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1、地理答题模式（自理）一、人口迁移对环境的影响：(一分为二)对迁出地利：缓解当地人口矛盾弊：劳动力、人才大量流失对迁入地利：劳动力、人才大量的涌入、促进当地经济发弊：加剧当地生态问题和社会问题二、旅游活动中的环境问题：1、环境污染2、对动植物资源的破坏3、对背景环境的破坏4、对文物古迹的破坏5、对正常社会秩序的冲击三、旅游资源开发条件的评价：1、游览价值（eg：旅游资源丰富、独特性、集群性）2、市场距离（旅游地和经济发达地区的距离）3、交通位置及其通达性（eg：交通位置、地理位置优越，交通便利）4、地区接待能力（强、弱）5、旅游的环境承载量（大、小）6、政府的支持和宣传四、地质灾害多发的原因：1
2、、处于、板块和、板块交界处（或者是出于板块交界处），地壳活动频繁2、地表物质破碎3、山体坡度大4、气候区域、降水集中多暴雨5、人为破坏植被五、全球性环境问题：1、二氧化碳增多2、酸雨增多3、雨林破坏严重，影响全球气候和二氧化碳的含量4、生物多样性六、影响太阳辐射强度的因素(即影响大气对太阳辐射削弱作用的因素)：1太阳高度(即纬度)；2天气状况；3地势；4空气密度。七、影响气温高低的因素：1纬度；2地形、地势；3下垫面性质(海陆位置、植被状况、洋流等)；4天气状况。八、河流的治理措施：上游：治理原则是调洪，做法是修水库、植树造林；中游：治理原则是分洪、蓄洪，做法是修水库，修建分洪、蓄洪工程；下游
3、：治理原则是泄洪、束水，做法是加固大堤，清淤疏浚河道，开挖河道。九、河流洪涝灾害的成因分析（一分为二）：自然原因(主要从三个方面考虑：水系特征、水文特征、气候特征)人为原因(主要从三个方面考虑：植被破坏、围湖造田、占用破坏河道)。十、分析河流水能丰富的原因：从两个方面：一是流速(位于地势阶梯过渡地带，河流落差大)；二是径流量大(看降水量的多少、流域面积的大小、蒸发量的大小)。十一、描述河流的水系特征：1.长度2.流向3.流域面积大小4.落差大小(水能)5.河道曲直情况6.支流多少7.河流支流排列形状(扇形,树枝状)十二、描述河流的水文特征：（二量二期一能）1、流量:大小,季节变化,有无断流(取
4、决于降水特征,雨水补给,河流面积大小)2、含沙量:取决于流域的植被状况3、结冰期:有无,长短4、水位:高低,变化特征(取决于河流补给类型,水利工程,湖泊调蓄作用)5、水能:与地形(河流落差大小,流速快慢),气候(降水量的多少,径流量的大小,蒸发量的大小)有关文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编
5、码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O
6、5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C
7、10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2
8、K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U
9、7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY
10、1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D
11、3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7十三、影响降水的因素：1、气候:大气环流(气压带,风带,季风)2、地形:迎风坡,背风坡3、地势(海拔高度):降水在一定高度达最大值4、海陆位置(距海远近)5、洋流(暖流:增温增湿;寒流:降温减湿)十四、渔场形成的区位条件：（具体问题具体分析）1.地形:面积广阔的大陆架(阳光直射,光合作用强,饵料丰富)2.温带海域:气温变化大,海水上泛3.河口处:河流带来丰富的营养盐类4.洋流:(交汇流或上升流)海水上泛,带来海底营养盐类,饵料丰富十五、评价河流的航运价值：自然因素：1.地形:平坦,流经平原,水流平缓2.气
12、候:降水丰富均匀,河流流量大,季节变化小,冰期短3.河道:宽阔平直,水深社会经济因素：流域内人口多,经济发达,联系密集,运输量大。十六、世界主要气候类型及分布：（详见“气候类型分布图与自然带分布模式图相结合记忆自然带分布图”）十七、农业区位因素：（一分为二）自然+社会1、自然条件（气候、地形、土壤、水源）2、社会经济条件（市场、交通运输、技术、政府政策）Ps：从光照、热量、降水、地形、水源、土壤、市场、技术等各个方面进行综合分析，找出最突出的优势因素和限制性因素，然后从中找出主导因素。十八、工业区位因素分析:(一分为二)自然+社会1.地理位置 2.资源因素 3.农业因素 4.交通因素5.市场因
13、素 6.科技因素 7.劳动力因素 8.历史因素十九、主要农业地域类型：水稻种植业、混合农业、商品谷物农业、大牧场放牧业、乳畜业、热带种植园经Ps：具体资料请自己去查阅文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV
14、1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A
15、3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 H
16、F2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T1
17、0U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7
18、ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y
19、7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7附
20、录：（1）判断等温线走向及原因1、与纬线平行：受纬度或太阳辐射影响2、与海岸线平行：受海陆位置影响3、陆地小范围弯曲：地形（山谷/山脉）4、海洋里小范围弯曲：寒/暖流（2）凌汛的因素（初冬、初春）1、河流有结冰期2、从低纬流向高纬3、河道弯曲（3）沼泽形成的原因1、纬度位置高（海拔高），气温低，蒸发量小2、地势低平，排水不畅3、下层有冻土，阻碍水流下渗（4）区域地理（综合分析法）导与练P15 文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10
21、HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T
22、10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7
23、 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6
24、Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7
25、文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:C
26、V1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7文档编码:CV1O5W4A3C10 HF2K6T10U7T7 ZY1C6Y7D3S7