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Santa Clarita is a city of about 229,000 people in northern Los Angeles County, strung along the Santa Clara River between the San Gabriel, Santa Susana and Sierra Pelona mountains. Its pavement is a heat-and-sun problem more than a frost problem: the nearest long-record weather station averages about 87 days a year at or above 90 degrees, and nearly all of the 16-plus inches of annual rain arrives in a few winter months.
Santa Clarita Paving is a paving contractor serving residential and commercial properties throughout Santa Clarita and surrounding communities in Southern California.
PremierPath Paving & Landscaping is a Santa Clarita, California contractor that handles both the hardscape and the green side of outdoor property improvement.
Weather, soils and pavement in Santa Clarita, California
Climate and freeze-thaw
There is essentially no freeze-thaw cycle here, so the usual northern explanation for potholes does not apply. What the climate does is bake the surface for months and then soak it in a short wet season. Long, hot, dry summers age the asphalt binder and open fine cracks; December through March then delivers most of the year's rain, often in heavy bursts, and that water reaches any base the cracks have exposed. Summer is also the only practical window for most sealing and striping work.
Annual precipitation
16.76 inches
Rain falling December through February
11.26 of 16.76 inches, about two-thirds (derived from the published monthly and annual normals)
Rain from June through September
Roughly 0.13 inch in total (derived: June 0.02, July and August 0.00, September 0.11)
Days with 1 inch or more of rain
About 4.9 a year, with the most in January and February
Days at or above 90°F
About 87 a year
Days at or above 100°F
About 20 a year
Typical July
High 94°F, low 63°F
Typical January
High 63°F, low 47°F
Days with a low at or below 32°F
About 1 a year
NOAA 1991-2020 climate normals for the Newhall 5NW cooperative station, roughly 3 miles from the center of Santa Clarita by the station's published coordinates. Conditions vary across a city that spans more than 70 square miles and several hundred feet of elevation, so treat these as a close local benchmark rather than a measurement taken at a particular lot.
Under the pavement
Soils and base conditions
Santa Clarita sits on the floor and margins of a structural valley that has been filling with sediment for millions of years. Recent sand, gravel and cobble alluvium lies along the Santa Clara River and its tributary canyons, and most of the surrounding hills are the Pliocene-Pleistocene Saugus Formation, a loosely consolidated sandstone and conglomerate with clay and clayey lenses. The practical result is that conditions change quickly from the river bottom to the hillsides, and the hillside ground is the part that moves.
Canyon floors and the river bottom are covered by Recent stream alluvium. Hydrogeologic descriptions of the region call that alluvium unconsolidated and range it from fine to very coarse material. Where it is sandy and gravelly it drains freely and makes a stable pavement subgrade; where it is silty or clayey it does not.
Away from the river, much of the hill ground is the Saugus Formation, described in regional geology reports as a loosely consolidated sandstone and conglomerate that contains layers and lenses of clay. Where a lot is cut into or built up on this ground, the clay lenses are what change moisture and volume with the seasons.
Expansive clay is documented in the older Mint Canyon Formation around Vasquez Canyon, where interbedded silts, sandstones and clay beds dip downslope and the area is landslide-prone; Plum Canyon sits inside a mapped landslide complex. Shrink-swell clay lifts and drops pavement unevenly, and light-loaded roads and lots are more easily deformed by it than buildings are.
Fill slopes and cut-fill transitions are where heave, settlement and edge cracking concentrate in this terrain, as pavement on one side of a line sits on compacted fill and on the other on native ground. If a lot cracks in a straight line that follows a grade change, ask about the original grading before assuming the asphalt is at fault.
Parcel-level soil information is free. The USDA Web Soil Survey shows the mapped soil unit, drainage class and depth to the water table for any Santa Clarita address, and a geotechnical report is the way to settle a large, hillside or repeatedly failing site.
What fails here
Common pavement problems in Santa Clarita
Sun and heat aging: oxidation, raveling and fine cracking
Gray, dry-looking asphalt that has lost its black color, loose stone at the surface, and a web of fine cracks, most visible on lots and cul-de-sacs that get full sun all day.
