Okhotsk Sea and Wakka Nature Center Lake Saroma

Total Page:16

File Type:pdf, Size:1020Kb

Okhotsk Sea and Wakka Nature Center Lake Saroma 斜里エリア 4 コース http://www.s-tsuruga.com/ http://www.sentyounoie.jp/ Lake Saroma Wakka Gensei Flower Garden (Kitami City, Tokoro-cho) START One of the largest seashore fields in Japan with lots of beach plants. Wakka means “fresh water” in the Ainu Lake Saroma language. This field has a distinctive long sandbank between the Okhotsk sea and Wakka Nature Center Lake Saroma. It was chosen as a Lake Saroma Tsuruga Resort Captain’s House (Senchou no Ie) Hokkaido heritage site in October 2001. (Kitami City, Tokoro-cho) (Kitami City, Tokoro-cho) About 300 kinds of flowers, including This resort hotel is located lakeside at Lake Saroma where you 37 conventional Japanese-style rooms are available at this Siberian lilies, Japanese roses, and the can enjoy the famed beautiful sunset over the lake. Looking into restaurant. The Captain’s House serves a variety of fresh common glasswort, grow wild here each Captain’s House the field scope, you can watch the rare wild birds that rest in the fish and shellfish from the Okhotsk Sea. You can also enjoy season. This field is also a habitat for wild (Senchou no Ie) shallows of the lake. You can also enjoy the “Wakka no Yu” a morning market at the seaside, a two minute walk birds. Lake Saroma Wakka Gensei Flower 栄浦大橋 natural spa while watching the lake as part of a day trip. away. The hotel restaurant is available at lunch time (11 Garden 093-0216 Kitami city Tokoro cho Sakae ura am~3 pm) for visitors and Hotate Zukushi and the Hotate 306-1TEL.0152-54-2000 Bowl are popular lunch items. Both are made of scallops, Lake Saroma the pride of Saroma. 常呂町栄浦 ● Tsuruga Resort CYCLE PARK Notoro Cape Lake Saroma ところ遺 跡 の 森 Seicomart 093-0216 Kitami city Tokoro cho Sakae ura lakeside of サロマ湖 Saroma-ko 駐車公園 7-Eleven Notoro Cape Kimuanep Cape Kitami City Tokoro Transportation Terminal 名 称 至湧別町・紋別市 Lake Notoroko Parking 電 話 巨樹・巨木百選 美岬ヤチダモ 営 業 時 間 Lake Notoroko’s Common Glassworts Road Station Ryuhyo Kaido Abashiri Lake Notoro 二つ岩 レイクサイドパークのとろ GOAL Ubaranai Transportation Park( Abashiri City) Abashiri Prison(Abashiri City) Abashiri Beer House(Abashiri City) This park is re-using ex-station(Ubara nai) of railway line Abashiri prison Wagyu(Japanese black beef) raised by There are many local beers that make use of local Abashiri Beer House (Yumo line)which was closed in 1987. At station platform Abashiri prison prisoners(cattle breeding team) is popular. produce and the local spirit which are very popular. Lake Notoroko’s station sign 'Ubara nai eki” is still exhibited and also SL and Under mother nature of Hokkaido calves are raised “Ryuhyo Draft” is a low malt, “Okhotsk blue” colored beer Common Glassworts モヨロ Number of national railway's old style passenger car are being carefully for 30 long term months with non- chemical that uses drift ice for water. “Shiretoko Draft” is inspired by 貝塚館 Bike Stands displayed.Beside SL there is a cycling road and it takes 5 meadow grasses. You can buy them at the shop inside spring at the Shiretoko World Heritage Site. And “Jailhouse Abashiri Prison minutes walk from the park facing Lake Notori to common Abashiri prison. Please note that they might be out of Black” is inspired by the Abashiri Jailhouse. At the YAKINIKU 1 * Abashiri City Abashiri glasswort growing in colonies.This place is suitable for stock because they are so popular. Abashiri Beer Pavilion you can enjoy Abashiri beer JR Abashiri st. Omagari Parking resting with fully equipped toilets. together with Abashiri beef. Abashiri