地理环境的整体性和差异性高考真题训练.pdf

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1、优秀学习资料欢迎下载地理环境的整体性和差异性高考真题训练(013 高考题新课标1)图 2为 45oN附近某区域的遥感影像，其中深色部分为植被覆盖区，浅色部分为高原荒漠区；终年冰雪覆盖的山峰海拔3424 米，距海约180 千米.读图 2，完成46 题。1 导致图示区域内降水差异的主导因素是A 大气环流B 地形C 纬度位置D 洋流2 该区域位于A 亚欧大陆太平洋沿岸地区B 亚欧大陆大西洋沿岸地区C 北美洲大西洋沿岸地区D 北美洲太平洋沿岸地区3 该区域中山脉西坡山麓的自然植被属于A 常绿阔叶林B 常绿硬叶林C 针阔叶混交林D 草原(2013 高考题大纲版)某种生物的种密度指单位面积该种生物的个体数

2、量。图2 为北美洲部分地区某种动物的种密度等值线图。据此完成1011 题。4H、K、Q、R四地中，该种动物的种密度可能相等的两地是A H、R BQ、R CQ、H DH、K 5该种动物的种密度与年均温的空间分布呈正相关的地区是墨 西 哥湾140 160 180 QMNRSHk大西洋太平洋图 2 100 200 160 180 140 160 180 120 60 80 100 墨西哥湾160 高原荒漠区植被覆盖区山峰山脉01020kmN 图 2-第 1 页，共 7 页精品p d f 资料 可编辑资料-优秀学习资料欢迎下载A Q、R之间BN、M之间CS、R之间DS、K之间(2013 高考题江苏卷)

3、国家领导人近期出访了俄罗斯等四国，行程如图2 所示。读图回答 56 题。6从俄罗斯到南非经过的自然带类型主要有温带草原带热带雨林带热带草原带热带荒漠带A BCD7我国在非洲投资时优先选择的产业类型有A 资源密集型和劳动密集型B劳动密集型和资金密集型C 资金密集型和技术密集型D技术密集型和资源密集型(2013 高考题山东卷)图 2 示意我国植被的地带性分布，读图回答3 4 题8图中为A 草原 B 荒漠 C 针叶林 D 针阔混交林9我国东部森林植被的东西宽度在南北方向发生变化，其主导因素是A 纬度 B 洋流 C 地形D 季风(2013高考题四川卷)读 图 2，回答 34 题。1511R 0200米

4、200500 米5001000 米10002000米海洋河流图 2 图例-第 2 页，共 7 页精品p d f 资料 可编辑资料-文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9

5、V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 Z

6、Q5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5

7、R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文

8、档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV

9、8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U

10、1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10优秀学习资料欢迎下载10 图示区域从沿

11、海向内陆，陆地自然带依次为热带雨林带、热带草原带。给该区域带来降水的主导风是A 东北风B 西南风C 东北风D 东南风11 R 河段A 流量季节变化大B春汛明显C 河流堆积作用强D 河谷横剖面呈槽型(2013 高考题四川卷)图 4 示意我国黄土高原某地林木的分布状况，图中相邻等高线之间高差均为30 米。读图回答7 8 题。图 4 12 林木生长与土壤水分条件相关，图中林木密集区位于A 鞍部B 山谷C 山脊D 山顶13 图示区域内东、西两侧最大高差可能是A 156 米B 178 米C 220 米D 255 米(2013 高考题新课标2)图 2 示意某地区年均温的分布，读图2，完成 68 题14影响

12、该地区年均温分布特征的主要因素是A 台风B海陆分布C地形D大气环流15图示四地中，年降水量最低的是A 地B地C 地D 地16樟树是亚热带常绿阔叶林的优势树种。图示四地中，可能有樟树集中分布的是A 地B地C 地D 地（2014 广东卷）3、沙漠中植被的出现可对沙丘产生一定的影响。其主要作用机制是 A、降低风速进而增加风沙流对地表的侵蚀北回归线22181424 1024 河流等温线121 E 24 N-第 3 页，共 7 页精品p d f 资料 可编辑资料-文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9

13、 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4

14、I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U1

15、0文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:

