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The Hohokam Millennium • To 1450

Scottsdale Before 1450: Ten Thousand Years of People, and the Hohokam Who Taught the Desert to Drink

Long before a chaplain filed on 640 acres, this valley held the largest irrigation system in ancient North America — and the McDowells held villages, ballcourts and rock art that are still up there.

Scottsdale.tips Editors • 11 min read • September 28, 2026
Population
Tens of thousands, Valley-wide (est.)
Oldest trace
~8000 BC

Archaic rock shelters and base camps in the McDowells; the Brown's Ranch site may go back that far

Canals
500+ miles

Documented Hohokam canals in the Phoenix Basin; the biggest were wider than a road and up to 20 feet deep

Pinnacle Peak Village
AD 300–1150

100–200 pit houses and a ballcourt in north Scottsdale, found when a golf course was graded in 1987

Illustration of a Hohokam village in the Salt River Valley: a walled platform mound, an oval ballcourt, pit houses, agave and corn fields, and a canal in the foreground, with the McDowell Mountains behind
A Classic-period Hohokam village as the valley knew hundreds of them: canal, fields, pit houses, a ballcourt and a walled platform mound. Scottsdale's own sites were smaller — but one had a ballcourt. Illustration: Scottsdale.tips.

At a glance: Every acre of Scottsdale was somebody’s country for a hundred centuries before it was anybody’s real estate. Archaic hunters camped in the McDowells 8,000 years ago. From about the time of Christ to about 1450, the Hohokam turned the Salt River Valley into the most heavily irrigated place in ancient North America — and planted two ballcourt villages in what is now north Scottsdale. Then the water turned on them. This chapter is what the archaeologists actually know, stripped of the postcard version.

Before the farmers: 8,000 years of camps

The oldest evidence of people in the Preserve is almost 10,000 years old. Mammoth bones have come out of the Salt River gravels, and Clovis hunters were in the Southwest by roughly 9500 BC — but no Paleo-Indian site has ever been found in Scottsdale. The whole record of that era here is one spear point, refashioned from a fluted Clovis-style blade, picked up at a much later Hohokam site during the DC Ranch surveys in 1995.

The Archaic people who followed left more. From about 8000 BC to the first century AD, small bands worked the McDowells seasonally: spear points in rock shelters in north Scottsdale, chipping stations on the south and west slopes, “several Archaic work areas and houses in pits” on the west side of the range, and dozens of bedrock mortars — bowls ground into granite by centuries of mesquite pods and seeds. The Brown’s Ranch rock shelter, a few minutes’ walk from today’s trailhead of the same name, was used from the Archaic straight through the Hohokam and Yavapai periods; test excavations found deep, intact deposits, some possibly as old as 8000 BC.

Around 1500 BC, corn, beans, squash and cotton arrived from Mexico, and some of these people began floodwater farming along the Salt and Gila. That is the hinge of the whole story: the desert was about to become a farm.

The Hohokam: a thousand years of canals

The people archaeologists call the Hohokam (an O’odham word usually rendered “those who are gone”) emerge in the Salt and Gila valleys around AD 1 — or AD 450, depending on how you count the early phases — and are the dominant fact of the region until about 1450. What made them different from every other desert people was engineering.

Working with digging sticks and baskets, they built more than 500 miles of documented canals in the Phoenix Basin, with individual main canals running 16 to 20 miles and serving on the order of 100,000 acres. The biggest trunk lines were more than 50 feet across and up to 20 feet deep; measured gradients ran from 1.2 to 4.8 feet per mile, which is exactly the range a modern engineer wants to keep water moving without scouring the banks. At Pueblo Grande, the headgate village on the north bank near today’s Sky Harbor, as many as ten main canals were in use at once. The American Society of Civil Engineers lists the system as a National Historic Civil Engineering Landmark.

A preserved prehistoric Hohokam canal channel at the Park of the Canals in Mesa, Arizona, a broad shallow earthen trench between desert trees
A surviving Hohokam channel at Mesa’s Park of the Canals, listed on the National Register in 1975. The trunk canals were far bigger than this lateral. Photo: Tony the Marine, CC BY-SA 3.0, via Wikimedia Commons.