City Eem Service Abashiri prison shop 093-0088 Abashiri city Sancho Kahan 網走港 Seicomart 二見ヶ岡 Lawson 093-0135 Abashiri city Ubaranai, Hokkaido San cho, Hokkaido TEL.0152-43-3174 1 chome 1-2, Minami 2 jo Nishi, 7-Eleven Park Business hours/9am~4pm Abashiri City TEL.0152-41-0008 Ubaranai オホーツク流冰館 Transportation Park 北方民族博物館 Okhotsk Sea 網走監獄 K WONDER オホーツク公園 OTS RO KH A O D Distance GREEN HILL 905 水芭蕉群生地(4月) 網走海鮮市場 Lake Notoroko’s Common Glassworts 43.1km (Abashiri City) 網 走 ス ポ ー ツ・ JR Mokoto st. In the fall, the common glassworts gradually turns red and トレー ニング フィー ルド Maximum Elevation in early to mid September it spreads over the water’s JR Yobito st. above Sea Level edge like a huge red carpet. It leaves a beautiful impression of fall in the north country and is reflected in 喜多山 Lake Abashiri the quiet lake surface and the clear blue sky. Around the Lake Mokoto south bank of the lake is the best view point in Japan for 丸山公園 30m these plants. In 28th Common Glasswort Festival held in 1991, Abashiri City declared this place to be the no. 1 common glasswort spot in Japan. 感動の径 郷 豊 濤沸湖 Okhotsk “Kitami City Tokoro-cho~Abashiri” メルヘンの丘 Road Station Meruhen-no-Oka Memambetsu 女満別住吉 JR Memanbetsu st. KAIDO UNCLE HOUSE K Golden Route 女満別朝日 O 7-Eleven enjoy! The Golden Route is packed with the charms of Okhotsk for all cyclists to enjoy. This route has an extraordinary view of 女満別 H Lake Saroma, Notoroko Lake, and Abashiri Lake. In the summer you can enjoy the flowers of the Wakka Genshi flower garden. In autumn you can enjoy a fantastic view that looks like a red carpet where common grasswort grows around the Notoroko lakeside together with a panoramic view of Abashiri Lake from a bridge over a roadway. This 43.1 km length course offers a never ending series of moving moments. OKHOTSKwonder COURSE ◆ Total Length 43.1km ◆ Maximum Elevation above Sea Level 30m road DATA ◆ Elevation Obtained 87m ◆ Estimated Required Time 3.5~4hrs 0 5km.
Recommended publications
  • Thorough Guidebook of Lively Experience in Kushiro
    Thorough Guidebook of Lively Experience in Kushiro A タイプ Map of East Hokkaido 知床岬 Cape Shiretoko 知床岳 Mt.Shiretoko-dake 知床国立公園 Shiretoko National Park 網走国定公園 カムイワッカの 滝 Abashiri Quasi-National Park Kamuiwakka Hot Water Falls 硫黄山 Mt.Io サロマ湖 知床五湖 Lake Saroma 能取岬 Cape Notoro Shiretoko Five Lakes 羅臼町 93 238 RausuTown ウト ロ 羅臼岳 87 道の駅「サロマ湖」 Utoro Mt.Rausu-dake Michi-no-Eki(Road Station)Saromako 知床横断道路 7 能取湖 76 網走市 334 佐呂間町 Lake Abashiri City オシンコシンの滝 冬期通行止 Saroma Town 103 Shiretoko Crossing Road Notoro 道の駅「流氷街道網走」 Oshinkoshin Falls Closed in Winter Michi-no-Eki(Road Station) 道の駅「知床・らうす」 Ryuhyo kaido abashiri Michi-no-Eki(Road Station) Shiretoko Rausu 網走湖 Lake Abashiri 334 道の駅「うとろシリエトク」 小清水原生花園 Michi-no-Eki(Road Station)Utoro Shirietoku Koshinizu Natural Flower Gaden 道の駅「メルヘンの丘めまんべつ」 333 Michi-no-Eki(Road Station)Meruhen no Oka Memanbetu 斜里町 104 大空町 244 Shari Town Oozora Town 道の駅「はなやか小清水」 道の駅「しゃり」 7 女満別空港 Michi-no-Eki(Road Station)Hanayaka Koshimizu Michi-no-Eki(Road Station)Shari 39 Memanbetsu Airport 102 道の駅「パパスランドさっつる」 Michi-no-Eki(Road Station) 335 334 Papasu Land Sattsuru 391 122 清里町 244 北見市 243 小清水町 Senmo Line 釧網本線Kiyosato Town Kitami City 美幌町 Koshimizu Town 斜里岳 50 Bihoro Town 津別町 102 Mt.Sharidake Tsubetsu Town 斜里岳道立自然公園 Sharidake Prefectural Natural Park 標津サーモンパーク 27 藻琴山 Shibetsu Salmon 143 Mt.Mokoto Scientific Museum 道の駅「ぐるっとパノラマ美幌峠」 野付半島 Michi-no-Eki(Road Station) 開陽台展望台 ClosedGrutto in WinterPanorama Bihorotouge Notsuke Peninsula Kaiyoudai 根室中標津空港 272 240 冬期通行止 屈斜路湖 Observatory NemuroNakashibetsu 野付湾 Lake Kussharo Airport Notsuke Bay
    [Show full text]
