land , accompanied by an increase in the rate of temperaturethe sea gradually retreatedand the

, , Valley became the bed of one broad river , between whose banks rolled its watersfed largely by periodically melting ice and snow—riddling , washing , and carrying away to sea by far the greater portion of the clay and other finer material , and by

this means allowing to settle down , upon the red marls beneath and between its two banks , to the reduced thickness of from fifteen to thirty-five feet , the sand , gravel , and boulders which composed the remaining portion of the deposits with which the Valley was originally infilled . A yet further change took place . The river , by the continued elevation of the land , became

gradually contracted in its dimensions , and by degrees small tracts of gravel-beds appeared at the surface ; and as they rose the lessening waters worked out therefrom new channels , and they lay in the broad river a series of small islands , which , in the course

of time , become covered with vegetation . The outlines of the islands of this period , which are generally oval , and do not exceed six feet above the present level of the Trent , are easily traceable , and it is upon one of these that the town of

Burton-on-Trent was ori ginally founded . A further elevation and silting up of about two feet , however , brought about a considerable change , and converted the area between the two banks from an island-dotted river into a Valley cut up and about equall

y ap portioned between land and water . In the course of time a yet further increase in the laud-area of the Valley took place—possibly the result , to a certain extent , of its elevation , but principally of silting—by which means its conditionas presented under

, the aspect of an ordinary flood , was established . The last change represents the present aspect of the Valley under ordinary circumstances . There have ,

therefore , been no less than four different levels of river-action in the Valley , each represented by a distinctive series of deposits , and occupying definite and well-defined areas . The first is , of course , when the whole of the Valley was under water , and

the terrace-gravels of Drakelow , Stapenhill , on the one side , and of Horninglow and Stretton on the other , formed the river banks ; the second when the first range of gravel-islands or banks appeared . Of these , the largest commences about 200

yards north of Branstone Cottage , [ the author ' s residence , ] and extends to the bottom of Anderstaff-lane , being thus occupied by the High-street , and all the old parts of the towrr of Burton . " And in an equally plain manner does Mr . Molyneux

point out to his neighbours the gradual formation of the land they live on , and the materials of which it is composed , as well as the best means of preventing inundations for the future . If Mr . Molyneux ' s larger work be half as interesting as his sixpenny

pam phlet—and it ought to be more so—it must be most agreeable reading ; anyhow , he deserves hi gh praise for the able treatise he has published on "The Old River Courses and the Recent Floods of the Trent Valley at Burtou-on-Trent . "

On the 1 lth of May last , Lady Smith , of Lowestoft , in Suffolk , completed her hundred and third year , on which occasion she received by post the following beautiful verses by Eta Mawr , with the' writer ' s photograrili : —

" fake—honour'd Lady—jiaid with joy and pride , This cordial tribute , on your natal day ! To kindred minds , though space and time divide , Th' electric spark of friendship finds its way .

Accept the humble offering which I send ; Your portrait I possess — enclosed is mine ; A feeling , though a somewhat failing , friend—For I too have arrived at life ' s decline ! And life seems but a dream , though full of years , When back we look upon the lapse of time ;

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