Krajinski park Secovlje
Krajinski park Secoveljske soline s površino
približno 650 ha leži na skrajnem jugozahodnem delu
Slovenije, tik ob meji z Republiko Hrvaško, v južnem delu obcine
Piran. Severni del Parka, kjer še poteka aktivna pridelava soli, se
imenuje Lera. Od južnega dela Parka, imenovanega Fontanigge, ga
deli struga potoka Drnica.
Na Fontaniggah so veliki bazeni, ki se postopoma
zarašcajo z znacilno slanoljubno vegetacijo – halofiti.
Prepredeni so s sistemom starodavnih nasipov, od katerih so
vecinoma ohranjeni le še vecji. Ob širših kanalih so raztresene
nekdanje solinske hiše, ki s svojo znacilno podobo sooblikujejo
edinstvenost solinske krajine. Glavna sladkovodna žila je reka
Dragonja, ki se po nekaj 10-kilometrskem toku v Secoveljskih
solinah izliva v morje.
Na Fontaniggah je bila pridelava soli v 60.
letih prejšnjega stoletja opušcena, v okviru dejavnosti Muzeja
solinarstva pa se še prideluje sol na nacin, ki izvira iz 14.
stoletja. Vsako solno polje je tu predstavljalo samostojno solino,
z lastnimi bazeni za zgošcevanje morske vode in kristalizacijo.
Na Leri (še danes »aktivnem« obmocju) pa so
solna
polja, namenjena kristalizaciji soli, locena od polj za
zgošcevanje morske vode (bazeni za izhlapevanje). Razlika med obema
nacinoma pridelave soli je torej v tehnološkem postopku, ki se veže
na pripravo slanice, žetev in skladišcenje soli ter razlicna
delovna orodja. Skupna znacilnost obeh solinskih obmocij je, da
solinarji na dnu solnih polj gojijo petolo, posebno vrsto
biosedimenta, ki preprecuje prehajanje morskega blata v sol in
zadržuje vgrajevanje posameznih ionov v sol.
V okviru dejavnosti Muzeja solinarstva se še prideluje sol na
nacin, ki izvira iz 14. stoletja.
K nepremicni kulturni dedišcini solin štejemo
solna polja (delujoca in opušcena), kanale in bregove s kamnitimi
zidovi, stopnicami in z zapornicami (ohranjeni so le njihovi
kamniti deli), solinske hiše z okolico (tudi njihove ruševine in
lokacije), poti, mostove, crpalke itd.
Strunjanske in Secoveljske soline se uvršcajo
med edine soline ob vzhodni obali Jadranskega morja, kjer s
tradicionalnimi postopki v celotnem procesu pridelujejo sol z
dnevnim pobiranjem v slanici na biosedimentu – petoli.
Krajinski park
Secoveljske soline sodi med najdragocenejše dele naše naravne
in kulturne dedišcine. Skozi stoletja je ta prostor sooblikoval
clovek - v skladu z zahtevami in s potrebami redkih, na slano
okolje posebej prilagojenih rastlinskih in živalskih vrst. Sledovi
kulture
solinarjev se kažejo v izjemni kulturni, tehniški, etnološki in
zgodovinski dedišcini. Izdelki iz prodajnega programa KPSS so
žlahtni spomniki, ki vabijo na obisk in aktivno spoznavanje
parka.
Secovlje Salina
Nature Park
Secovlje Salina Nature
Park covers about 650 ha along the Slovene-Croatian boundary in the
extreme south western part of Slovenia, in the southern part of the
Community of Piran.
Its northern part, where active salt-making is
still taking place, is called Lera. From the Park's southern part,
called Fontanigge, it is separated by the bed of the Drnica
stream.
The Fontanigge is full of
large basins which, however, are being gradually overgrown by the
characteristic salt-loving vegetation – halophytes. The
basins are crisscrossed by the system of ancient levees, amongst
which mostly the larger ones have been preserved. Along the wide
channels, the former salt-pan houses are scattered, which with
their characteristic appearance co-create the truly unique image of
the salina landscape. The main freshwater vein is the Dragonja
river, which after few tens of kilometres of its course joins the
sea at the Secovlje salt-pans.
At Fontanigge,
salt-harvesting was abandoned in the 1960s, but the tradition of
salt-making, which originates from the 14th century, is still
practiced within the Museum of Salt-making. Here, each salt-field
used to constitute an independent salt-pan with its own basins for
seawater condensation and crystallisation.
At Lera (still »active«
pans), the salt-fields used for crystallisation of salt are
separated from the fields used for condensation of seawater
(evaporation basins). The difference between the two procedures of
salt-making therefore lies in the technological process, associated
with the preparation of brine, harvest and storage of salt, and in
very diverse implements. Their common characteristics, however,
lies in the fact that at Fontanigge and Lera the salters cultivate,
on the bottom of salt-fields, the so-called petola , a
special type of biosediment that prevents sea mud from merging with
salt and at the same time restrains separate ions from building in
salt.
The tradition of
salt-making, which originates from the 14th century, is still
practiced within the Museum of Salt-making.
The salt-pans immovable
cultural heritage includes the still functioning as well as
abandoned salt-fields, channels and levees with stone walls, steps
and sluice gates (with only their stone parts preserved), salt-pan
houses with their immediate vicinity (including their ruins and
localities), paths, bridges, wind pumps, etc.
The Strunjan and Secovlje salt-pans are the only ones along the
eastern Adriatic coast, where salt is produced, with traditional
procedures in the entire process, by daily gathering in brine on
the biosediment – the petola.
Peljite na lokacijo /
Drive to the location:
N 45° 28.623'
E 013° 37.160'
Poišcite pravilne
informacije in odgovorite: / Look for
correct imformation for an answer:
1. V katerem stoletju je
med drugim v Secovljah deloval rudnik crnega premoga? /
In which century was black-coal mine in
the village of Secovlje?
A: 18. stoletju = N 45° 28.823'
B: 19. stoletju = N 45° 28.894'
C: 20. stoletju = N 45° 27.894'
D: 21. stoletju = N 45° 27.793'
2. V pisnih virih je bil
Parecag leta 1067 prvic omenjen in zapisan kot? /
Parecag was in written sources in the
year 1067 for the first time mentioned as?
A: Parenzago = E 013° 36.848'
B: Parencago = E 013° 37.848'
C: Parezzago = E 013° 36.368'
D: Parezaago = E 013° 36.668'
Uporabite vprašanje 1 za N in
vprašanje 2 za E koridinate lokacije cacha.
Use question 1 for N and question 2
for E cooridinates of the cache.
Zacetna vsebina cacha / Initilal
contents of the cache:
Vpisni blok in svincnik / Logbook
and Pencil
Sveca / Candel
Denarnica / Wallet