  • Out and About in Abashiri
    6 Luxury Zone Walk Talk II 7 ② Melt, Bar & Grill A little further afield Enjoy dining, an aperitif or an after-dinner wine while taking in OutOut andand AboutAbout inin AbashiriAbashiri the magnificent view of Mt. Yotei. Choose from spacious Lake Notoro booths, private rooms or the counter bar. Dinners consist of Located amid the mountains, rivers, seashores and lakes of the area Notoro Cape is a beautiful sand spit that locally produced Hokkaido ingredients grilled simply to designated as Abashiri Quasi-National Park, the city of Abashiri has lots to juts out into the Sea of Okhotsk – a great preserve their natural flavors. Lunches are hearty buffets of offer visitors – natural landscapes, ice floes, museums displaying artifacts from the Okhotsk culture, parks inhabited by wildlife, top-class sports facilities, place to experience the wilds of pasta, curry and the like, complete with hotel-made sweets and sightseeing spots and lots more. In winter, the ice floes that drift from the Hokkaido, with views of expansive soft drinks. far-off Amur River estuary arrive on the coast, turning the Sea of Okhotsk into a grasslands and the sprawling coastline of mystical, solid, white world. View the ice drifts from close range from the deck the northern sea. ③ Japanese Dining, Ren of an ice-breaking pleasure cruiser – an experience unique to the region. A variety of dishes made from fresh seafood, top-quality meat Koshimizu Wild Flower and locally produced vegetables, prepared Japanese style. Preserve/Lake Tofutsu Savor the taste of Japan’s four seasons. Part of Abashiri Quasi-National Park to the Southeast of the city, the preserve stretches for approximately 8 km on a thin strip of land between the Sea of Okhotsk and Lake Tofutsu.
    [Show full text]
  • Modelling Global Fresh Surface Water Temperature
    Modelling global fresh surface water temperature Tessa Eikelboom MSc Thesis Physical Geography May 2010 Supervisors: Dr. L.P.H. van Beek and Prof. Dr. Ir. M.F.P. Bierkens Department of Physical Geography Faculty of Geosciences Utrecht University 1 ABSTRACT A change in fresh surface water temperature influences biological and chemical parameters such as oxygen and nutrient availability, but also has major effects on hydrological and physical processes which include transport, sediment concentration, ice formation and ice melt. The thermal profile of fresh surface waters depends on meteorological and morphological characteristics. Climate change influences the water and energy budget and thereby also the thermal structure of fresh surface waters. The oceans temperature is influenced by the inflow of rivers and streams. The variations in fresh surface water temperatures are only known for a scarce amount of long term temperature records. The understanding of changes in thermal processes by modelling the variations in temperature over time is therefore very useful to simulate the global effect of climate change on water temperatures. A physical based model was validated with regional daily and global monthly water temperature data of fresh surface water which includes both rivers and lakes. The basic assumption for the PCR‐GLOBWB model is the assumption that the fresh surface water temperature is the net result of all incoming en outgoing fluxes. The global hydrological model PCR‐GLOBWB contains a water and heat budget. The heat balance is solved using the following terms: short‐wave insolation, long‐wave atmospheric radiation, water‐surface backscatter, evaporation, air/water conduction and can be simplified into lateral and advective energy.