Scottsdale had its own, smaller share. Omar Turney’s 1929 map of the prehistoric network shows a cluster of canals that started at the Salt River to the east and ran west across what is now the Salt River Pima-Maricopa Indian Community into the southern end of the city — what archaeologists now call the “Scottsdale Canal system.” Classic-period farmsteads along the southern foot of the McDowells were tied to it by their pottery. And when the Phoenix pioneers cleaned out an ancient ditch in 1868, the Arizona Miner reported land that “looks as if recently cultivated,” with volunteer cotton, tobacco and castor beans still sprouting in Hohokam fields four centuries after the farmers left.

Upland Scottsdale: agave, rock piles and two ballcourt villages

The north of the city was Hohokam country of a different kind. With no river to tap, the upland villages farmed the bajada with rock-pile fields — thousands of low cairns that trapped moisture for agave and cholla — and roasted the agave hearts in pits that still show up as ashy rings near the CAP canal and at Brown’s Ranch. Agave murpheyi, the “Hohokam agave” they domesticated, still grows wild in the McDowells.

The prize find is Pinnacle Peak Village. In late 1987, graders cutting the Troon Village golf course southeast of Pinnacle Peak turned up pottery, and the landowners, Jerry and Florence Nelson, stopped the machines. Over the winter of 1988 Dr. Patricia Gilman of Arizona State University and more than sixty Arizona Archaeological Society volunteers excavated a village of 100 to 200 pit houses with its own ballcourt, some thirty trash mounds and fifteen cremation pits. Out of the ground came 26 intact vessels, a copper bell with its clapper still inside — cast in central Mexico — 51 pieces of turquoise in a single cremation, amethyst from a Four Peaks mine 29 air miles away, corn cobs, and 1,794 animal bones, 82 percent of them rabbit. People lived here from about AD 300, peaking between 500 and 1150, twenty miles from the Salt and ten from the Verde, on nothing but springs and wash runoff. Three acres were set aside as open space, and the site went to the Archaeological Conservancy in 1991.

A second large ballcourt village, recorded only by its site number, stands in the northern McDowells. Both are “unique for their large size, ballcourt, and upland setting with limited water resources,” in the words of the Preserve’s cultural plan — and both emptied when the regional ballcourt network collapsed around AD 1070, four hundred years before the Hohokam world as a whole came apart.

The excavated adobe and stone walls of the Hohokam platform mound at Pueblo Grande in Phoenix, a raised earthen platform with a masonry retaining wall
The platform mound at Pueblo Grande (now the S’edav Va’aki Museum), the headgate town of the north-side canals. No platform mound has ever been found in Scottsdale. Photo: Visitor7, CC BY-SA 3.0, via Wikimedia Commons.

Then there is the rock art. Two major concentrations of petroglyphs sit along washes and springs on the east and west sides of the McDowells. The state site files list only four petroglyph sites in the Preserve, but a 2007 volunteer inventory counted up to 333 unrecorded panels in one mountainous section alone. The Empie site near Scottsdale Road and Carefree, on the National Register, carries markings that line up with the summer and winter solstices. All told, the Preserve holds 76 recorded sites — 52 of them prehistoric — across 30,000 acres of which only about three-quarters have been surveyed.

The collapse

After 1150 the Hohokam built differently: walled compounds, platform mounds, fewer and larger towns. Then the river turned. Canal sediments record three destructive floods between 1000 and 1400 in the north-side trunk canals; after one around 1300, the biggest of them was abandoned and never replaced. Each wrecked headgate meant a year or two with no water, and a farming society cannot skip two harvests forever. Between the early 1300s and the mid-1400s the population fell by more than 75 percent. By about 1375 most of the villages and canals on the lower Salt were empty; 1450 is simply the conventional end date. Drought, salt-crusted fields, disease and political breakdown have all been argued, and the current model is a long unraveling rather than a single catastrophe.

The descendants stayed. The Akimel O’odham and Piipaash who greeted the Spanish on the Gila two centuries later called the vanished builders Huhugam, and O’odham tradition remembers the Salt River villages emptying north and south while the Gila families intermarried with newcomers and became the modern Pima. What happened next — the Yavapai in the McDowells, the Spanish who never quite got here, the soldiers who did — is the next chapter.

