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Is more than one source of the Nile River, the farthest source is called the Kagera River, which from Tanzania Karma Tanganyika Hubei side outflow into Lake Victoria, and from the north shore of Lake Jinja out into the Great Rift Valley, forming the famous Murchison Falls (later changed called kabarega falls).
尼罗河是一个多源河,最远的源头叫卡盖拉河,它从坦噶尼喀湖北端流出,注入维多利亚湖,又从湖的北岸金贾流出进入东非大裂谷,形成著名的默奇森瀑布。
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Bennett.That was my commission,and I set out to Africa intending tocomplete Livingstone's explorations,also to settlethe Nile problem,as to where the headwaters ofthe Nile were,as to whether Lake Victoria consist- ed of one lake,one body of water,or a number ofshallow lakes; to throw some light on Sir SamuelBaker's Albert Nyanza,and also to discover theoutlet of Lake Tanganyika,and then to find outwhat strange,mysterious river this was which hadlured Livingstone on to his death—whether it wasthe Nile,the Niger,or the Congo.
贝内特。那就是我的使命,我动身去非洲意欲完成利文斯通的探险任务,还要解开尼罗河之谜,弄清尼罗河的源头在哪里,维多利亚湖仅由一个湖泊、一个水体构成还是由若干浅湖组成;弄清塞缪尔·贝克爵士发现的阿伯特湖;还要找到坦噶尼喀湖的出口,然后找出那条诱使利文斯通走上死亡之路的奇怪、神秘的河流是尼罗河,尼日尔河,还是刚果河?
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Some innovative results are listed below:1、According to the lithologic characters,lithofacies,genetic classification and the geomorphy,the Quaternary system is divided into piedmont-gully\'s and plain\'s. The piedmont-gully\'s Quaternary sediment,which is about 3~20 meters in thick,is in the western hills of the study area.The plain\'s Quaternary sediment is widely distributed in the study area,which is about 30~60meters thick and become thicker from southwest to northeast.2、The Quaternary sediments of plain can be divided into five sedimentary cycles.The Late Pleistocene series Quantan group,at the bottom of the Quaternary System,is constituted by a fluvial facies-river and lake facies sedimentary cycle. The Late Pleistocene series Jiashan group,at the middle of the Quaternary sediment, is constituted by two fluvial facies-neritic facies-river and lake facies sedimentary cycles.The Holocene series Binhai group,at the upper of the Quaternary sediment, is divided into three parts,the under layer and middle layer are constituted by two littoral facies-river and lake facies sedimentary cycles,the upper layer is constituted by paludal facies,which was deposited at the lower-lying land like West Lake, Jiangcun-Gu dang,Xianghu lake,and coastal-estuary facies in other area.3、Folding and fault activities were weak in Quaternary and the tectonic activity had little influence on the Quaternary sedimentation.The ancient landforms,the evolvement of the river system and transgression were the main elements which controlled the Quaternary sedimentation in Hangzhou.The ancient landforms formed the basis of the Quaternary sedimentation.The evolvement of the river system and transgression individually or jointly controlled the Quaternary sedimentation of this area.4、The alternation of the climate was the main reason for the evolvement of the river systems and transgression,and it\'s also the reason why the Quaternary system of Hangzhou has the special sedimentary structure which is called soft interbed with hard layers.
通过研究取得了以下成果:1、根据岩性、岩相、成因类型和地貌特点,将本区第四系划分为山麓沟谷区沉积和平原区沉积:山麓沟谷区第四系主要分布于西部丘陵地区,厚度较薄且变幅大,一般厚3~20m;平原区第四系广布分区,由南西向北东逐渐增厚,一般厚30~60m.2、平原区第四系自下而上大体由五个完整或不完整的沉积旋回构成:底部上更新统全塘组,由河流相—河湖相的沉积旋回构成;中部上更新统嘉善组,由河流相—浅海相—河湖相两个沉积旋回构成;上部全新统滨海组,其下中两段由滨海海湾相—河湖相的两个沉积旋回构成,上段由西湖、蒋村—古荡、湘湖等低洼处沉积的湖沼相和其他地区沉积的滨海河口相构成。3、第四纪以来,研究区内褶皱、断裂活动微弱,构造运动对第四系沉积的影响不大,古地形、古水系的发育、变迁和海侵是杭州市第四系沉积的主要控制因素:古地形构成了第四系沉积的基底,水系与海侵在其后的不同阶段或分别或联合的主导了区内的第四系沉积。4、水系的发育、变迁和海侵的共同原因是天气变化,正是由于第四纪以来"冷热交替"的天气特点形成了杭州市第四系"软硬互层"的特殊沉积结构。
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At the municipal garden, the city will improve the construction of six major functional areas and intensify environmental governance and beautification, greening efforts, dredging water, the pleasance green building and achieving overall urban image "three years to upgrade, five changes," to Anyang become a beautiful environment, and a healthy ecosystem, transport facilities, living happy and harmonious are advised humanities in cities; Speed up urban road network construction, complete transformation of governance alley project, increase import and export of urban rectification, improve urban infrastructure facilities; urban greening and water systems around the center building, and continue to promote cycling River, the development of river flood management, a comprehensive management of urban rivers absence, the Huan River River scenery tourism belt development.
在市政园林方面,该市将完善六大功能区建设,加大环境治理和美化、绿化力度,疏浚水系,加快游园绿地建设,实现城市整体形象"三年提升、五年大变",使安阳成为环境优美、生态良好、交通便利、生活舒畅、人文和谐的宜居城市;加快市区路网建设,完成小巷改造治理工程,加大市区出入口的整治力度,完善城市基础设施配套;围绕中心城区绿化及水系建设,继续推进环城河治理,开发治理洪水河,抓好市区河湖坑塘综合治理,加快洹河风光旅游带开发建设。
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The last interglacial strata sequence of Milanggouwan stratigraphic section in the Salawusu River valley has recorded 8^5 sedimentary cycles of aeolian sand alternatively interlaid with fluvio-lacustrine facies or paleosols.