    [Show full text]
  • Hydrogen Sulfide Distribution in Bottom and Pore Waters During an Anoxic Period in Lake Nakaumi, Japan
    LAGUNA(Research for Coastal Lagoon Environments)11, p.65-68(2004) Hydrogen sulfide distribution in bottom and pore waters during an anoxic period in Lake Nakaumi, Japan Saburo Sakai1,Masaru Nakaya2 and Katsumi Takayasu3 Abstract: Hydrogen sulfide concentrations in bottom water and surface sediment pore water were measured during an anoxic period (September 2003) in brackish Lake Nakaumi, Japan. Bottom water hydrogen sulfide concentrations were greatest (5-127μg-Sl−1;except for artificially dredged area) in the southern part of the lake and the Yonago-Bay area, where the hypolimnion is most stagnant, whereas hydrogen sulfide from pore water was detected ( ~1-37 mg-Sl−1)inamuch wider area. This indicates that surface sediments may maintain anaerobic conditions long after the bottom water return to oxygen rich. Hydrogen sulfide was not detected in bottom and pore waters near the Sakai-StraitandOhashi River, where seawater and river water flow into the lake. In comparison with two other Japanese brackish lakes (Lake Abashiri and Lake Asokai), Lake Nakaumi has a lowerconcentration of hydrogen sulfide. Lake Nakaumi is characterized by an unstable hypolimnion, in which anoxic conditions are easily mediated by an oxygen-rich tidal-induced inflow. Keywords: Hydrogen sulfide, anoxic environments, Lake Nakaumi Introduction ‰and that of the lower layer is about 27‰(Date et al., 1989). The vertical gradient in salinity increases during Bottom water in brackish lakes often becomes anoxic the summer, when the bottom water of the lake develops due to the development of a stagnant hypolimnion. oxygen-poor or anoxic conditions. This indicates that the Bacterial mats and associated sulfate reduction often lake bottom may be below the redox boundary during occur in anoxic bottom waters and at the redox summers.
    [Show full text]
  • Abashiri Guidebrochure En.Pdf
    IS 」ⅡSt ?07 mclcls h h01η lhじ SumnlH IS 0IS C註" cnjoY P【1"01'a訂U . Iento 1.akc Ab;1S11in.【"1{kc l"ofⅡISU N010ro ;"1d l"akC 入・10k010 '1S 、YじⅡ a S1111'ctoko pc"1ns nd lhc sc ▲ Viewing pla廿orm overlookin套_ Ok110lsk al】d 111. .' .',ン'. N11 TC11to 、、'as dcslcn:"C〔 h hiretoko world Natura11t-j11 鳳・ , Beauti6.11, . \八later・rich . City ofthe Nort ' へlt. Tento overlooking A world NaturalHeritage site 、 Ca.e Notoro In the okl)otsk Breeze Connect 圦lith okhotsk cultlH'e Abashiri prison Museum Froln seasonal Foods to The Sτ則Cture oflhis historic outdoor museum was odgina11y .史奥^、 bU11t otthc foot ofMt. Tento overlooking l"ake Abashid, aTld New Local cuisine Was used as Abashid prison before being relocated, PrcseNed and opened to thc pub11C. Today it seNes as a haTlds、on faC11ity 晒,here Ⅵ5itors can leam oboutthe historyof Hokkaido's development from the exhibits on display in t11is genuinc Meiji・e鳳 Structure ゛Guided louTs aTc ava11able ln the museum (inqU1訂es required) .1.1' Yobito, Abashiri .Hours: Apr.- oct.:8:00 -18:00; NOV.- Mar.:9:00 -17:00 ●Open year-『ound .Admission: Adults:1,050 yen; univetsity/high scho01 Students:730 yen; elemenねⅣ/junior high school studen{S 520 yen (group rates ava11able) (For more information) Abashlri prison preservation Foundetion Tel:015245・24TI Mt. Tento observatory/okhotsk Ryuhyo Museum Hana Tento Flower Garden DHn ice muscum on top ofMt. Tcnto alongside the obseNatory. TheN ate fiv In the summer one ofthc slopes on Abashiri CxhibitioD rooms including a hl・visio"小eater dcpicting the four seasons o Lake view ski HiⅡ is tTansformed by Abashid on a large 300、inch scrccn and a space where ⅥSitors can see clione Abashin city volunteer aroups into an (also known assca angels)andothermystcri0ⅡS creatures.
