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Cadrul natural al japoniei

Cadrul natural al japoniei

Acest proiect trateaza Potentialul Turistic al Japoniei. Mai jos poate fi vizualizat un extras din document aprox. Iti recomandam sa te uiti bine pe extras si pe imaginile oferite iar daca este ceea ce-ti trebuie pentru documentarea ta, il poti descarca.

Ai nevoie de doar 5 puncte. Japonia are climat musonic. Acest "baiu zensen" care se extinde din sudul Chinei spre Arh. Partea Japoniei de la Oc. Pacific, de la regiunea Tohoku din nordul ins. Suprafata Japoniei este de Populatia ei este de Localizarea geografica si caracterizarea judetului 1. Scurt istoric Istoria judetului Prezentul studiu are la baza oportunitatea dezvoltarii si diversificarii ofertei turistice pentru Municipiul Turnu Magurele este unul dintre cele mai vechi porturi dunarene, fiind situat in sudul Limba oficiala Introducere Romania se afla in pragul relansarii; dupa o experienta a economiei centralizate SUA constituie al patrulea stat ca marime dupa suprafata si al treilea ca populatie, fiind prima Introducere 1.

Potentialul Turistic al Japoniei. Iarna Decembrie, Ianuarie, Februarie. Preview document. Fisiere in arhiva 1 : Potentialul Turistic al Japoniei.In Japonia principalele unitati de relief sunt :campia Kushiro, localizata in sudul si estul insulei Hokkaido, de forma triunghiulara cu numeroase lacuri ex. Furen ,Toro si mlastini ;campia Ishikari strabatuta de raul omonim, joasa sub mformata pe substrat argilos ; campia Tokachi strabatuta de raul omonim, de origine fluvio-lacustra, in care se gasesc numerosi martori de eroziune.

In Japonia Campia Kanto, dezvoltata pe raul Tone, de forma tentaculara, presarata cu numeroase lacuri si mlastini ; campia Osaka, strabatuta de raul Yodo, cu suprafata ceva mai mare. Unitati de campie se mai gasesc si-n insulele Shikoku campia Tokushima si Kyushu campiile Kumamoto, Miyazaki, Yatsushiro.

Cadrul natural

Peisajul regiunilor montane si colinare este reprezentat de : culmile muntoase extinse pe directia nord-sud din zona subtropicala- Kiso, Hida,Akaishi, Kanto, iar dintre varfuri :Uradake m si Yanigatake m. Pe aceeasi directie se dezvolta si marele graben Fosa-Magna, la sud-est de care se inalta vulcanul Fuji-Yama m.

Acelasi graben se continua la nord in insula Shykoku, unde se gasesc numeroase conuri vulcanice, dintre care cele mai reprezentative sunt : Aso mKirishima mUnzen m si Tsurughi m. In insula Hokaido, altitudinile de peste m se gasesc in partea centrala-conul vulcanic Daisetsu m.

Din acest nod orografic se desprind mai multe culmi : Hidaka, Kitami etc. Periferia regiunii mediane este ocupata de munti mai josi cu altitudini ce rar depasesc m. Muntii Japoniei sunt binecuvantati cu multe rauri. Majoritatea raurilor Japoniei sunt repezi, apele lor ajungand oceanul nu dupa mult timp dupa ce au parasit vaile si bazinele muntilor.

Un exemplu de rau abrupt este Kurobe, care se varsa in Marea Japoniei, dupa ce pluteste numai 83 de kilometri de la sursa sa, in Alpii Japoniei, la o altitudine de 2.

Raul cel mai lung al Japoniei este Shinano, care pluteste km de la muntii din regiunea Chubu prin Prefectura Niigata spre Marea Japoniei. Al doilea in lungime este Tone, care pluteste prin Campia Kanto spre Oc. Pacific, si al treilea in lungime este Ishikari, in Hokkaido, la km. Multitudinea de rauri care izvorasc din munti inseamna mult pentru topografia Japoniei, deoarece creeaza mici si mari vai si bazine pentru pescuit, inainte de varsare formand delte.

Imber Travel. Search this site. Navigare Imber Travel. Cadru natural- Peru. Relief si Hidrografie- Peru. Clima- Peru. Biodiversitate- Peru. Obiective turistice- Peru. Traseu- Peru. Oferte de cazare- Peru.Slideshare uses cookies to improve functionality and performance, and to provide you with relevant advertising.

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Ambasada Japoniei în Regatul Unit

You can change your ad preferences anytime. Upcoming SlideShare. Like this presentation? Why not share! Embed Size px. Start on. Show related SlideShares at end. WordPress Shortcode. Elena Negotei Follow. Published in: Education. Full Name Comment goes here. Are you sure you want to Yes No. Raluca Albu. David Doroftei. No Downloads. Views Total views. Actions Shares. No notes for slide.Denumirea oficiala este Nipponkoku, traducandu-se tara de la originea soarelui.

Este cunoscuta in romaneste si sub numele de Tara Soarelui Rasare. Potrivit legendei, Japonia a fost creata de catre zei care au infipt o sabie in ocean, la scoaterea ei formandu-se patru picaturi ce au devenit insulele principale, precum si o multitudine de insule mici peste Prin specificul, continutul si valoarea lor, resursele turistice naturale reprezinta, pe de o parte, atractii turistice, pretabile pentru vizitare, iar pe de alta parte ele pot fi valorificate direct in activitatea de turism ca "materie prima".

