En: Indiki EarthCache-e hoş geldiňiz! Bu gün Lýuksemburgda gyzykly ýere baryp göreris. Bu ýerde gaty gyzykly gaýalary görüp bilersiňiz ...
Geologiýa
Biri bu seýilgähe, Antalýa-Alanya awtoulag ýolunyň 49 km-de demirgazyk tarapa bölünýän asfalt ýoly bilen baryp ýetýär. Bu ýol Taşağyldan geçip, Beşkonak şäherine baryp ýetýär. Milli seýilgähiň dynç alyş gurluşy Köprü derýasyndan emele gelýär.
Palçykdan, gum daşyndan, konglomeradan we hek daşlaryndan ýasalan sebitiň geologiki emele gelmegi, karstiki ýer emele gelmegini mümkin edýär. Kopru derýasynyň Bolasan obasy bilen Milli seýilgähiň tebigy çeşmesini emele getirýän Bes konak arasynda emele gelen jülge, uzynlygy 14 km bolanlygy sebäpli Türkiýäniň iň uzyn kanýonydyr. diwarlary beýikligi 100 m-den geçýär. Milli seýilgähdäki sosna, serwi we kedr agaçlary we jülgäniň aýagyndan daglaryň ýalaňaç depelerine çenli uzap gidýän ýaprakly köp sanly agaç görnüşleri bilen emele gelen ösümlik örtügi baý maqui toparlary bilen goldanýar.
Bu ýerdäki gaýalar hek daşyndan emele gelýär we erän (we şu güne çenli) has uly gaýanyň galyndylarydyr. Hk daşy çökündi metamorfik gaýadyr. Esasan kalsiý karbonatdan (80% -den gowrak) durýar. Wagtal-wagtal palçykdan, kwarsdan ýa-da galyndylardan bölekler bolýar. Dürli hapalar gaýany çal, gyzyl (demir oksidleri) reňkleýär. Hk daşy biohimiki we biomehaniki taýdan emele gelýär. Biohimiki taýdan emele gelen hek daşlary merjen gaýalary ýaly organizmleriň biohimiki prosesleri bilen döredildi. Biomehaniki taýdan emele gelen hek daşlary, gabyklaryň we molýusk gabyklarynyň toplanmagy bilen emele gelýär. Bu hek daşlaryny organogen ýa-da organodetrit diýip atlandyrýarys.
Hk daşlary karsta degişlidir. Uly ýerleri emele getirýärler - karst. Hk daşlarynyň daşlary dürli-dürli egrilen, sözüň doly manysynda çyzylan. Sebäbi hek daşy kömürturşy gazyny öz içine alýan suwda aňsat erýär. Bu berk ýüzlere galyndylar diýilýär. Hk daş massiwleriniň içinde ajaýyp stalaktit bezegi bolan çukurlar we giň gowak ulgamlary döredilýär.
Hk daşlary çalt, sement, ezilen agregat we nepis daş öndürmek üçin, metallurgiýada, himiýa senagatynda, kagyz senagatynda we beýleki köp ugurlarda ulanylýar. Çap etmek tehnologiýasy üçin inçe däneli hek daşy ulanylýar.
Wezipeler:
1. heerli hek daşy haýsy reňk?
2. Köprülü kanýony näçe çuň we giň?
3. Bu ýerde galyndylary görüp bilersiňizmi?
4. youanyňyz bilen ýa-da GPS bilen hek daşy bilen surata düşüň
Maňa jogaplary profil arkaly iberiň, soňra adaty giriň.
Çeşmeler: wikipediýa
En: Welcome to next EarthCache! Today will visit interesting place in Luxembourg. You can see here very interesting rocks...
Geology
One reaches this park by following the asphalt road which separates towards the north at the 49 km of Antalya-Alanya highway. This road passes through Taşağıl and reaches Beşkonak. The recreational texture of the national park is formed by the river Köprü.
The geological formation of the region made of clay, sandstone, conglomera and limestone masses of rocks makes the carstic ground formations possible. The valley formed by the river Kopru between the Bolasan village and Bes konak, which makes up the natural source of the National Park, is the longest canyon of Turkey owing to its length of 14km. and its walls exceeding 100 m in height. The plant cover in National Park formed by the pine, cypress and cedar trees and many other tree species with leaves which extend from the feet of the valley up to the naked peaks of the mountains are supported with the rich maqui groups.
The rocks here are formed by limestone and are the remnants of a much larger rock, which eroded (and erodes to this day). Limestone is a sedimentary metamorphic rock. It consists predominantly of calcium carbonate (more than 80%). Occasionally it contains fragments of claystone, quartz or fossils. Various impurities color the rock gray, red (iron oxides). Limestone is formed biochemically and biomechanically. Biochemically formed limestones were created by biochemical processes of organisms, such as coral reefs. Biomechanically formed limestones are formed by the accumulation of shells and mollusk shells. We call these limestones organogenic or also organodetritic.
Limestones are subject to karst. They form large areas - karst. The surface of limestone rocks is variously furrowed, literally etched. This is because limestone dissolves easily in water containing carbon dioxide. These rugged surfaces are called scrapes. Inside the limestone massifs, abysses and extensive cave systems are being created, where there is a beautiful stalactite decoration.
Limestones are used for the production of quicklime, cement, crushed aggregate and for fine stone production, in metallurgy, the chemical industry, paper industry and in many other fields. Fine-grained limestone is used for printing technology.
Tasks:
1. What color is local limestone?
2. How deep and wide is Köprülü Canyon?
3. Can you see fossils here?
4. Take picture with you or with your GPS with limostone
Send me answers via profile, then log in normally.
Sources: wikipedia