A.Workshop"Our natural heritage"
This workshop will be implemented by teachers in Science. They will use PowerPoint presentations or Prezi to introduce natural heritage in the region the partner school is situated.
B.Elaboration of WebQuest"European natural heritage"
Teachers will create a WebQuest in Weebly or Wixx .It will have all components: introduction, task, process, resources, evaluation and conclusion.
Students will have the following tasks:
Task 1:Working in groups, gather infromation about a few national parks in your country and create presentations in English about them. Then publish all presentations on a common website.
Task 2:Learn about national parks in different European countries from the websites created by students from partner schools. Create in your own language posters inviting visitors to different national parks in Europe.
C. Evaluation
Evaluation will be don by survey monkey.
D. Online communication in TwinSpace
E.Evaluation questionnaires
Questionnairs about the satisfaction of the project participation will be created through Google forms.It will be a resposibility of the Bulgarian partner to implement and conclude the results of this research.
The Madara Rider or Madara Horseman (Bulgarian: Мадарски конник, Madarski konnik) is a large early medieval rock relief carved on the Madara Plateau east of Shumen in northeastern Bulgaria, near the village of Madara. The monument is dated to the very late 7th or more often the very early 8th century, during the reign of the Bulgar Khan Tervel. In 1979, the monument was listed as a UNESCO World Heritage Site.
The relief sculpture depicts a majestic horseman, approximately 23 m (75 ft) above ground level, carved into an almost vertical 100 m-high (328 ft) cliff. The sculpture is almost life-size. The horseman, facing right, is thrusting a spear into a lion lying at his horse's feet, and on the left a dog is running after the horseman. The carving of the horseman's halo and garments, as well as the bird in front of the horseman's face, are barely recognizable due to centuries of erosion and the generally poor condition of the monument. The relief is similar to the carbon images found in Saltovo, Soulek, Pliska and Veliki Preslav.
Plitvice Lakes National Park, Croatia's largest national park covering almost 30,000 hectares, is situated in the lower elevations of the Dinarides in the central part of the country. Within a beautiful karst landscape dominated by a mix of forests and meadows, the magnificent Plitvice lake system stands out, fascinating scientists and visitors alike. Interconnected by many waterfalls and watercourses above and below ground, the lakes are grouped into the upper and lower lakes. The former are formed on dolomites, with mild relief, not so steep shores and enclosed by thick forests, whereas the latter, smaller and shallower, are situated in limestone canyon with partially steep shores. The lake system is the result of millennia of ongoing geological and biochemical processes creating natural dams known as tufa barriers. These are formed by the deposition of calcium carbonate from the waters flowing through the property. In the case of the Plitvice lake system, this geochemical process of tufa formation interacts with living organisms, most importantly mosses, algae and aquatic bacteria. The scale of the overall lake system and the natural barriers are an exceptional expression of the aesthetically stunning phenomenon, acknowledged since the late 19th century. Plitvice Lakes National Park area is mainly covered with very well preserved forests essential for the continuity of geochemical processes in water system (above and below ground), which include an area of 84 ha of old-growth forest of beech and fir. Besides the striking landscape beauty and the processes that continue to shape the lakes, the park is also home to noteworthy biodiversity. The tufa barriers themselves provide habitat for diverse and highly specialized communities of non-vascular plants. Brown Bear, Grey Wolf and Lynx along with many rare species roam the forests, while the meadows are known for their rich flora.
The cave is situated 30 km. north, north-west of Antalya. It is on the east slope of mount Katran which is in the range of western Taurus mountains. Carved in Cratese period limestone, its altitude is 430m from the sea level and 150m from the travertine plain. The plain which is formed by transgression, is one of the largest travertine plais in the world. There are fine water springs where the plain meets the mountains. Geological and geomorphological researches in the recent years revealed a lake in the middle of the plain in Pleistocene; and many open air settlements in Paleolithic period. This is proved by the fossils of hippopotamus bones and shells of invertebrata found in the fauna of the Karain cave. The location of the cave is near the strait of Cubuk which is an important passage connecting the Mediterranean region with Inner Anatolia and the Region of Lakes. Karain is a complex of caves rather than a single cave. It consists of many chambers. These chambers are separated by calcite walls and narrow and curve passageways. Stalactites and stalagmites enriches the marvellous appearance of the cave. On the outer surface of the cave there are numerous niches and Greek inscriptions. The cave is found by Prof.Dr.Isin Yalcinkaya with the cooperation of the University of Liege and some other foreign universities.
Property encompasses valley located within the Pieniny National Park in the south of Poland. During the selection of representative sites defined location represents a unique and extremely interesting geological and geomorphological features and which is characterized by poor anthropogenic influence with preservation of specific natural ecosystems.
Evaluation of high level of ecological stability and high biodiversity of flora and fauna, preservation of relict phytocenoses and zoocenoses as well as high representation of rare and endangered species of flora and fauna on the small territory served as the secondary criterion for the selection of sites.
Selected site represents the main stages of geological and geomorphological evolution of the existing territory in the period since the early cenozoic till quaternary. Geological structure, petrographic composition and proportion of rocks, tectonic movement as well as exogenetic factors created original territories, extremely valuable and rich in natural beauty.
The landscape of the Dunajec River Gorge has in contrary to the other types of country lot of specific features which distinguish it evidently from the other areas. Mainly, it is a strong interaction of all natural factors of the area (geological ground, relief, water, soil, climate, flora, fauna) and their evolutional relationships. These facts simply underline the complexity of natural conditions of the area in a whole and also in some individual details.
Limestone and dolomite ground, its shape and original evolution makes conditions for specific elements of flora and fauna which are by its existence linked to this environment. There is a typical occurrence of Carpathians plant and animal species, in many cases endemitic. With their varied morphologic segmentation they give the area original and highly valuable landscape and esthetical character.