Japonia ofera resurse turistice naturale prin componentele sale legate de: relief, clima, rauri, lacuri, vegetatie, fauna, s. Teritoriul Japoniei dispune de un fond bogat si foarte variat de resurse naturale, componente ale peisajului sau geografic cu importante atribute definite de numar si densitate relativa mare si de valente estetice, stiintifice, recreative si educative superioare.

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Aceste valente au facut ca zestrea naturala a teritoriului sa reprezinte principalele elemente de atragere a sa si de retinere a turistilor. Principalul element atractiv il constituie relieful, valoarea sa turistica fiind amplificata de particularitatile celorlalti factori geografici cum ar fi clima, hidrografia, vegetatia si fauna. Se deosebesc regiuni de cutari tertiare, formand geanticlinale si masive ceva mai vechi, ingropate.

Miscarile tertiare - cuaternare au conturat relieful major al acestei parti insulare. In Japonia au loc foarte des cutremure de intensitati mici si medii, iar de cateva ori in fiecare secol au loc cutremure devastatore cum a fost cutremurul din Kanto in si cel din Kobe in In acelasi timp ele au scufundat sau ridicat o serie de compartimente ale reliefului.

Unele din ariile coborate au functionat ca zone de sedimentare, in care s-au depus nisipuri, gresii, marne, argile etc.

Dislocatiile longitudinale si transversale au usurat declasarea vulcanismului in cea mai mare parte in lungul unor linii, existand un vulcanism mai vechi, dar si vulcanism actual.

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Seismicitatea pronuntata este inca un caracter al evolutiei geosinclinalului actual, la care se ataseaza intr-un fel arhipelagul japonez. Intr-un profil morfologic de ansamblu, se evidentiaza urmatoarele trepte ale reliefului: regiuni muntoase, cu altitudini ce depasesc m, regiuni deluroase si montane, cu altitudini cuprinse intre m, campii litorale si interioare, piemontane, fluviatile, cu suprafete mlastinoase.

Foarte frecvent apare relieful vulcanic, inclusiv cel recent, datorita intensei activitati tectonice. Japonia are climat musonic. Vanturile sufla dinspre est in timpul verii si dinspre vest in timpul iernii. Marea Japoniei, care separa insulele de Asia, are un efect moderator asupra climei.

cadrul natural al japoniei

Iarna nu este la fel de rece iar vara la fel de calda ca in China si Coreea. Ploile cad in principal in lunile de vara in est, dar nord-vestul primeste ploaie de iarna adusa de vanturi de peste Marea Japoniei.

Hakodate, in nord, are temperatura medie de -3 grade C in ianuarie si 19 grade C in iunie, cantitatea de precipitatii fiind de cm. Numerele corepunzatoare pentru Tokyo sunt 3 grade C, 25 grade C si cm de precipitatii.

La Nagasaki, pe Kyushu, acestea devin 5 grade C, 26 grade C si circa cm, inclusiv peste 30 cm in iunie. Toamna Septembrie, Octombrie, Noiembrie De la sfarsitul verii spre Septembrie, Japonia este adeseori lovita de taifun. Taifunul se naste din mari mase de aer tropical cu presiune joasa in Nordul Pacificului intre latitudinile de aproximativ de grade, si este aproape acelasi fenomen ca uraganul si ciclonul din alte parti ale lumii.

Cand un taifun incepe sa ia forma, se misca spre nord. In fiecare an, in timpul acestei perioade, imprejurul a 30 de tipuri de taifunuri, care de obicei 4 ating Japonia, cateodata cauzand mari distrugeri. Dupa mijlocul lunii Octombrie, Japonia se bucura in general de vreme buna, nu este nici rece si nici calda.

Tara se bucura de asemenea de vreme buna la inceputul lunii Noiembrie. Multi dintre pomi iau culoarea stralucitoare a toamnei, facand in acest timp al anului, impreuna si cu inflorirea copacilor din primavara, un sezon cu adevarat frumos. Iarna Decembrie, Ianuarie, Februarie. Dupa sfarsitul lui Noiembrie, vanturile reci sezoniere incep sa sufle dinspre continent. Aceste vanturi nord-vestice incep sa ridice umezeala de pe Marea Japoniei si sa lase mult din umezeala in forma de ploaie si zapada in vestul Japoniei fiind impiedicate sa avanseze in est din cauza reliefului muntos din partea centrala a tarii.

Regiunea Hokuriku prefecturile Fukui,Ishikawa, Toyama si Niigata din fata Marii Japoniei, fiind separata de celelalte regiuni ale Japoniei de muntii inalti, este cunoscuta pentru imensa ei zapada.

In opozitie, zona Pacificului se bucura in general de ceruri senine in timpul iernii. In Tokyo, in ciuda norilor senini, temperatura din iarna ajunge in jur de 5 grade, o diferenta de aprox.

Insulele din Prefectura Okinawa din departatul S-V au un climat subtropical cu temperturi mai putin diferite dintre anotimpuri. Temperaturile din iarna sunt mult mai moderate decat din alte parti ale tarii.Pe la mijlocul sec al VI-lea e. Floarea familiei imperiale japoneze este crizantema. Hokkaido 2.

Potentialul Turistic al Japoniei

Aomori 3. Iwate 4.

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Miyagi 5. Akita 6. Yamagata 7. Fukushima 8. Ibaraki 9. Tochigi Gunma Saitama Chiba Tokyo Kanagawa Niigata Ishikawa Fukui Yamanashi Nagano Gifu Shizuoka Aichi Mie Shiga Kyoto Osaka Hyogo Nara Wakayama Tottori Everyday we show you the best paid apps that you can download for free AND we write in-depth answers to questions that our users submit to the app.

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cadrul natural al japoniei

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cadrul natural al japoniei

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