The two parts of Malaysia, separated from each other by the South China Sea, share a largely similar landscape in that both Peninsular and East Malaysia feature coastal plains rising to hills and mountains.[2] Peninsular Malaysia, containing 40 per cent of Malaysia's land area,[91] extends 740 km (460 mi) from north to south, and its maximum width is 322 km (200 mi).[94] It is divided between its east and west coasts by the Titiwangsa Mountains,[95] part of a series of mountain ranges running down the centre of the peninsula.[91] These mountains are heavily forested,[96] and mainly composed of granite and other igneous rocks. Much of it has been eroded, creating a karst landscape.[91] The range is the origin of some of Peninsular Malaysia's river systems.[96] The coastal plains surrounding the peninsula reach a maximum width of 50 kilometres (31 mi), and the peninsula's coastline is nearly 1,931 km (1,200 mi) long, although harbours are only available on the western side.[94]
A view from Low's peak, the highest peak of Mount Kinabalu
Around these two halves of Malaysia are numerous islands, the largest of which is Banggi.[99] The local climate is equatorial and characterised by the annual southwest (April to October) and northeast (October to February) monsoons.[94] The temperature is moderated by the presence of the surrounding oceans.[91] Humidity is usually high, and the average annual rainfall is 250 cm (98 in).[94] The climates of the Peninsula and the East differ, as the climate on the peninsula is directly affected by wind from the mainland, as opposed to the more maritime weather of the East. Local climates can be divided into three regions, highland, lowland, and coastal. Climate change is likely to affect sea levels and rainfall, increasing flood risks and leading to droughts.[91]
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