地理事物分布特征的描述.pdf

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1、1 地理事物分布特征的描述及成因分析总体来说，地理事物的分布形状分为点线面三大类；其特征要从位、数、形三方面来描述，每一个具体特征都隐含着不同的原因，要学会具体问题具体分析。位置：绝对位置有经纬度、高程；相对位置指“在,地区,方向或与,平行或沿,分布”；形状看延伸方向、弯曲方向得总体形状（团块状、条带状）；数量指数值大小、递变规律、变化快慢（梯度）、极值（闭合中心）、面积大小、范围宽窄。一、点状地理事物的描述。（1）点的疏密:均匀一致；分布不均（总分结构描述），沿什么线（或面）密集；沿什么线（或面）稀疏。（2）点的位置：在-线（沿河谷、海岸线、边境线、交通线）上分布；在-面（面的什么位置）上分

2、布。（3）点的数量：多少（极值最多、最少、最集中等），反应的规律（哪多哪少）。(4）点的大小:代表的含义(如城市等级)。（5）其他：点的动态变化提示：看图说话，突出重点，因题而宜（不一定要面面俱到），分值决定要点（2 分/点）【例题 1】（08 天津）甲区域的城镇分布有明显特征。请你归纳出三点。（6 分）【例题 2】（2011 全国课标卷）下图示意2007年中国大陆制造业企业500 强总部的空间分布。读图，回答下列问题。简述中国大陆制造业企业500 强总部空间分布的特点。（8 分）【例题3】读德国和日本不同等级城市分布图，完成下列要求。2（1）比较德国和日本城市的等级和分布特点，并说明其形成原

3、因。（22 分）（2）说明德国和日本地理位置的主要差异（4分）。（3）概括德国和日本经济的共同特征。二、线状地理事物的描述1、描述一条等值线文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6

4、K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5

5、A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV

6、5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6

7、O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档

8、编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6

9、H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O63 突出位置、延伸方向，凸出

10、（弯曲）方向；明显转折时要分段描述。2、描述一组等值线（1）变化趋势：由总体延伸方向得递变规律，向,方向逐渐变大（变小）（2）分布范围：最大到最小的范围是,（3）分布 凸变：某地区偏大（小）、极值或特殊值。【例题 1】读某地等温线图，回答问题。（1）描述图中 -10 C等温线分布特征。（6 分）【例题 2】下图中的虚线为一月0等温线。描述图中0等温线的走向及影响因素【例题 3】描述图中10等温线的走向，并说明其原因。【例题 4】（08 年北京卷变式题）读图回答下列问题。文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K

11、1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A

12、10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5

13、C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O

14、9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编

15、码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H

16、4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T

17、3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6（3）指出图示的年降水量分布特征，并分析原因。【例题5】下图是我国某区域10积温等值线图（单位：）。描述4500 等积温线的走向并说出影响因素。【例题 6】描述下面图示区域气温年较差的分布特征(6 分)文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码

18、:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4

19、V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3

20、 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1

21、M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A1

22、0 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C

23、10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9

24、O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O65【例题 7】（2011 年山东卷）下图为1969 年 2008 年山西省长治市寒潮发生总次数等值线图。读图回答问题。指出该区域寒潮发生总次数的空间分布特征，并说明该特征形成的主要影响因素。(8分)【例题 8】阅读下列材料，回答问题。描述图示地区干燥度分布规律

25、，并简析其成因。（8 分）【例题 9】读我国某区域“日平均气温5的积温”图，完成下列各题：（14 分）（1）从图中信息判断，该地区地势特点是_，判断的依据是_（4 分）（2）描述 该地等积温线的分布特点。并简要说明理由。（10 分）909530600 400 200 100 拉萨图例国界线河流等积温线600 文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM

26、6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E

27、5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 Z

28、V5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U

29、6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文

30、档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX

31、6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B

32、5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O66【例题 10】描述北美洲年温差等值线在西部分布特点,并说明影响因素。（8 分）【例题11】（1）甲图方框所示地区某季节的气温分布如图乙所示，简述等温线的分布规律（6 分）乙甲20o20o20o20o10o20o10o10o10o20oBA10方框区域等温线示意图（单位文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4

33、V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3

34、 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1

35、M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A1

36、0 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C

37、10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9

38、O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码

39、:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O67【例题 12】读下列材料图,结合你所掌握的知识，回答下列问题。材料一某区域图和地形剖面与降水量关系图（1）乙图大致为甲图从A 至 B 一线附近地形剖面图，若图中虚线表示当地一次特大暴雨量分布状况，据图判断中最大暴雨量分布的地区海拔高度约为多少米？()（2 分）A1800 B700 C200 D500（2）试描述材料一中的图乙中降水量线的变化规律，并分析

40、其原因。（8 分）（3）试叙述图示区域的自然地理特征，并根据当地的自然地理特征，说明该区域自然条件对发展农业的有利因素。（12 分）（4）影响 A 地气温差异的主要因素（）（2 分）A海陆位置B地势C纬度位置D太阳辐射（5）简述乙河流的水文特征。（8 分）（6）根据图中所给信息，说明该区域农业发展的潜力及农业开发中应注意的问题。（8 分）（7）简述该区域发展小水电建设的有利条件及环境意义。（8 分）三、面状地理事物的描述乙甲文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档

41、编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6

42、H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5

43、T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6

44、K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5

45、A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV

46、5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6

47、O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O68（1）描述位置属性（相对位置）：分布方位、分布范围、伸展方向；（2）数量属性（面积、形状）：面积大小、形状、延伸方向态变化趋势。【例题 1】比较图 7 中 A、a所示的热带沙漠气候分布的异同点。【例题 2】（2009.浙江）读下图，完成下列问题。图示区域中，水土流失地区分布规律是什么？【例题3】（2010.安徽 34）地理环境是一个整体

48、，一个区域地表形态的变化往往受另一个区域物质运动的影响。描述图示期间该区域陆地变化特点。（6 分）文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O

49、6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:

50、CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V4B5T3 HM6K1M2E5A10 ZV5C10U6O9O6文档编码:CX6H4V