KRK
KRK
KRK
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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