    [Show full text]
  • A Synopsis of the Parasites from Cyprinid Fishes of the Genus Tribolodon in Japan (1908-2013)
    生物圏科学 Biosphere Sci. 52:87-115 (2013) A synopsis of the parasites from cyprinid fishes of the genus Tribolodon in Japan (1908-2013) Kazuya Nagasawa and Hirotaka Katahira Graduate School of Biosphere Science, Hiroshima University Published by The Graduate School of Biosphere Science Hiroshima University Higashi-Hiroshima 739-8528, Japan December 2013 生物圏科学 Biosphere Sci. 52:87-115 (2013) REVIEW A synopsis of the parasites from cyprinid fishes of the genus Tribolodon in Japan (1908-2013) Kazuya Nagasawa1)* and Hirotaka Katahira1,2) 1) Graduate School of Biosphere Science, Hiroshima University, 1-4-4 Kagamiyama, Higashi-Hiroshima, Hiroshima 739-8528, Japan 2) Present address: Graduate School of Environmental Science, Hokkaido University, N10 W5, Sapporo, Hokkaido 060-0810, Japan Abstract Four species of the cyprinid genus Tribolodon occur in Japan: big-scaled redfin T. hakonensis, Sakhalin redfin T. sachalinensis, Pacific redfin T. brandtii, and long-jawed redfin T. nakamuraii. Of these species, T. hakonensis is widely distributed in Japan and is important in commercial and recreational fisheries. Two species, T. hakonensis and T. brandtii, exhibit anadromy. In this paper, information on the protistan and metazoan parasites of the four species of Tribolodon in Japan is compiled based on the literature published for 106 years between 1908 and 2013, and the parasites, including 44 named species and those not identified to species level, are listed by higher taxon as follows: Ciliophora (2 named species), Myxozoa (1), Trematoda (18), Monogenea (0), Cestoda (3), Nematoda (9), Acanthocephala (2), Hirudinida (1), Mollusca (1), Branchiura (0), Copepoda (6 ), and Isopoda (1). For each taxon of parasite, the following information is given: its currently recognized scientific name, previous identification used for the parasite occurring in or on Tribolodon spp.; habitat (freshwater, brackish, or marine); site(s) of infection within or on the host; known geographical distribution in Japan; and the published source of each locality record.
    [Show full text]
  • Taxonomic and Ecological Studies of the Genus Hypomesus of Japan
    Title TAXONOMIC AND ECOLOGICAL STUDIES OF THE GENUS HYPOMESUS OF JAPAN Author(s) HAMADA, KEIKICHI Citation MEMOIRS OF THE FACULTY OF FISHERIES HOKKAIDO UNIVERSITY, 9(1), 1-55 Issue Date 1961-06 Doc URL http://hdl.handle.net/2115/21833 Type bulletin (article) File Information 9(1)_P1-55.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP TAXONOMIC AND ECOLOGICAL STUDIES OF THE GENUS HYPOMESUS OF JAPAN KEIKICHI HAMADA Faculty of Fisheries, Hokkaido University, Hakodate, Japan Contents I. Introduction.................................................................... 2 II. Material and Method............................................................ 4 III. Taxonomic Study on Samples from Japan........................................ 5 A) Hypomesus olidus from the Ishikari River .................................. 5 a) Hypomesus olidus ascending to spawn in the spring........................ 5 b) Hypomesus olidus from Oshoro Bay........................................ 6 B) Hypomesus olidus from Lake Abashiri, adjacent waters and two other waters.. 7 a) Hypomesus olidus from Lake Abashiri and a flowing river ................ 7 b) Hypomesus 0lidu8 from the port of Abashiri and adjacent coast............ 7 c) Hypomesus olidus from Lake Tofutsu...................................... 7 d) Hypomesus olidus from the coast of Abuta . .. 7 C) Hypomesus sakhalinus and Hypomesus olidus from Lake Ishikari-Furu- kawa, and Hypomesus olidus from Lake Onuma............................ 7 a) Hypomesu8 sakhalinus
    [Show full text]
  • Japan-Birding "Birding Spots"
    Top-page Inquiry Trip reports Check list News Links Birdwatching Spots Hokkaido Regeon Tohoku Regeon Kou-Shin-Etsu Regeon Northern-Kanto Regeon Southern-Kanto Regeon Tokyo Regeon Izu Islands Ogasawara Islands Izu-Hakone- Fuji Regeon Tokai Regeon Hokuriku Regeon Kansai Regeon Chugoku Regeon Shikoku Regeon Kyushu Regeon Okinawa Regeon Cruise - Over 400 popular birding sites in all over Japan are listed in this page. - The environment, the time required for birding (the traveling time to the site is not included), the birds expected and the visit proper season of each site are briefly described. - You can also check the location of the site in Googl Map. Please click Google-Map in the descriptions. On the Google Map, search the site with the number (i.e,: D6-1 for Watarase Retarding Basin). - The details of the sites can be checked on the linked websites (including Japanese sites). A) Hokkaido Regeon Google-Map West-Northern Part of Hokkaido A1-1 Sarobetsu Plain (Sarobetsu Gen-ya) - Magnificent wetland extending at the mouth of Sarobetsu River, a part of the northernmost national park in Japan - 1-2 days - summer birdss - Best season: May to Sep. A1-2 Kabutonuma Park (Kabutonuma-Koen) - Forest and lake, a part of the northernmost national park in Japan. - 0.5 day - summer birds - Best season: May to Sep. A2-1 Teuri Island (Teuri-Tou) - National Natural Treasure in Japan, the breeding ground for around a million sea-birds; Common Murre, Spectacled Guillemot, Rhinoceros Auklet and Black-tailed Gull . - 1-2 days (*depending on the ship schedule) - the breeding sea-birds or the migrating birds in springa and autumn - Best season: Apr.
