Mount Kilimanjaro in the context of "List of peaks by prominence"

Montane grasslands and shrublands are a biome defined by the World Wide Fund for Nature. The term montane in the name of the biome refers to high elevation, rather than the ecological term that denotes the region below the treeline. The biome includes high-elevation (montane and alpine) grasslands and shrublands around the world, including the puna and páramo in South America, subalpine heath in New Guinea and East Africa, steppes of the Tibetan plateaus, and other similar subalpine habitats.Drier subtropical montane grasslands, savannas, and woodlands include the Ethiopian Highlands, the Zambezian montane grasslands and woodlands, and the montane habitats of southeastern Africa.

The páramos of the northern Andes are the most extensive examples of the habitat type. Although ecoregion biotas are most diverse in the Andes, these ecosystems are distinctive wherever they occur in the tropics. The heathlands and moorlands of East Africa (e.g., Mount Kilimanjaro, Mount Kenya, Rwenzori Mountains), Mount Kinabalu of Borneo, and the Central Range of New Guinea are all limited in extent, isolated, and support endemic plants and animals.The plants and animals of tropical montane páramos display striking adaptations to cool, wet conditions and intense sunlight. Around the world, characteristic plants of these habitats display features such as rosette structures, waxy surfaces, and abundant pilosity.

The Chagga States or Chagga Kingdoms also historically referred to as the Chaggaland (Uchaggani, in Swahili) were a pre-colonial series of Bantu sovereign states of the Chagga people on Mount Kilimanjaro in modern-day northern Kilimanjaro Region of Tanzania. The Chagga kingdoms existed as far back as the 17th century according to oral tradition, a lot of recorded history of the Chagga states was written with the arrival and colonial occupation of Europeans in the mid to late 19th century. On the mountain, many minor dialects of one language are divided into three main groupings that are defined geographically from west to east: West Kilimanjaro, East Kilimanjaro, and Rombo. One word they all have in common is Mangi, meaning king in Kichagga. The British called them chiefs as they were deemed subjects to the British crown, thereby rendered unequal. After the conquest, substantial social disruption, domination, and reorganization by the German and British colonial administrations, the Chagga states were officially abolished in 1963 by the Nyerere administration during its third year as the newly independent nation of Tanganyika.

Hans Heinrich Josef Meyer (22 March 1858 – 5 July 1929) was a German geographer from Hildburghausen, who was the son of publisher Herrmann Julius Meyer (1826–1909). Hans Meyer is credited with being the first European to reach the summit of Mount Kilimanjaro at 5,895 m (19,341 ft) in modern day Moshi District of Kilimanjaro Region in Tanzania. Kilimanjaro has three peaks: Shira, 3,962 m (12,999 ft); Mawenzi, 5,149 m (16,893 ft); and Kibo, whose summit was reached by Meyer in 1889.

Mount Kenya (Meru: Kĩrĩmaara, Kikuyu: Kĩrĩmanyaga, or "Kīrī-nyaga", Kamba: Ki nyaa, Embu: Kĩ nyaga) is the second-highest peak in Africa, after Kilimanjaro. The highest peaks of the mountain are Batian (5,199 metres (17,057 feet)), Nelion (5,188 m (17,021 ft)) and Point Lenana (4,985 m (16,355 ft)). Mount Kenya is located in the former Eastern and Central provinces of Kenya; its peak is now the intersection of Meru, Embu, Kirinyaga, Nyeri and Tharaka Nithi counties, about 16.5 kilometres (10.3 miles) south of the equator, around 150 km (90 mi) north-northeast of the capital Nairobi. Mount Kenya is the source of the name of the Republic of Kenya.

Mount Kenya is a volcano created approximately 3 million years after the opening of the East African Rift. Before glaciation, it was 7,000 m (23,000 ft) high. It was covered by an ice cap for thousands of years. This has resulted in very eroded slopes and numerous valleys radiating from the peak. There are currently 11 small glaciers, which are shrinking rapidly, and may disappear by 2050. The forested slopes are an important source of water for much of Kenya.

