河湖的

Gatineau Park in 360 degrees is a free screensaver that includes 5 wonderful 360 interactive panoramic movies of Gatineau Park, Canada: Carman Lake, Brown Lake, Lac La Peche, Giant's Trail and The Ruins on Meech Creek.

加蒂诺公园， 360度是一个免费的屏幕保护程序，其中包括5美好的360 互动全景电影的加蒂诺公园，加拿大：映红湖，布朗湖，拉丁美洲和加勒比香格里拉peche ，巨人的径及废墟上meech河。

A young margay cat peeks over a step at the Smithsonian Tropical Research Institute station on Barro Colorado, a forested island in the Panama Canal waterway. The island rises from Lake Gatun, which formed in 1907 when the Chagres River was dammed during construction of the canal.

一只幼虎从台阶上窥视Smithsonian热带研究所在科罗拉多Barro岛上的试验站，这是巴拿马运河水道上一个被森林覆盖的岛屿，在Gatun湖上立出，湖是1907年在建造运河时围堰Chagres河而形成。

The Severn River is the longest river in Britain, which is about 338km long.

最重要的河为泰晤士河，最大的湖为内伊湖。

Here can see have high Li Gong Shan as ice snow the Great Wall main ridge, can watch the drop water river two waterfalls that have the reputation of " the cloudy mountain water of dartlike weapon " on mountain climb , reach the ice of high mountain to lose lake —— take order lake.

这里可以看到有如冰雪长城的高黎贡山主山脊，可以观赏到有&阴山镖水&之誉的滴水河双瀑布，往山上攀登，即可到达高山冰蚀湖——听命湖。

By studying reservoir rock characteristics, diagenesis and physical property, investigation showed that there were distributary channel, branch channel, mouth bar, distal bar, sand sheet, lakeshore, shallow lake and limestone flat . we concluded that the reservoir of N1～N21 is low porosity and permeability reservoir with the types of primary porosity and secondary intergranular porosity, which is in the early diagenetic stage B into the late diagenetic stage A subperiod. The role of effecting reservoir physical property is deposition, cementation, dissolution and tectonic rupture. After researching of reservoir, we divided it into three categories and division the favorable facies belt and relatively favorable. We think that the favorable facies belt is braided river delta front and partly shallow lake in east of the Fault Ⅶ. favorable reservoir is in the first and the second class.

进一步研究了本区碎屑岩储层的岩石学特征、成岩作用特征、物性特征，研究认为该区储集体类型有分流河道砂体、分支河道砂体、河口坝、远砂坝、席状砂砂体、滨湖砂滩、浅湖砂坝砂体及灰坪；N1层属于低孔、特低渗储层，孔隙类型以原生、次生粒间溶孔为主；分析了影响储层物性的因素主要为沉积作用、胶结作用、溶蚀作用和构造破裂作用；进行了储层评价与有利相带预测，将储层分为三类并划分了有利区带、较有利区带，认为Ⅶ号断层以东的辫状河三角洲前缘亚相和部分浅湖亚相是N1的有利储集相带，储层以Ⅰ、Ⅱ类为主。

In a natural state, the Junggar Basin, inland river sub - 4 Drainage District:(1) Buluntuohai water; Health ulungur water, out of Yamaguchi average annual runoff of 11.3 billion cubic meters, the last 10 years into the lake for many years for the most amount of 600 million cubic meters, most juveniles is only B 01.5 billion cubic meters; in 1970 from Elgin Qi period after the introduction of part of the river water, B the amount of water level decline eased Buluntuohai.

在自然状态下，准噶尔盆地的内陆河分为4个排水区：（1）布伦托海水系；汇乌伦古河水量，出山口平均年径流量113亿立方米，最近10年入湖水量最多年为6亿立方米，最B少年仅015亿立方米；1970年后从额尔齐期河引进部分水B量，缓和了布伦托海的水位下降。

Results River, braided delta, delta, lake and deep lake turbidite are developed.

结果 研究区在延长期发育的沉积体系有河流、辫状河三角洲、曲流河三角洲、湖泊及深湖浊积岩。

They have curiously come from the Balkhash foreland, and perhaps, from the rivers Tshu and Saryssu, and from the area of Lake Saisan.

它们是从巴尔喀什湖边缘或者 Tshu and Saryssu河，以及 Saisan湖地区来的。

The depositional facies are normal alluvial fan, braided river, meadering river, swamp and littoral and shallow lake.

沉积相类型有正常沉积的冲积扇相、辨状河相、曲流河相、沼泽相和滨浅湖相。

"Chu:river of southern Central asian U.S.S.R. flowing about 1,126 km (700 mi) eastward into Issyk-Kul."

&朱河：苏联中亚部分南部的一条河，流程约1，126公里(700英里)，向东注入伊斯库尔湖。&

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。