    [Show full text]
  • Variation in Migration Patterns of Pond Smelt, Hypomesus Nippo- Nensis, in Japan Determined by Otolith Microchemical Analysis
    Bull. Jpn. Soc. Fish. Oceanogr. 71(3) 175–182, 2007 水産海洋研究 Variation in migration patterns of pond smelt, Hypomesus nippo- nensis, in Japan determined by otolith microchemical analysis † Satoshi KATAYAMA1 , Toshiro SARUWATARI2, Kazuhiko KIMURA3, Motohito YAMAGUCHI4, Tsuyoshi SASAKI5, Mitsuru TORAO6, Takashi FUJIOKA7 and Nozomi OKADA8 In order to investigate the migration pattern of the pond smelt, Hypomesus nipponensis, the life history trajectories of populations from various localities in Japan were estimated using the otolith microanalysis technique. The strontium:calcium (Sr : Ca) ratio of otoliths was determined for pond smelt reared in fresh, brackish and sea water and was found to show a linear increase with increasing salinity. Salinity trajectories were constructed for populations based on a regression of Sr : Ca ratio to salinity. Some individuals in Lakes Abashiri and Ogawara, and all fish in Lakes Taka- hoko and Shinji showed values which were consistently low, indicating residence in these lakes throughout the life his- tory. High values were also absent in individuals from the Ishikari River, so it was concluded that the populations mi- grated between fresh and brackish waters. However, pond smelt with high Sr : Ca ratio profiles indicating seawater resi- dency were found in the Hei River, off Hachinohe, off Misawa, Lake Obuchi, Oppa Bay, and also some individuals from Lakes Abashiri and Ogawara. In these cases, residence in the sea appeared to have been short, except for Hei River and Lake Ogawara. These results indicate a wide flexibility in habitat selection by pond smelt, with brackish environments possibly playing an important role in the life history of the species.
    [Show full text]
  • Nature Conservation Bureau, Ministry of the Environment Peninsula Offers Scenic Mountains, Seashores, and Lake Inawashiro Is Beautiful
    ⑮ Fuji-Hakone-Izu National Park ⑨ Bandai-Asahi National Park SOY A S TRAIT ① Rishiri-Rebun-Sarobetsu National Park REBUN Is. Designation: 1936/02/01 Designation: 1950/09/05 T SOYA B. Designation: 1974/09/20 RAIT Area: 121,695 ha Area: 186,389 ha Area: 24,166 ha RISHIRI Is. STRAI Mt.Rishiri This is the northernmost national park in Japan. Mt. Fuji, a World Cultural Heritage site inscribed in This park is composed of many mountains. Mt. ⑧ IRI National Parks of Japan Sanriku Fukko (reconstruction) National Park REBUN ST H Dewa-Sanzan is famous for mountain worship, Mt. Mt. Rishiri soars majestically above the sea. June 2013, rises high in a vast stretch of forests RIS Designation: 1955/05/02 1721 and several lakes. The Hakone area features Asahi, Mt. Iide and Mt. Bandai are also located ①RISHIRI-REBUN-Mt.Horoshiri Rebun Island has many alpine plants such as several volcanoes, volcanic vents and lakes. Izu within the park boundaries. The view of Urabandai Area:28,537 ha Rebunsou (Oxytropis megalantha). Sarobetsu Nature Conservation Bureau, Ministry of the Environment Peninsula offers scenic mountains, seashores, and Lake Inawashiro is beautiful. This park is sur- This park extends for 250 km from Kabushima in SAROBETSU N.P.427 Tonbatsu Riv. Plain, abundant in marsh plants, and and a chain of characteristic islands in the ocean, rounded by mountains, forests and a lot of lakes. Aomori prefecture to Oshika Peninsula in Miyagi Wakasakanai' s dunes contribute to the exciting Teshio Riv. Izu-shichito. Antelopes and black bears live in this park. prefecture.
