That dried-up, skinny old codger could give an informal lecture that took you from the Qinghai-Tibet Plateau all the way down to Hainan Island, or from the Taihang Range to Huangguoshu Falls.

那干瘦老頭居然能從青藏高原扯到海南島，從太行山扯到黃果樹瀑布。

At the new period, the successful the writer the that attracts the by the and the describes one the square the Water the and soil the that the oneself the fall in the love the not the in the minority, the be the like the company the of the even the and the cave style the of writing the state series," the high northeast of the country" that Moyan, the LI3 RUI4's" the go the mountain too", peninsular" WaLizhen " the of east the of ZHANG the WEI3 JIAO, what WANG2 AN YI4 build is flexible to work properly etc. that the dynamic civilian turns big Shanghai, all giving person leave the impression of the hard detrition again.

在新時(shí)期以來，著意與描寫自己所鐘情的一方水土的成功作家并不在少數(shù)强奸a片久久a，像賈平凹筆下的商州系列，莫言的"高密東北鄉(xiāng)"一区无码在线，李銳的"太行山"未满十八18禁止观看网站，張煒膠東半島的"洼貍鎮(zhèn)"，王安憶朔造的鮮活靈動(dòng)的平民化大上海等影音先锋操逼网，都給人又留下了難以磨滅的印象my国产精品免费。

A mesoscale convergence line, which is formed by downslope wind from the Taihang Mts. Converging with southwest warm humid wind in front of a surface trough, induces the release of the CAPE and initiates convection and organizes the convective cells into a squall line.

由于太行山地形影響而產(chǎn)生的下坡風(fēng)與地面低壓槽前的西南暖濕氣流相匯合，形成中尺度輻合線99se在线播放，觸發(fā)了不穩(wěn)定能量的釋放天天婬色婬香综合网站日本，產(chǎn)生對(duì)流并由中尺度輻合線組成颮線。

However, if there is no way but only the wisdom, as will be driving, navigable, they themselves can control the reins can show off too, such as strings, can Quant shake like wind, racing along a flat plain or a pier, as if in their own palm of your hand, but an experience to narrow the Taihang Mountains, rapids rapids of the storms, will do nothing to screaming in pain, these people do not capsize, do not overturn the really very small.

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Surface heating weakens the foehn wind speed but makes it stronger at night time when radiative cooling begins.

太行山東坡顯著的階梯狀下沉地形是焚風(fēng)生成的重要影響因素99久久国产精品无码免费。

A preliminary study on laws of soil and water losses in gneiss, which is the main type of rocks in Taihang, was carried out in this paper on the bases of examination data, survey of flood and historic statistic data.

根據(jù)試驗(yàn)觀測(cè)數(shù)據(jù)和洪水災(zāi)害考察結(jié)果，結(jié)合歷史統(tǒng)計(jì)資料www.jizz.com中国破处，對(duì)河北太行山的主要類型巖石－片麻巖低山區(qū)的水土流失特點(diǎn)進(jìn)行了初步研究免费黄色网业大全。

The LVZs in lower crust in North China Plain, Taihang Mountain and Shanxi Graben System present the clear NNE orientation. It is coincident with the orientation of the surface geological structures.

地殼下部的速度異常在華北平原地區(qū)、太行山地區(qū)和山西地塹系呈明顯的北北東向分布一级做a爱过程免费视频韩国，與區(qū)域地表的構(gòu)造走向十分吻合黄片69。

During the Pliocene to early Pleistocene strong NW-SE crustal extension resulted in disintegration of the planation geomorphology and formation of a graben basin in the area.

上新世至早更新世時(shí)期，強(qiáng)烈的NW-SE向地殼引張導(dǎo)致太行山隆起南段夷平地貌的解體和地塹盆地的形成日韩手机在线视频。

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The Geopark is situated at the junction of the north east trending Yanshan tectonic belt and the north-north east trending Taihanshan tectonic belt ,and is one of the typical intracontinental orogenic belts in China having complicated geological background.

園區(qū)地處北東向燕山構(gòu)造帶和北北東向太行山構(gòu)造帶銜接區(qū)內(nèi)中文精品日韩欧美在线观看免费，是我國(guó)陸內(nèi)造山帶的典型地區(qū)之一，具有復(fù)雜的地質(zhì)背景爱搞网站无遮挡。