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Zbog svoje veli~ine i velike te`ine one ne mogu poletjeti<br />

sa zemlje bez pomo}i uzlaznih zra~nih struja.<br />

Ovdje se gnijezde nad morem, na zastra{uju}e visokim<br />

nepristupa~nim liticama s kojih im uzlazne zra~ne<br />

struje omogu}uju sigurno polijetanje. Fosilni nam<br />

nalazi kazuju da su bjeloglavi supovi ovladali ovim<br />

nebom i ovim kopnom jo{ prije desetak tisu}a godina.<br />

Pretpovijesni ~ovjek i bjeloglavi sup gledali su ovo isto<br />

nebo, i sunce i ovu istu zemlju otoka Krka i kvarneskog<br />

arhipelaga jednako kao i mi danas, ali nisu vidjeli ovo<br />

divno more jer tada ga ovdje jo{ nije bilo. Tek prije<br />

15000 godina po~eo se ovaj prostor postepeno prekrivati<br />

morem, a ovi su otoci nepotopljeni hrptovi i<br />

vrhovi nekadanjih planina. Jo{ prije desetak tisu}a<br />

godina sav Kvarnerski zaljev i svi kvarnerski otoci bili<br />

su povezani suhim kopnom, zapravo je ~itavi sjeverni<br />

Jadran bio plodna naplavna ravnica koju je presijecala<br />

rijeka Pad, a u nju se ulijevale Mirna, Dragonja,<br />

Rje~ina, Dubra~ina i Zrmanja.<br />

Tada{nji je Jadran po~injao tek negdje kod [ibenika,<br />

a pod U~kom i Velebitom na dana{njem morskom<br />

dnu oko otoka Krka pasla su stada mamuta, bivola,<br />

antilopa, jelena i tko zna kojih jo{ `ivotinja. Prije oko<br />

sedam tisu}a godina zavr{ilo je posljednje odle|ivanje,<br />

zatoplilo je i okon~ao se proces otapanja velikih<br />

koli~ina leda na polovima i u planinama. Svjetska su<br />

se mora podigla za oko 90 metara i nastali su sjevernojadranski<br />

otoci, a taj proces u ne{to izmijenjenom<br />

obliku traje i danas. Bjeloglavi supovi svjedoci su svih<br />

tih doga|anja kroz tisu}e godina od postupnog<br />

stvaranja otoka, pretvaranja nekada{njih pa{njaka u<br />

morsko dno danas bogato ribama, rakovima i {koljkama<br />

do pripitomljavanja<br />

ovaca, koza, krava te<br />

procvata i pada pojedinih<br />

kultura ovoga podneblja.<br />

Nije nam poznato<br />

kako se u najstarije ilirsko<br />

doba nazivao otok i<br />

grad Krk. Prvu napisanu<br />

povijesnu naznaku o postojanju<br />

na{ega otoka u<br />

imenu KURIKTIKE ostavio<br />

nam je anti~ki gr~ki<br />

geograf Strabon (63. prije<br />

Kr. do 19. po Kr.).<br />

Kurikta i Kurikum, te<br />

Kurikon i Kirijatika, Vecla<br />

odnosno Becla te Veggia,<br />

Veglia, Veja i danas<br />

samo <strong>KRK</strong> - neka su od<br />

imena grada Krka i cijelog<br />

otoka, kroz milenijsku<br />

povijest. Otok i grad Krk<br />

dobili su hrvatsko ime<br />

jezi~nom evolucijom imena<br />

ilirskih oto~ana –<br />

Kurikte: Kark, Kerk, Krk;<br />

u doma}em se govoru<br />

grad naziva Veja, {to na<br />

vi{e slavenskih jezika<br />

we do today, but they did not see this beautiful sea<br />

since back then it did not in exist. It was only 15,000<br />

years ago that this territory was gradually filled by<br />

the sea, these islands being the crests and the peaks of<br />

what used to be the mountains. Some 10,000 years<br />

ago the entire Gulf of Kvarner and all of the Kvarner<br />

islands were connected with the mainland. In fact, the<br />

entire northern Adriatic was a fertile alluvial plane<br />

intersected by the Po river, and into which drained the<br />

Mirna, the Dragonja, the Rje~ina, the Dubra~ina and<br />

the Zrmanja.<br />

At that time, the Adriatic began somewhere around<br />

[ibenik, while at the foot of the U~ka and the Velebit<br />

on the present-day seabed surrounding the island of<br />

Krk, grazed herds of mammoths, buffaloes, antelopes,<br />

deer and who knows what other animals. The last<br />

thaw occurred around 7,000 years ago when it<br />

warmed up and the last process of melting of large<br />

quantities of ice at the poles and in the mountains<br />

was completed. The seas were raised by some 90<br />

meters worldwide and the islands of the northern<br />

Adriatic originated. This process under a somewhat<br />

different form has continued to date. The Eurasian<br />

griffons have borne witness to all of these events<br />

throughout the thousands of years during which the<br />

islands were gradually created, the then pastures<br />

turned into a seabed rich in fish and shellfish, the<br />

sheep, goats and cattle domesticated, and various<br />

crops of this region cultivated and abandoned.<br />

The name of the island and town of Krk in the earliest<br />

Illyrian times is not known. The first written historical<br />

record of the existence of this island was made<br />

by the ancient Greek<br />

geographer Strabo (63<br />

BCE – 19 CE).<br />

Curicta and Curicum,<br />

Curikon and Criatika,<br />

Vecla and Becla,<br />

as well as Veggia, Veglia,<br />

Veja and Krk are<br />

some of the names of the<br />

town of Krk and the<br />

whole island throughout<br />

the millennial history.<br />

The island and town<br />

of Krk received the Croatian<br />

name through the<br />

linguistic evolution of<br />

the name of the Illyrian<br />

residents, the Curictas:<br />

Kark, Kerk, and Krk.<br />

The town is commonly<br />

called Veja, which in<br />

several Slav languages<br />

indicates a dry branch<br />

or straw, or generally a<br />

plant, according to Academician<br />

Petar Str~i}.<br />

The island and the town<br />

were called Vecla (Becla)<br />

by the Byzantines and<br />

Veggia and Veglia by<br />

49

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