The wellspring in Mecca is believed to have been flowing for more than 4,000 years and continues to nourish pilgrims to this day.
The Hajj pilgrimage began on Wednesday. Some 1.8 million Muslims from across the globe are expected to gather in the Saudi holy city of Mecca for the annual gathering that will conclude on June 8.
Hajj is a once-in-a-lifetime obligation for all adult Muslims who are physically and financially able to make the journey.
Throughout the sacred pilgrimage, pilgrims drink from Zamzam, a wellspring believed to have been flowing for more than 4,000 years, nourishing them to this day.
But where does this water come from, and why does it hold such deep significance?
Zamzam water comes from a well, located within the Grand Mosque of Mecca (Masjid al-Haram), some 21 metres (69 feet) east of the Kaaba.
The Zamzam well is beneath the Mataf area, which is the white marble-tiled space surrounding the Kaaba where pilgrims perform Tawaf.
In 1962, King Saud commissioned the expansion of the Mataf area to better accommodate the growing number of pilgrims. As part of this project, the opening of the Zamzam well was lowered and enclosed in a basement approximately 2.7 metres (9 feet) deep beneath the Mataf.
Zamzam water is deeply connected to the origins of Mecca and the story of Prophet Abraham (Ibrahim), his wife Hagar (Hajar), and their son Ishmael (Ismail).
According to Islamic tradition, Prophet Abraham left Hagar and baby Ishmael in the desert valley of Mecca by God’s command as a test of faith.
When their provisions ran out, Hagar ran back and forth seven times between the two small hills of Safa and Marwa searching for water.
God responded to her faith and struggle with a miracle: water began to gush from the ground near baby Ishmael’s feet – this became the Zamzam well.
This spring saved their lives and led to the settlement of Mecca, which today has a population of about 2.2 million.
Where is the Zamzam well located?
During Hajj and Umrah, pilgrims re-enact Hagar’s search for water by walking seven times between the hills of Safa and Marwa in the ritual of Sa’i and drink Zamzam water following the tradition of the Prophet Muhammad, who praised its purity and healing qualities.
According to Islamic tradition, when the Zamzam spring miraculously gushed forth near baby Ishmael’s feet, Hagar tried to contain the water, fearing it would run out.
The Zamzam well is about 31 metres (101 feet) deep and was originally hand-dug. Water enters the well through loose sand and gravel in the top part, and also from cracks in the solid rock below.
Today, electric pumps bring the water up instead of the old rope-and-bucket method. The well itself is now closed to the public, but the water is available through fountains and dispensers around the Grand Mosque.
The Zamzam well is considered to have flowed uninterrupted for more than 4,000 years. The continuous flow of water and its central role in Hajj and Umrah have been well-documented for centuries.
According to the General Authority for the Care & Management of the Grand Mosque and the Prophet’s Mosque, extraction and consumption of Zamzam vary by season:
According to the Saudi visa office, ​​Mecca is expecting to welcome 15 million Umrah pilgrims in 2025.
To manage this demand, the Zamzam well is monitored in real time using digital sensors that track water level, pH (potential of hydrogen; a measure of the acidity or alkalinity of a liquid), temperature, and conductivity. Additional monitoring wells across Wadi Ibrahim help assess how the entire aquifer responds to water use and rainfall.
The Zamzam Studies and Research Centre (ZSRC) estimates how much water can be safely extracted and advises the Grand Mosque authority on sustainable pumping levels. Each year, the Saudi Geological Survey (SGS) issues a pumping schedule, with peak demand during Ramadan and Dhul-Hijjah and the lowest in Muharram.
If water levels fall below a set threshold, pumping is paused to allow the well to recover, ensuring a stable, long-term supply.
Zamzam water is clear and odourless, but it has a distinct taste due to its rich mineral content. It is slightly alkaline, with a pH between 7.9 and 8.0, higher than regular drinking water.