16、CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V

17、2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5

18、HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7

19、M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10优秀学习资料欢迎下载 B、增加风沙流中颗粒物的含量而减少堆积 C、促进风沙流携沙能力的增强而增大侵蚀 D、拦截风沙流中的悬浮颗粒物并形成沉降（2014 重庆卷）图 1 示意三峡区滑坡频率（月滑坡次数占全年滑坡次数的百分比）与月均降水量关系。读图1，完成 5-7 题。5.图 1 表明该区滑坡多发的诱因是：A.年

20、降水量少 B.夏季降水多 C.冬季降水少 D.降水季节分配均匀6.三峡水蓄水后岸滑坡几率增大，主要是因为水水体的 A.流速减小 B.流速增大 C.水位涨落 D.水位稳定7.三峡水蓄水后区渔业天然捕捞量增加，其主要原因是 A.水生植物增加 B.水体富营养化 C.鱼的种类增加D.水面面积扩大（2014大纲卷）图 2 中岛于1983 年火山爆发，植被消失殆尽。1987 年，该岛上已有64种植物生长旺盛。据研究，百年之内该岛上的天然植被就可以恢复。据此完成46 题。-第 4 页，共 7 页精品p d f 资料 可编辑资料-文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U

21、10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码

22、:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5

23、V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5

24、 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G

25、7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X

26、9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q

27、4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10优秀学习资料欢迎下载4.岛天然植被类型属于 A.热带雨林 B.热带草原 C.亚热带常绿硬叶林 D.亚热带常绿阔叶林5.与相同植被类型的大陆地区相比，岛植被恢复迅速的独特条件是 A.海拔高 B.种源丰富 C.火山灰深厚 D.光照充足6.岛处于 A.印

28、度洋板块与太平洋板块界线的东侧 B.印度洋板块与太平洋板块界线的西侧 C.亚欧板块与印度洋板块界线的北侧 D.亚欧板块与印度洋板块界线的南侧（2014山东卷）图 3 为我国某区域冬季某日8 时至此日8 时的降雪量和积雪深度分布图，该时段该区域风向主要为偏东风，云量分布差异不明显。完成5-7 题。5、造成该区域东西部积雪深度差异的主要因素 A、降雪量 B、温度 C、光照 D、地形6、图中 M地积雪深度低于周围地区，该地可能是 A、农田 B、林地 C、城区 D、乡村-第 5 页，共 7 页精品p d f 资料 可编辑资料-文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R

29、7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档

30、编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8

31、U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1

32、D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX1

33、0G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V

34、8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ

35、5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10优秀学习资料欢迎下载7、道路积雪会影响交通，应用GPS技术可以 A、获取道路积雪影像数据 B、解译积雪遥感影像 C、分析道路积雪空间分布 D、确定带救援车辆位置(2012 北京卷)图 2 为某山地的垂直带谱示意图。读图，回答第45 题。图 2

36、4图中所示山地A各自然带的界线随季节变化而移动B北坡热量条件差，林带上界比南坡低C南坡冰雪带下界因降水量大而较低D南北坡山麓水平距离造成基带差异大5该山地位于A喜马拉雅山脉 B天山山脉 C祁连山脉 D昆仑山脉(2014 海南卷)21.阅读图文材料，完成下列要求。（10 分）在冷湿环境下，未完全分解的 植 物 残 体 逐 级 堆 积，形 成 泥 炭。图9所 示 岛 屿 泥 炭 资 源 丰 富。分析该岛屿适宜泥炭形成的冷湿环境的成因。（2014上海卷）（十九）读澳大利亚自然带分布示意图，回答问题。（10 分）-第 6 页，共 7 页精品p d f 资料 可编辑资料-文档编码:CV8U5V2U1D5

37、 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G

38、7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X

39、9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q

40、4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U

41、10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码

42、:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5

43、V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10优秀学习资料欢迎下载在地理位置、地形地势、大气环流和洋流等因素的共同影响下，澳大利亚大陆形成了独具特色的半环状自然带格局。47、判断 A、B两地所属的自然带类型，解释导致这两个自然带特征差异的主要原因

44、。48、阐述图中B、C、D、三地水分差异及其主要原因。49、以 C地所在的自然带为例，分析如何因地制宜发展农业。-第 7 页，共 7 页精品p d f 资料 可编辑资料-文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:

45、CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V

46、2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5

47、HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7

48、M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9

49、 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4

50、I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U10文档编码:CV8U5V2U1D5 HX10G7M9V8X9 ZQ5Q4I5R7U1