Itza/t e Hoe _or THE ITZAS Br SYLVANUS G. TiffTPT FY ~n i •X : bei... iii«- 4iic0ier> of America ih*-r* Oc ia southern Mexico. Iil< ■ In. itl parts of Huiluoi a great iM. iBtica. which has been caU <4 the Maya U «nay be said at tbe acfset uititout x*g*eratiot that this .•wiliutint had reached a heigh* •OadM by w other peep!-* of the • Mara *m -Uphero p io; to the corn •t« of the white *iaa. la arct Hectare ia ecuIptwre mad ia priatiai the Mayas esrefied Their j .“teste were rdrusuom of tw. mear ability, hat .«■*■ r*«4 sad rw-arded without oe aid of in UfaeVa 'Of prceMas- .u m as are ha*, it it to us «*•< ! -ra'hs of (be Solar acd Vsiei rear# and psobtM r the bag'i- of I be Mercery aid Mar roars la addition to this they L*>. dei eloped » cei-wdar syateoi and perfe* -d a * brctti*!o*y wfci -h la mono of its chart. tertsik way snpe nor n ear sea TV the Mrini cittfT uf this people t -o U«y «**• i-a i4i* Their star had act. The.: greai -* cm -*» had to** abandoned and lay in ndw. wad h*4» rwoatry was promt rated by the qua: "*• d • scare wr nun- of petty tauer-ender: ibxAhH, each of abuts mas waging war on the .. fees Bte» the tw*waor> ««f the older c!t •e*. d their ralt-it. sorb a* Paleeqoe. t'opan «wd far » _*j*|4e seeoiv ;<• hit past 'd ft wo the tatad of iu«. *1 etr farat: rihtncr < • c • -a Khattae pr.ruew-# acd Internet m tdeide ore aJ so*d ft. hoie bees .uw r butory k'tae« ’a the 4er.> and eeiijioe which overtook >«<•• hrttiam aboriginal rtiniiitlo" seven.: Wh* before the *pgr -■ ' L t i-e. ~*~ — t*t •■%«*» jr the targea*. *«mi - tutf r the Qu>i u gulf * *s*. af Che rwt'Md mie> *he apma.--b « satjj»r •*»» Inal am their amt at u, *■ tmm anas Chi rhea fitta. * '»■**! * Stark nr* ta its 1-Mbtua there stilt oita* • r a »h» >«bd sradukta* of foasaer uadlt; aid apiea dw The Baste <~k-he« Itxa *» Hsta aad strap* ch aiek ' Vt-sdb aat kza • he saar of the Kata irthr rh * S*t«d ta the aeidabor (••*« af she tdare. "Ttw h»Mt af he Waits of tfe* I'tt im m a vast tune* toor lormanoa a.tu .t t • wrfaca «Urr One ild travel (nr <•-«. ccwotea. are found all over Yucatan. Ta-. ace usually shout 1M feet in diameter, or . j • era muhr. aad about 7* feet in depth to the nd of tnr water. Geologists say that is rant«a are places where the limestone r««. which everywhere covers the surface at «uratan. haa become weakened by the of aabferraaeaa waters ana has cai laps'd of l«a own weight, forming great sink boom tar natural wells on a large scale. And a. r* II Is clear why the ancient inhabitants af l niches tu* as named their city. In the ».iw of t'jrir aaaderiags. the general trend *al which was aurthward. the Itzas. entering Ya ataa (rva the south, finally reached the . pi remote*, around which Chichen Iua late' was le.itt. but which then waa probably noth tag but wilderness. Mere the striking contrast •4 «d--d by such aa abundance of water in a ■ sue try so generally parched could not fail to bar— slimmed their attention The plar« mat i.a.-e ufsmad ta the thirsty wanderers a God gtsen rite for (he iocs'too of their nea home. Hi right of discover* they claimed the place, aad tv the city which crew up around the cen wtvw 'hey gate the same of Chichen Itza. ‘ The Mwwtb of the Weds of the Itsas " The two rroolM U Cttlrhri Itu have been k»w* by the Mayas from lime immemorial a> the Ceaate Crande mad the Ccnote Sacra ■» *ue large ('rant* and tk* Barren Ceaote. re lye’i.py The first of these unly la former av used for the water supply of the •4‘t. >he Sacred Ceeote being reserved for re