Once I first changed into co-director of an archaeological undertaking at Jebel Barkal in northern Sudan in 2018, I used to be amazed via the website online’s pyramids, temples and palaces. It have been an city heart within the historical empire of Kush, which ruled the Nile Valley on and off for over 2,000 years, from 2000 B.C.E. to 350 C.E.
Landscape of Jebel Barkal with royal pyramids at left.
Gregory Tucker
I used to be a long way from by myself in admiring the ruins – Eu and American vacationers have visited and archaeologists had documented the website online for the previous two centuries. Extra lately, Jebel Barkal was once identified as a UNESCO Global Heritage website online in 2003.
However researchers nonetheless know so little in regards to the historical town and its citizens, specifically in comparison with different historical towns of Egypt, Assyria, Greece and Rome. The place did nonroyal folks reside? What did they consume? We don’t even understand how they were given their water, for the reason that website online is ready a mile clear of the place the Nile flows these days. May there were a close-by channel of the Nile that has since crammed in? What was once this panorama like when Jebel Barkal was once a significant city heart? Extra extensively, how did adjustments in local weather during the last 4,000 years impact the expansion of town?
A few of these questions may also be studied via a box known as geomorphology, the find out about of ways the Earth’s floor adjustments, particularly via erosion. To be told extra about how the panorama round Jebel Barkal had modified over millennia, I invited two Dutch geomorphologists, Jan Peeters and Tim Winkels, who had up to now labored on Nile landscapes in Egypt, to return to Sudan to design a find out about.
The Nile as a supply of existence

The Nile runs via Sudan, previous the traditional town of Jebel Barkal after which via Egypt prior to attaining the Mediterranean Sea.
Peeters et al PNAS 2026, CC BY
The Nile floods on the finish of each and every summer season, as rains from the Indian Ocean monsoon fall at the highlands of East Africa. The traditional historian Herodotus famously known as Egypt “the gift of the Nile” as a result of in Egypt. the wealthy silt the floods deposited annually made for fertile fields. Egyptians retained the floodwaters in ponds and basins to make use of later for irrigation.
Upstream in Sudan, alternatively, the underlying geology and geomorphological surroundings is other. This stretch of the Nile is interrupted via bedrock outcrops that destroy the go with the flow of the river via what are known as cataracts: islands, rapids or even small waterfalls.
The Nile additionally cuts extra deeply into the bedrock and is extra confined to the riverbed in Sudan than in Egypt. The floodplains listed here are in most cases extra restricted. In consequence, it’s more difficult to carry onto water to make use of for irrigation after the once a year flood has handed.
Our workforce sought after to know how the traditional town interacted with the Nile and the way that courting advanced via time as local weather and the native atmosphere shifted. Our contemporary find out about, revealed within the Court cases of the Nationwide Academy of Sciences, checked out how the Nile channel and floodplain and Jebel Barkal developed over centuries.

