Show DESERT or n e ali IM is a whole is nut belew 8 lei el it is not hie dry bed of i re cent md it is not as flat s the proverbial lanct keall avci I 1 ait of it indeed Is very ind ill of it Is booie rooie or less tailed lit level 11 e sahara consists of a locky pla rising at times into leaks the LoMei to winch it descends by a steep slope is v depression of caay and but still for tl e most I 1 art standing high abot c sea level 0 portion of the alner bahara is less than feet high most of th reaches from SOU to feet 1 lie two blots below tic sea level consist of alie beds of ancient aliks now much shi link by evaporation to tl e ri inless condition of the country tho soil around these is deep in and the itself is considerably than the sea hi it however is alway the cise with fresh v ater lakes in their last dotage as american geologists have amply in thee ise of the great salt I 1 ake of altah bloking sand undoubtedly coltra a 1 argo irgo spice in both divisions of the desert but ac cording to sr I 1 ambert I 1 jayfair our bet modern authority on the subject it occupies abot more than one third T art of the entire algerian y ilian alse chere rock clay and muddy like are the prevailing features with no infrequent date groves and I 1 villages the product of artesian irtes ian wells I 1 ar excavated spaces or nver oases iven in choit to it its due is not by any means so bl ick n it is painted CM hilt una nf |