马拉河流域概览 Mara River Basin Overview

本部分提供了马拉河流域(Mara River Basin)的宏观背景信息。马拉河是东非最著名的跨国界河流之一,发源于肯尼亚的毛森林(Mau Escarpment),蜿蜒穿过马赛马拉国家保护区和坦桑尼亚的塞伦盖蒂国家公园,最终注入维多利亚湖。这里展示的核心指标帮助您快速建立对该流域物理规模和跨国重要性的认知。 This section provides the macro background of the Mara River Basin. One of East Africa's most famous transboundary rivers, it originates in Kenya's Mau Escarpment, winds through the Maasai Mara National Reserve and Tanzania's Serengeti National Park, and finally empties into Lake Victoria. These core metrics establish the physical scale and transboundary importance of the basin.

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主干流长度Main Stem Length

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公里 (km)Kilometers (km)

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总流域面积Total Catchment Area

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平方公里 (km²)Square Kilometers (km²)

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覆盖国家/区域Regions Covered

肯尼亚 & 坦桑尼亚Kenya & Tanzania

65% (KE) / 35% (TZ)

地理形态与海拔落差 Geography & Elevation Profile

马拉河流域的地理特征极为多样。上游被茂密的亚热带山地森林覆盖(海拔高达近3000米),这里是河流的“水塔”。中游流经广阔的稀树草原,这里是野生动物聚集的中心区域。下游则进入坦桑尼亚境内,穿越湿地和冲积平原,最终排入维多利亚湖。 The geographical features are extremely diverse. The upstream is covered by dense subtropical montane forests (up to 3,000m), serving as the "water tower". The midstream flows through vast savannas, the epicenter of wildlife concentration. The downstream enters Tanzania, traversing wetlands and alluvial plains.

  • 源头:Source: 肯尼亚的毛森林。Mau Forest, Kenya.
  • 终点:Mouth: 坦桑尼亚维多利亚湖。Lake Victoria, Tanzania.
  • 气候类型:Climate: 典型的双雨季气候,降水极不均匀。Typical bimodal rainfall, highly uneven spatial distribution.
🏔️ ➔ 🦓 ➔ 湖

高山森林至草原泊湖的垂直生态走廊 Vertical Ecological Corridor from Montane Forest to Savanna Lake

超过1800米的海拔落差造就了多样的微栖息地,并为河水冲刷泥沙提供了强大的动能。 An elevation drop of over 1,800m creates diverse micro-habitats and provides powerful kinetic energy for sediment transport.

沿程海拔高度剖面 (源头至入湖口) Elevation Profile (Source to River Mouth)