萨拉乌苏河流域米浪沟湾剖面末次间冰期层系记录了8 5个风成的古砂丘砂与河湖相或/和古土壤构成的沉积旋回。
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As there is no water gate across the ring-river and vertical-river, the application of synchronous conservancy would brought flow short circuit, the suggestion was made that nonsynchronous conservancy is more suitable at present.
但对于边引边排模式而言,前提是下在链河上设置闸门,形成引水直接入湖的人工导流条件,以避免现状条件下引水水量通过链河短路而不进入滴水湖。
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There are three genetic types of mineral deposits in the Beiya ore district:① Cu-Au polymetallic deposits related to alkaline porphyries, comprising porphyritic Cu-Au deposits and polymetallic skarn deposits related to quartz-albite porphyry and quartz-K-feldspar porphyry;② Fe-Au deposits related to gabbro or basalt magma, consisting of magmatic Fe-Au deposits and sedimentary polymetallic deposits formed in caves and lakes; and ③ palaeo-placers formed at the weathering surface, in lakes and in karsts.
北衙金矿有3种成因不同的矿床:①与碱性斑岩有关的铜金多金属矿,包括与石英钠长斑岩和石英正长斑岩有关的斑岩型铜金矿床和矽卡岩型多金属矿床;②与辉长-玄武岩浆有关的铁金矿床,包括熔浆型铁金矿床和喷流沉积型多金属矿床,后者又有洞穴和湖相沉积环境之分;及③古砂矿,有古风化壳型砂矿、河湖相古砂矿和洞穴沉积古砂矿。
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Shrinking lakes and rivers, the Yellow River drying up in the Yellow River from 1972 to the beginning of 1998 there disconnection of the 27 years, the Yellow River Lijin station stop in a total of 21, reached four years of stop-off frequency, for a total disconnection 1,050 days, the average Each year 50 days disconnection, 1997 devascularization 226 days, up to 704 km river drying up of the lower reaches of the chief of 90%.
河湖萎缩,黄河断流黄河从1972年开始出现断流到1998年的27年间,黄河利津站共有21年发生断流,断流频率已达四年五断,共计断流1050天,平均每个断流年份50天,其中1997年断流226天,断流河段长达704公里,占下游河段总长的90%。
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Just upstream from the town of Del Rio is a dam that holds back water from the Rio Grande and two other rivers to form the 263 square-kilometer reservoir called Lake Amistad .
戴尔李欧镇上游处有一座水坝,其水源有二:一为李欧河,再者为源自鄂米斯达湖的两条河,此湖面积达263平方公尺,宛如一座储水池。
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There was a heated dispute between the merit and fault of water hyacinth on purification or pollution in water-bodies.
凤眼莲在城市河湖的污染与净化中的是非功过争议很大,双方意见均有部分正确,但各有片面性。
- 更多网络解释与河湖的相关的网络解释 [注:此内容来源于网络,仅供参考]
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eat up phr:吃完,吃光
1427 as conj 因为,由于 | 1428 eat up phr. 吃完,吃光 | 1429 bank n (海,河,湖的)岸,堤
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fluviology:河川学/河流学
fluviolacustrine 河湖的 | fluviology 河川学 河流学 | fluviomarine 河海栖
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Rhine:萊因河
(这可能与全球气候有关)莱因河(Rhine)源于阿尔卑斯山中的一个湖,湖的名字叫constance.位于德国、瑞士、奥地利三国交界处. 湖水是阿尔卑斯山上融化流下的雪水. 雪水出湖西行成河,沿德法边界绕过德国西南部的"黑森林"地区,
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Sharlotta Vespers:夏洛塔.维斯帕 巴沙多尼盗贼公会头领之一,帕夏巴沙多尼的情妇
Shaongarne River 盛冈河 流入都尔登湖的河 | Sharlotta Vespers 夏洛塔.维斯帕 巴沙多尼盗贼公会头领之一,帕夏巴沙多尼的情妇 | Shining White 耀白 哥林泰河上一个小镇
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fluvioglacial:冰水的
fluviodeltaic 河成三角洲的 | fluvioglacial 冰水的 | fluviolacustrine 河湖的
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fluviograph:河流水位自动测录仪 水位计
fluvioglacialterrace 冰水阶地 | fluviograph 河流水位自动测录仪 水位计 | fluviolacustrine 河湖的
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fluviolacustrine:河湖的
fluvioglacial terrace 冰水阶地 | fluviolacustrine 河湖的 | flux 焙剂
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fluviomarine:河海的
fluviolacustrine 河湖的 | fluviomarine 河海的 | fluvioterrestrial 陆上河流的
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Shaanxi and Zhejiang to see wild red and yellow:陕西和浙江等见到野生的红黄色的鲫鱼
还不断有人在我国安徽 Anhui Province in China has als... | 陕西和浙江等见到野生的红黄色的鲫鱼 Shaanxi and Zhejiang to see wild red and yellow | 这类鲫鱼生活在江,河,湖,池塘Such carp living in the river ,...
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St. Lawrence:圣劳伦斯河
蒙特利尔是一个河湖上的岛,位于圣劳伦斯谷地,是世界上最处于内陆的海港. 它像个艺术珍品似的依偎在皇家山(Mont Royal)与圣劳伦斯河(St Lawrence)旁 ,距魁北克首府魁北克市约200公里,渥太华东约150公里.