Mount Kenya

Mount Kenya is a very big mountain.

It is in Africa. It is the second highest mountain there.

A long time ago, it was a volcano.

Now, the volcano is quiet. The mountain has white ice on top.

The ice is melting fast.

It might all be gone by the year 2050.

Many plants grow on the mountain. Some plants only live there. Animals like the rock hyrax live there too.

The mountain helps give water to many people. It is a very special place.

Mount Kenya is a very large mountain in Africa.

It sits near the equator. It is the second highest mountain on the continent.

A long time ago, it was a volcano.

Now, the volcano is extinct, which means it is quiet. The mountain has several high peaks. The tallest is Batian. It is 5,199 meters tall.

There are small glaciers on the peaks. A glacier is a large mass of ice. The Lewis Glacier is the largest one.

These glaciers are melting very fast. They might be gone by the year 2050.

Many plants live on the mountain. Some plants only grow there. You can see giant lobelias in the high areas. The mountain also helps provide water to many people.

Local groups like the Kikuyu live nearby. They have lived there for many centuries. They believe the mountain is a holy place. To them, the white snow looks like a crown. They even build their houses to face the mountain.

Mount Kenya is a huge and famous landmark in Africa.

It sits about 150 km north-northeast of Nairobi. The mountain is also just 16.5 km south of the equator. It is the second highest mountain on the whole continent. The mountain is part of a large area with many counties. These include Meru, Embu, Kirinyaga, Nyeri, and Tharaka Nithi.

This mountain was once a very active volcano.

It formed about 3 million years after the East African Rift opened. Long ago, the volcano was likely much taller than it is now. It used to have a huge ice cap covering the top. This ice carved out the mountain over many thousands of years. Now, the ice has left behind deep valleys and eroded slopes.

Many people have explored this amazing place over the years. Joseph Thomson first described the mountain in 1883. He saw it from the Laikipia Plateau. Later, in 1893, an expedition reached the Lewis Glacier. This helped prove the volcano was extinct. In 1949, the government created the Mount Kenya National Park.

Later, in 1997, it became a UNESCO World Heritage Site.

There are many different parts to the mountain's landscape. The highest peaks are Batian, Nelion, and Point Lenana.

Batian is the tallest at 5,199 meters. There are also 11 small glaciers left on the peaks. The Lewis Glacier is the largest of these.

These glaciers are shrinking very fast right now. They might disappear completely by the year 2050.

Local people have deep connections to the mountain. The Kikuyu, Embu, Ameru, and Maasai all live nearby.

The Kikuyu believe the mountain is the throne of God. They call it Kirinyaga, which means "the one with the ostrich." This name comes from the white snow looking like an ostrich tail. Many plants also live here that you cannot find anywhere else.

You might even see a local rock hyrax there.

Mount Kenya is the second highest mountain in Africa.

It sits about 150 km north-northeast of Nairobi. The mountain is located just 16.5 km south of the equator. It sits at the intersection of several counties. These include Meru, Embu, Kirinyaga, Nyeri, and Tharaka Nithi. The area is protected as the Mount Kenya National Park.

This park was officially gazetted in 1949. It later became a UNESCO World Heritage Site in 1997. The site is famous for its natural beauty and ecological importance. It serves as a critical sanctuary for many endangered species. It also acts as a primary water tower for the region.

The mountain began as a stratovolcano. A stratovolcano is a type of volcano built by layers of ash and lava.

This volcano formed roughly 3 million years after the East African Rift opened. In the past, the mountain was likely much taller. Some experts believe it may have been higher than Mount Kilimanjaro. The volcano is now extinct. It has undergone two major periods of glaciation. This means it was covered by ice during two different times. Glaciers are large masses of moving ice. This ice carved the mountain into its current shape. The movement of prehistoric ice sheets created shallow, U-shaped valleys in the high moorland. In contrast, the lower slopes have deep, V-shaped valleys made by river erosion.

The central peaks of the mountain are volcanic plugs. A volcanic plug is the hardened remains of magma inside a vent.

These plugs have resisted erosion better than the surrounding rock. The highest peaks are Batian, which is 5,199 m, and Nelion, which is 5,188 m. These two peaks are separated by the Gate of the Mists gap. Point Lenana is the third highest peak at 4,985 m. Other notable peaks include Point Piggot and Point Dutton. There are also twin peaks to the north called Terere and Sendeyo. These form a large parasitic plug. The rocks here include basalts, phonolites, and trachytes. One specific rock type, kenyte, was named after the mountain in 1900.

Glaciers still exist on the mountain, but they are changing. There are currently 11 small glaciers remaining. The Lewis Glacier is the largest of these.

These glaciers are retreating very rapidly. Scientists predict they may disappear by the year 2050. This happens because more ice melts in summer than accumulates in winter. This retreat is caused by changes in temperature or precipitation trends. The total area of these glaciers was much larger in the 1980s. The loss of this ice is a significant environmental change.

Many different living things depend on Mount Kenya. The mountain has several distinct vegetation bands.

These zones change as you move from the base to the peak. The lower slopes are covered in various types of forest. The high moorland contains many endemic species. Endemic species are plants or animals found nowhere else on Earth. Examples include giant lobelias and senecios.

You can also find a local subspecies of rock hyrax.

The mountain is also a vital source of water. Runoff from the mountain provides water for over 2 million people.

Local ethnic groups have lived near the mountain for centuries. The Kikuyu, Embu, Ameru, and Maasai all have deep ties to the land. The Kikuyu live on the southern and western sides. They use the fertile volcanic soil for agriculture. They call the mountain Kirinyaga, meaning "the one with the ostrich." This refers to how the white snow looks like an ostrich tail. They believe the mountain is the throne of God, Ngai. The Embu people live to the southeast. They also view the mountain as a sacred home for God. The Ameru live on the east and north slopes. They also practice agriculture and keep livestock. The Maasai are semi-nomadic people. They graze cattle on the land to the north. They call the mountain Ol Donyo Keri, or "mountain of stripes."

History shows how humans have studied this landscape. Joseph Thomson first described the mountain scientifically in 1883. He saw it from the Laikipia Plateau. He identified it as an extinct volcano. Later, an expedition in 1893 reached the Lewis Glacier. This helped confirm the presence of ice. In 1966, Europeans performed the first thorough survey. Today, the Kenya Wildlife Service manages the national park. They work to protect the biodiversity of the area. They also manage the forest reserve. To protect crops, the government is building an electric fence. The Rhino Ark Trust has already built 250 km of this fence. This helps keep animals from straying into local farms.