The workforce extracted soil samples in a line that stretched throughout all sides of the Nile River and in any other line nearer to Jebel Barkal.
Peeters et al PNAS 2026; background WorldView-3 satellite tv for pc imagery © 2025 Maxar Applied sciences, CC BY
To be told in regards to the historical panorama, we accrued 26 sediment cores, averaging 26 toes (8 meters) intensive and three inches (8 centimeters) in diameter. Those cores are like time pills that maintain the stacked layers of sediment from Nile floods that amassed regularly over hundreds of years. Connecting the dots, 17 of our cores shaped a line around the Sudanese Nile valley. A 2d workforce of 9 cores centered at the space the place the traditional town advanced.
The paintings was once bodily difficult, due each to the unrelenting Saharan solar and the intensity of the sediments. In conjunction with a workforce of 5 native males, we spent weeks drilling the cores the use of hand augurs and a gas-powered drill.
The workforce works to drill and extract a core that may stretch from these days’s floor of the Earth down a median intensity of 26 toes (8 meters).
Pawel Wolf
Hatim Awad Abdullah was once this workforce’s full of life chief. He had his personal passion within the historical past of Nile flooding, partly as a result of his father and grandfather had advised him that the river used to flood other spaces than it has in newer instances. Our conversations with Hatim have been a part of a broader effort on our undertaking to interact contributors of the local people, and so they knowledgeable and enriched our figuring out of the panorama. Different initiatives in Sudan have taken equivalent steps towards group engagement.
Extracting data from the sediment layers
As soon as our workforce had extracted the lengthy sediment cores, we laid them out in sections so the geomorphologists may just file what was once in them at other ranges. Sediments on the most sensible of the cores are newer, the ones decrease down come from previous in time.
The cores have been got rid of in 3-foot (1-meter) segments that preserved the layers of sediment.
Pawel Wolf
Finer clays, silts and coarser sands would all had been deposited via other processes. Mild flooding from the Nile may have carried a few of these debris. Extra turbulent water draining from the barren region by the use of seasonal drainage channels known as wadis may have introduced others. Via running from the inner most, oldest portions of the core samples to the bottom floor, the geomorphologists may just reconstruct a chain of flooding and sediment deposition over hundreds of years.
Our subsequent step was once to take a look at to determine dates for when the sediments at other ranges have been deposited. One set of data got here from fragments of historical pottery present in one of the cores. Our workforce’s ceramic specialist, Saskia Büchner-Matthews, was once in a position to research those small items and may just frequently inform via their colour, texture and form after they have been made.
Any other line of proof trusted one way known as optically stimulated luminescence courting. Via measuring the power given off via minerals within the pattern, like quartz grains, this superb methodology establishes when a sediment was once final uncovered to mild. To ensure that optically stimulated luminescence courting to paintings, the samples want to be saved in the dead of night, so we needed to be cautious that our sediments have been accrued in black opaque tubes. Our workforce member Liz Chamberlain did this labor-intensive research in a specialised lab at Wageningen College in The Netherlands.
Our effects display, initially, that there have been an historical Nile channel with reference to Jebel Barkal, however extra like 10,000 years in the past – millennia prior to the folk of Kush constructed their town right here. By the point the website online was once first occupied round 2000 B.C.E., that channel had lengthy since crammed in. So we nonetheless don’t know evidently how the folk of Jebel Barkal were given their water, however it’s transparent that the Nile wasn’t operating proper subsequent to town.

This schematic reconstruction illustrates how the Nile channels and floodplain modified through the years to the current situation within the most sensible symbol.
Peeters et al PNAS 2026, CC BY
The knowledge additionally presentations that the floodplain started to increase from common Nile flooding beginning round 2000 B.C.E. This procedure persisted till the early twentieth century, when upstream dam development altered the Nile’s herbal flood regime. That mild accumulation of fertile soil within the floodplain, which the folk of Jebel Barkal used as agricultural fields, encompasses just about all of the historical historical past of town.
The cores our workforce drilled display that town grew right through a time of ample rains and productive, predictable Nile flooding that equipped fertile soil for agriculture. It doesn’t appear to be native local weather exchange is the rationale Jebel Barkal in the end went into decline.
Our clinical effects lend new weight to an inscription of the traditional Kushite king Taharqo, who dominated over each Nubia and Egypt from about 690-664 BCE. It data a gradual and specifically ample flood within the 6th 12 months of his reign.
“When the time for the emerging of the Inundation got here, it persisted emerging very much on a daily basis and it handed many days emerging on the price of 1 cubit on a daily basis.
“It penetrated the hills of South-land, it overtopped the mounds of North-land, and the land was once (once more) Primeval Waters, an inert (expanse), with out land being distinguishable from river. …
“Each and every guy of Nubia was once inundated with an abundance of the whole thing, Egypt was once in gorgeous pageant, and so they thanked the god Amun for His Majesty.”
This analysis has been specifically gratifying for me as it is helping construct a richer image of existence in historical Sudan, similar intensive and element to what we learn about different historical civilizations.