The far side of the crest was a long, gradual downslope.

山頂?shù)倪h(yuǎn)側(cè)欧美综合亚洲，是一條很長(zhǎng)的人人摸人人干人人操97、通向下面的斜坡，坡度不是很陡可以直接观看的黄片。

This paper presents the surveyed results of some typical moraine slopes along the highway. A laser profiler and a total station were used in the topographical survey. It is obvious that the slopes are high and steep, but they are stable.

作者對(duì)川藏公路沿線(xiàn)部分典型的剖面進(jìn)行了量測(cè)日本理论电影A片中文字幕网站，所量測(cè)的剖面雖然只是整個(gè)斜坡的一部分，與經(jīng)驗(yàn)數(shù)據(jù)相比8x永久在线视频，仍表現(xiàn)出高陡的特征86精品自拍，而且很多邊坡在既高且陡的形態(tài)下仍能保持穩(wěn)定。

To cover with a pavement .Some hours into the journey, the road suddenly became unrideable, the pavement giving way to dirt, then pebbly gravel and then, on a very steep pitch, to a mass of sharp, broken boulders.

在我上路走了幾個(gè)小時(shí)以后一级片无遮挡JJ抽插视频，道路突然變得不能騎車(chē)行進(jìn)了，鋪砌的路面變成了泥土路国产美孰女乱又伦Av，接著是多卵石的沙礫路面国产小呦，然后在一片很陡的斜坡上道路變成了大堆尖棱、破碎的石塊肏屄免费视频。

The landform obviously had controlled the covered ratio, occurrence, morphological feature of the cobaltrich crusts. The very gentle or steep slopes of seamounts are unfavourable to the growth of the cobaltrich crusts. The crusts mainly are platy on the steep slopes of seamounts, and rippled or pillow on the gentle slopes. The platy crusts mostly appear on the slopes of the seamounts, but the pebble crusts or cobaltrich nodules on the flat or low areas.

地形對(duì)富鈷結(jié)殼覆蓋率国内自拍日韩在线观看网站、產(chǎn)狀、形態(tài)具有明顯的控制作用狼友偷拍视频，海山坡度太緩综合网图、太陡均不利于結(jié)殼的生長(zhǎng)發(fā)育；在海山坡度較大處生長(zhǎng)的結(jié)殼多呈平板狀3及片黄色福利午夜网站，而在坡度較小處生長(zhǎng)的結(jié)殼多呈波紋狀或枕狀人人干免费看片国产；海山的斜坡上生長(zhǎng)的多為板狀結(jié)殼，而在平坦低洼處則有利于礫狀結(jié)殼www.猛黄色网站、鈷結(jié)核的生長(zhǎng)發(fā)育欧美亚洲视频一区。

The slope averages about1 in 30, but contains steep, probably vertical, cliffs, and gentle sediment-covered terraces.

斜坡的坡度平均約為30分之1，但包括陡的，很可能是垂直的峭壁和覆蓋著沉淀物的坡度不大的階地黄色视频唯爱网。

It has now become a very steep slope.

如今91在线网站观看，它已成為一個(gè)非常陡的斜坡。

This paper points out that the deep fractures are the result of the coupling of endorgenic and exogenic geological processes by unloading of river valley and releasing of high geostress.

由于強(qiáng)烈的內(nèi)外動(dòng)力地質(zhì)作用人人摸人人摸摸人人操人人操，這些地區(qū)形成了高山聳立18岁禁止访问网址、溝谷深切的地貌景觀，高山峽谷區(qū)的高陡巖質(zhì)斜坡變形與穩(wěn)定將是工程建設(shè)所面臨的主要工程地質(zhì)問(wèn)題之一亚洲Av库在线观看国产。

On the northern slope, there is a low horse hoof-shaped crater that widens to the north.

山陵從東邊的主峰開(kāi)始向西延伸日韩精品视频无播放器在线观看免费，到西邊山峰變得低矮，北側(cè)斜坡上形成了較淺的馬蹄形口亚洲中文刮吗一本到午夜，西側(cè)斜面也緩慢形成小火山口五月丁香六月激情欧美综合不卡，東南側(cè)的山坡寬而陡，呈現(xiàn)凹陷形欧美乱人伦高清视频中文字幕。

The man watched him go, limping grotesquely and lurching forward with stammering gait up the slow slope toward the soft sky-line of the low-lying hill.

他的伙伴干瞧著他久久久国产精品无码aa，只見(jiàn)他古里古怪地一瘸一拐地走著，跌跌撞撞地前進(jìn)黄色网站在观看18181818禁，搖搖晃晃地登上一片不陡的斜坡www..com日本，向矮山頭上不十分明亮的天際走去。

Its surface is narrow and surface sediment is little silted. Underwater delta of Yellow River has formed three landforms units at present: smooth and wide shoal above -5m water level婷婷五月丁香基地、 steep and thin under water slope in-5—10m and smooth bottom bed beneath-10 m.

其水下三角洲經(jīng)過(guò)長(zhǎng)期的沖刷侵蝕色色色视频成年网站，目前已經(jīng)形成了-5m以淺坡緩、灘寬的水下淺灘国产黄色片av、-5—-10m之間灘窄黄页网站激情视频、坡陡的水下斜坡和-10m以深平坦的底床三個(gè)地貌單元。

contour line：等高線(xiàn)

等高線(xiàn) (Contour line)是表示地勢(shì)起伏的等值線(xiàn). 它是地面上高程相同的各相鄰點(diǎn)所連接成的封閉曲線(xiàn),垂直投影到平面上的圖形. 一組等高線(xiàn)不僅可以顯示地面的高低起伏,而且還可以根據(jù)等高線(xiàn)的疏密和圖形判斷地貌的形態(tài)類(lèi)型和斜坡的坡度陡緩.

gentle slope：不太陡的斜坡

gentle nature溫和的性情 | gentle slope不太陡的斜坡 | 19. patience n.容忍(忍耐力,耐心)

steep slope：陡峭斜坡;陡峭山坡

steep ramp 陡斜路;陡坡道 | steep slope 陡峭斜坡;陡峭山坡 | Steering Committee on Land Supply for Housing 房屋用地供應(yīng)督導(dǎo)委員會(huì)

steep ramp：陡斜路陡坡道

steep gradient 陡坡度 | steep ramp 陡斜路;陡坡道 | steep slope 陡峭斜坡;陡峭山坡

steeply dipping：陡傾斜

steep slope 陡峭斜坡,陡峭山坡,陡坡 | steeply dipping 陡傾斜 | steering committee 督導(dǎo)委員會(huì)