    [Show full text]
  • Title Morphometric Features and the Classification of All the Lakes In
    Morphometric Features and the Classification of all the Lakes Title in Japan Author(s) Horie, Shoji Memoirs of the College of Science, University of Kyoto. Series Citation B (1962), 29(3): 191-262 Issue Date 1962-06-30 URL http://hdl.handle.net/2433/258665 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University MEMOIRS OF THE COLLEGE OI? SCIENCE, UNIVERSITY oF 1<YOTO, SERIES B, Vol. XXIX, No. 3, Article 2 (Biology), 1962 Morphome'tric Features and the Classification of all the Lal<es in Japan By Sh6ji HoRIE Otsu Hydrobio}ogical Station, Universi.ty of Kyoto (Osbom Zoological Laboratory, Yale ILJniversity) (Received MarÅëh 20, 1962) !ntroduetien The Japanese IslaRds which consist of four main parts, narnely Hol<kaido, Honshu, Shikoku and Kyushu, stretck from approximately 460N to 240N along tke easterR margin of the Ellrasiatic continent. Geologically speaking, this part of the globe is on.e of typically unstable crust, hence the Japanese often ex- perience severe earthquakes. Besides, the western part of the Peri-Pacific Volcanic Zone runs from the KamÅëhatka Peninsula via the Kuriles, Hokkaido, Honsltu, Kyushu, Ryukyu and to the Phillipine Is}ands. Both the presence of the eartltquake zone and severe vulcanism, together with the steep slopes of the mountains wkich occupy almost all of the country, have resulted in many lakes and ponds in the Japanese Islands. The total numbey of them is about 600 ln this small in.".u}ar country, which is almost equal in area to the State Montana of the United States. They are, moreover, not only numerous but sorae are very important Iakes from the viewpoint of both limnology and geology.
    [Show full text]
  • Hydrogen Sulfide and Organic Carbon at the Sediment–Water Interface In
    Environ Earth Sci (2013) 68:1999–2006 DOI 10.1007/s12665-012-1887-5 ORIGINAL ARTICLE Hydrogen sulfide and organic carbon at the sediment–water interface in coastal brackish Lake Nakaumi, SW Japan Saburo Sakai • Masaru Nakaya • Yoshikazu Sampei • David L. Dettman • Katsumi Takayasu Received: 20 December 2011 / Accepted: 30 July 2012 / Published online: 22 August 2012 Ó The Author(s) 2012. This article is published with open access at Springerlink.com Abstract The relationship among H2S, total organic TOC [3.5 %, H2S was correlated with TOC content (pore carbon (TOC), total sulfur (TS) and total nitrogen contents water H2S (ppm) = 13.9 9 TOC (%) - 52.1, correlation of surface sediments (0–1 cm) was examined to quantify coefficient: 0.72). H2S was also present in areas with sed- the relationship between H2S concentrations and TOC iment TS above 1.2 % (present as iron sulfide), which content at the sediment water interface in a coastal brackish suggests that iron sulfide formation is tied to the amount of lake, Nakaumi, southwest Japan. In this lake, bottom water TOC. Based on this relationship, H2S production has pro- becomes anoxic during summer due to a strong halocline. gressively increased after the initiation of land reclamation 2- Lake water has ample dissolved SO4 and the surface projects in Lake Nakaumi, as the area of sapropel sedi- sediments are rich in planktic organic matter (C/N 7–9), ments has significantly increased. This TOC–H2S rela- which is highly reactive in terms of sulfate reduction. In tionship at sediment–water interface might be used to infer this setting the amount of TOC should be a critical factor H2S production in brackish–lagoonal systems similar to 2- regulating the activity of sulfate reduction and H2S pro- Lake Nakaumi, with readily available SO4 and reactive duction.
    [Show full text]