Why the Hohokam still matter in Scottsdale today

  • The valley was pre-graded. Nineteenth-century canal builders in Phoenix cleaned out Hohokam alignments; the modern SRP system still follows some of them. The Arizona Canal that made Scottsdale possible was the first to break that pattern and cut virgin ground.
  • The Preserve is an archaeological district as much as a park. Rock shelters, mortars, agave fields and hundreds of petroglyph panels are the reason the Preserve’s trail plans route around certain washes.
  • The name on the map. The O’odham and Piipaash of the Salt River community along Scottsdale’s eastern edge are the living continuation of this chapter.
  • The lesson. A society that engineered its way to abundance in this valley was undone by water it could not control — a theme the city has been rehearsing since the 1891 flood and is still rehearsing on the Colorado River.

Frequently asked questions about Scottsdale before 1450

Who lived in Scottsdale before the Hohokam?

Archaic hunter-gatherers, for roughly 8,000 years. The city's archaeological survey found their spear points in north Scottsdale rock shelters, work areas and pit houses on the west side of the McDowells, and dozens of bedrock mortars. The Brown's Ranch rock shelter in the Preserve was used from Archaic times right through the Hohokam and Yavapai periods, with deposits that may date to 8000 BC. Before that, Clovis hunters roamed the Southwest around 9500 BC; Scottsdale's only trace of them is a single reworked fluted point found at a later site in DC Ranch.

Were there Hohokam canals in Scottsdale?

Yes, in the far south. Omar Turney's 1929 map of the prehistoric canals shows a group of ditches that left the Salt River near today's Salt River Pima-Maricopa Indian Community and ran west across what is now southern Scottsdale — archaeologists call it the 'Scottsdale Canal system.' The famous big canals (Canal System 2, headed at Pueblo Grande) ran through Phoenix to the west. The 1885 Arizona Canal was dug on a new, higher alignment; it did not reuse a Hohokam ditch, though Jack Swilling's 1868 Phoenix ditch did.

What is Pinnacle Peak Village?

A Hohokam village of 100 to 200 pit houses, about 1.5 miles southeast of Pinnacle Peak, exposed in late 1987 when grading for Troon Village turned up pottery. Landowners Jerry and Florence Nelson stopped the work, and in early 1988 Dr. Patricia Gilman led an ASU dig with more than sixty volunteers. It was occupied from about AD 300 to 1150, had its own ballcourt, and held a copper bell from central Mexico, 51 pieces of turquoise in one cremation, amethyst from Four Peaks and thousands of rabbit bones. Three acres were preserved as open space and the site was given to the Archaeological Conservancy in 1991.

Why did the Hohokam disappear around 1450?

They didn't vanish so much as disperse. Tree-ring and canal studies show unusually large floods hitting the Salt River systems repeatedly after about 1300, wrecking headworks that took a year or two to rebuild; the population fell by more than 75 percent between the early 1300s and the mid-1400s. Drought, salted fields, disease and political breakdown all get argued. The O'odham (Pima) and Piipaash (Maricopa) peoples are their descendants, and O'odham tradition says the Salt River villages west of Pueblo Grande emptied toward the north and south while families in the Gila country stayed and became the modern Pima.

Can you still see Hohokam sites in Scottsdale?

Rock art, mostly. The McDowell Sonoran Preserve has 76 recorded archaeological sites, 52 of them prehistoric, including eleven rock shelters and four registered petroglyph sites — and a 2007 volunteer survey counted up to 333 more unrecorded petroglyph panels. Their locations are kept confidential by the city to protect them, so the honest answer is that you will not be directed to them; our note on Preserve rock art explains why, and where to see petroglyphs legally. The excavated villages are backfilled and unmarked. For a platform mound and an excavated canal, the S'edav Va'aki Museum (formerly Pueblo Grande) in Phoenix and Mesa's Park of the Canals are twenty minutes away.

Who shaped Scottsdale before 1450

The people whose Scottsdale years run through this chapter — each with a full profile in the people who made Scottsdale.