Nyiri Desert, also called The Nyika, Taru Desert, Taru desert, is a desert in southern Kenya. It is located east of Lake Magadi and between Amboseli, Tsavo West and Nairobi National Parks. A high proportion of Kajiado County's land area is covered by the Nyiri Desert. Its aridity is caused by the rain shadow of Mount Kilimanjaro.

The African humid period (AHP; also known by other names) was a climate period in Africa during the late Pleistocene and Holocene geologic epochs, when northern Africa was wetter than today. The covering of much of the Sahara desert by grasses, trees and lakes was caused by changes in the Earth's axial tilt, changes in vegetation and dust in the Sahara which strengthened the African monsoon, and increased greenhouse gases.During the preceding Last Glacial Maximum, the Sahara contained extensive dune fields and was mostly uninhabited. It was much larger than today, and its lakes and rivers such as Lake Victoria and the White Nile were either dry or at low levels. The humid period began about 14,600–14,500 years ago at the end of Heinrich event 1, simultaneously to the Bølling–Allerød warming. Rivers and lakes such as Lake Chad formed or expanded, glaciers grew on Mount Kilimanjaro and the Sahara retreated. Two major dry fluctuations occurred; during the Younger Dryas and the short 8.2 kiloyear event. The African humid period ended 6,000–5,000 years ago during the Piora Oscillation cold period. While some evidence points to an end 5,500 years ago, in the Sahel, Arabia and East Africa, the end of the period appears to have taken place in several steps, such as the 4.2-kiloyear event.

The AHP led to a widespread settlement of the Sahara and the Arabian Desert, and had a profound effect on African cultures, such as the birth of the Ancient Egyptian civilization. People in the Sahara lived as hunter-gatherers and domesticated cattle, goats and sheep. They left archaeological sites and artifacts such as one of the oldest ships in the world, and rock paintings such as those in the Cave of Swimmers and in the Acacus Mountains. Earlier humid periods in Africa were postulated after the discovery of these rock paintings in now-inhospitable parts of the Sahara. When the period ended, humans gradually abandoned the desert in favour of regions with more secure water supplies, such as the Nile Valley and Mesopotamia, where they gave rise to early complex societies.

Mount Damavand (Persian: دماوند [dæmɒːvænd] ) is a dormant stratovolcano and is the highest peak in Iran and Western Asia, the highest volcano in Asia, and the 3rd highest volcano in the Eastern Hemisphere (after Mount Kilimanjaro and Mount Elbrus), at an elevation of 5,609 metres (18,402 ft). Damāvand has a special place in Persian mythology and folklore. It is in the middle of the Alborz range, adjacent to Varārū, Sesang, Gol-e Zard, and Mīānrūd. It is near the southern coast of the Caspian Sea, in Amol County, Mazandaran Province, 66 km (41 mi) northeast of the city of Tehran.

Mount Damāvand is the 12th most prominent peak in the world and is part of the Volcanic Seven Summits mountaineering challenge.

The Explorer's Grand Slam, also known as the Adventurer's Grand Slam, is an adventurer goal to reach the North Pole and South Pole, as well as climb the Seven Summits: Everest, Aconcagua, Denali, Kilimanjaro, Elbrus, Vinson, and Puncak Jaya or Kosciuszko.

The Chaga or Chagga (Swahili: Wachagga) are a Bantu ethnic group from Kilimanjaro Region of Tanzania. They are the third-largest ethnic group in Tanzania. They founded the now former sovereign Chagga states on the slopes of Mount Kilimanjaro which governed the current Kilimanjaro region (eastern) of Tanzania.

The Chagga people are recognized as one of the economically successful groups in Tanzania. Their relative wealth is attributed to the fertile soil of volcanic Mount Kilimanjaro, which supports intensive agricultural activities. The Chagga have developed a strong work ethic and engaged in trade, contributing to their current economic standing in the country. They are known for historically employing various agricultural techniques, including sophisticated irrigation systems and terracing. Furthermore, they have intensive farming methods for centuries, a tradition that dates back to the time of the Bantu expansion within their historical states.