... the water- line more or less above the level of the adjoining valleys, ultimately in greater part finds its way by springs into streams at the lower level of the district, auy water drawn from the store by artificial means will most probably be at the expense of those streams ; if this be true, it follows...

... t o the adjoining river. Fig. 4, Plate 2, wasasection taken fromStoke Common, nearlyin anorthandsouthline,through WindsorCastle. TO the north of Slough the Chalk fell nearly with the same inclina- tion as the surface, and was covered by the Lower Tertiary beds and the London Clay, with a quantity...

... LOCOMOTIVES TESTS PASSES ROUTES LOWER CARBONIFEROUS GRADING CUTTINGS TUNNELLING ROCKS BRIDGING WOOD TIMBER RIVERS TRACKLAYING ROCKY MOUNTAINS ROCKIES KICKING HORSE 100 CUNINGHAM ON THE CASADIANPACIFICCAILWAT. [ i \ I h U t C S Cf 23 March, 1886. SIRFREDERICK J. BBAMWELL, F.E.S...

...J LUCAS 200 LUCAS ON LOWER GREENSANDS OF SURREY ABD HANTS. [Selected (Paper No. i614.j The Hydrogeology of the LowerGreensands of Surrey and Hampshire. By JOSEPLHUCASF,.G.S. THElower greensandsof Surrey and Hampshire rangoever portions of four river basins, the Wey, the Arun, theMole...

...D T ANSTED © Thomas Telford and ICE 1850 CHALK WATER CONTENT GEOLOGY GROUNDWATER CAPACITY ABSORPTION CRETACEOUS FORMATION DEPOSITS UPPER CHALK UPPER LOWER CHALK LOWER EXPERIMENTS ROCKS ABSORBENT 360 WATER CONTENT%OF CHALK. April 30, 1850. WILLIAM CUBITT, President...