The physiography of the river Nile and is basin . 0 - 25 11 i 25 - 50 50 - too 100 - 20O ?00 - 300 hoV9 SOO ? Survey L>ept. Cairo MEAN MONTHLY RAINFALL. c I I

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RM2AN8YXN–The physiography of the river Nile and is basin . 0 - 25 11 i 25 - 50 50 - too 100 - 20O ?00 - 300 hoV9 SOO ? Survey L>ept. Cairo MEAN MONTHLY RAINFALL. c I I

RM2AN92NN–The physiography of the river Nile and is basin . mm.0 - 25 2S - 50 SO - too 100 - »oo 200 - aoo bovo 300 1 Survey Hept. Cairo MEAN MONTHLY RAINFALL. — 11 — As this condensation is constantly taking place in this equatorial belt,it follows that the greatest precipitation will be in the neighbourhoodof the centre of the belt, as it iHOes northwards and southwards in itsannual oscillation, a change deterniined by the position of the sunat noon, since where it is in the zenith at noon, it will have the greatestheating effect, causing the ascensional movement of air above referredto. A place situ

$The physiography of the river Nile and is basin . > and the Atbara. / This trough was determined in the first instance by - fractures of the crust which caused a strip of country from about Edfu(hit. 25° N.) to Cairo to be depressed, leaving the plateau standing highabove it, just as the Ked Scii and the gulfs of Suez and Akaba wereformed, probal)ly about the same epoch. This intiirference with thedrainage of the country doubtless produced a series of lakes in the low-lying area, Avhile the drainage of the eastern jjlateau conunenced toexcavate the valleys wliich now exist as dry desert wad Stock Photo$

RM2AN7XRH–The physiography of the river Nile and is basin . > and the Atbara. / This trough was determined in the first instance by - fractures of the crust which caused a strip of country from about Edfu(hit. 25° N.) to Cairo to be depressed, leaving the plateau standing highabove it, just as the Ked Scii and the gulfs of Suez and Akaba wereformed, probal)ly about the same epoch. This intiirference with thedrainage of the country doubtless produced a series of lakes in the low-lying area, Avhile the drainage of the eastern jjlateau conunenced toexcavate the valleys wliich now exist as dry desert wad

RM2AN86XY–The physiography of the river Nile and is basin . r stretched across the river by means of which a boat was passedacross ; these distiuices were subsequently corrected to agrie with theknown width of the section. The results are given in the following table. Bi.uK Nile. Date. l.1()2 0 May ..23 „ (i June20 .,27 .. 4 July ..11 „1« „25 „ VVidtli. dM|.tll. Sc;-t!o;i aiva. Meanvelocity. Diseliarge. Gauge atKhartoum. 111. 111. ni m. i>. s. 111.* p. B. 111. .•547 4 •••54 1420 0-120 1l 1774 (l-:il4 t;{i4 ()7(; :],] ;)•.)(?» 1S2.I 0-;i72 (V.t.-) imh; :r,i rrs-) 201O ()-;i:i;i s;i7 ]-;5() ?A->1 (

$The physiography of the river Nile and is basin . i-r I- !)? I Hi+-4i-. 03. s 5 >u 31 O — 2S1 VoH;MF. IHSClAKIiKD AT SaKUAS ).) KII.OlIiaP.ES LP-STUF.AM OF VaI>I-HALFA {continued). Width MeanDpi)th SeitioiialArea MeanVelocity UiAcliarge 1 i A I 1.1; Date Sarras HiilfaI tliy later IDof, metres metres metresi III. p. 8. Ill3 |». 8. metres ni. .I;.n. 1.. .. 170 I.-) 2571t 0-630 1570 3-02 2-62 .. (].... 17(1 1.V4 25(;6 (1-61(1 1567 3-81 2-56 .K. .. It^.S l.v4 2545 0-5()0 1431 3-70 2-.50 11.. .. 108 l.)-4 2.543 (»-5.)0 1.525 3-66 2-48 14.. .. 168 1.5-2 2524 0-610 1548 3-61 2-45 17.. .. 168 1 Stock Photo$

RM2AN7Y4B–The physiography of the river Nile and is basin . i-r I- !)? I Hi+-4i-. 03. s 5 >u 31 O — 2S1 VoH;MF. IHSClAKIiKD AT SaKUAS ).) KII.OlIiaP.ES LP-STUF.AM OF VaI>I-HALFA {continued). Width MeanDpi)th SeitioiialArea MeanVelocity UiAcliarge 1 i A I 1.1; Date Sarras HiilfaI tliy later IDof, metres metres metresi III. p. 8. Ill3 |». 8. metres ni. .I;.n. 1.. .. 170 I.-) 2571t 0-630 1570 3-02 2-62 .. (].... 17(1 1.V4 25(;6 (1-61(1 1567 3-81 2-56 .K. .. It^.S l.v4 2545 0-5()0 1431 3-70 2-.50 11.. .. 108 l.)-4 2.543 (»-5.)0 1.525 3-66 2-48 14.. .. 168 1.5-2 2524 0-610 1548 3-61 2-45 17.. .. 168 1

The physiography of the river Nile and is basin . 0 - 25 11 i 25 - 50 50 - too 100 - 20O ?00 - 300 hoV9 SOO ? Survey L>ept. Cairo MEAN MONTHLY RAINFALL. c I I

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The physiography of the river Nile and is basin . 0 - 25 11 i 25 - 50 50 - too 100 - 20O ?00 - 300 hoV9 SOO ? Survey L&gt;ept. Cairo MEAN MONTHLY RAINFALL. c I I

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The physiography of the river Nile and is basin . 0 - 25 11 i 25 - 50 50 - too 100 - 20O ?00 - 300 hoV9 SOO ? Survey L>ept. Cairo MEAN MONTHLY RAINFALL. c I I