Likely causes
Years of sun and heat oxidizing the asphalt binder until it is stiff and brittle
Wear from turning traffic that strips the weakened surface, especially on parking-stall edges and drive-aisle turns
Water entering the fine cracks during the winter rains and weakening the layers below
When to get it looked at: Preservation treatments pay off while the base is still sound. The city itself treats slurry seal as maintenance and overlay as the rehabilitation that follows when damage is extensive; a lot that is already cracked in a connected pattern has moved past what a seal coat can fix.
Interconnected chicken-wire cracking in the wheel paths, then broken pieces that come out and leave potholes after a stretch of heavy rain.
Likely causes
Repeated truck, bus and trash-truck loading on pavement that is thinner than the traffic requires
A base that has lost support after a wet season, because the surface cracks let rain reach it
Heavy bursts of rain on a surface that has been dry for months, which is when water finds every opening
When to get it looked at: Fatigue cracking starts at the bottom of the asphalt layer and works upward, so by the time it shows at the surface the damage is structural. Patching the surface of an alligator-cracked area usually fails; the repair is removal and rebuilding of the section, with the cause of the water entry fixed.
Clay and slope movement on hillside and canyon-mouth sites
Ridging, dips and long cracks that follow a slope or a grade change, and roads that stay bumpy no matter how often they are patched.
Likely causes
Shrink-swell clay in the Saugus and Mint Canyon formations changing volume through the wet and dry seasons
Cut-and-fill boundaries that settle or creep at different rates
Irrigation or roof drainage feeding water into clay under a lot's edge
When to get it looked at: If the same dip or crack comes back after patching, or the lot sits on or below a slope, a geotechnical opinion is cheaper than a second repair. Moving ground does not hold a surface patch.
Runoff, scour and drainage on river-adjacent and canyon sites
Washed-out edges, sediment on the lot after storms, and standing water in low corners of lots near the river or at the mouth of a canyon.
Likely causes
The Santa Clara River and its tributary creeks, which are dry most of the year and run hard in heavy rain
Inlets, swales and culverts that fill with sediment between storms
Pavement edges with no curb or with a drop-off where flow concentrates
When to get it looked at: Clear and inspect drainage before the first winter storm. A lot that floods repeatedly, or an edge being undercut, calls for a grading and drainage review before any more asphalt goes down.
By April the rainy season is largely over (April averages under an inch). Spring is the time to find out what the winter did: map the potholes and the new cracking, and book the repairs for the dry months.
Summer
The working season for sealing, slurry, striping and overlays. July and August average a high of 94 to 96 degrees and effectively no rain, which suits curing, but fresh pavement stays soft and tracks in the afternoon heat, so schedule heavy truck traffic around it. The city runs its own Road Rehab slurry seal work through the summer.
Fall
September through November is still dry (about 1.45 inches across the three months), and October into November is the last comfortable window to seal cracks and clear drainage before December's rain begins.
Winter
December through February brings about 11 of the year's 17 inches, often in heavy bursts that run to an inch or more on a few days a year. Expect potholes where cracks were left open, and cold-patch what is unsafe; permanent repairs generally need dry weather.
Santa Clarita incorporated in 1987 from four unincorporated communities, Valencia, Newhall, Saugus and Canyon Country, and is now the third-largest city in Los Angeles County. A large share of its commercial pavement comes from Valencia, a master-planned community begun by the Newhall Land and Farming Company in the 1960s.
Interstate 5 forms the city's western edge and State Route 14 part of its eastern edge; the two meet at Newhall Pass, and State Route 126 meets I-5 at the city's lowest point. Most contractor trips start from one of these corridors.
Valencia's main routes are McBean Parkway (north-south) and Valencia Boulevard, Magic Mountain Parkway, Newhall Ranch Road and Lyons Avenue (east-west). The neighborhood has most of the city's government buildings, hotels, car dealerships, medical centers and corporate headquarters, as well as office parks and industrial warehouses.
Large anchor lots include Westfield Valencia Town Center (over 1,000,000 square feet of retail), Henry Mayo Newhall Memorial Hospital (a 357-bed trauma center on McBean Parkway), College of the Canyons and CalArts. Six Flags Magic Mountain is west of I-5, outside the city limits, though it is often assumed to be in Valencia.
Saugus is organized around Bouquet Canyon Road, which runs northeast to southwest to Magic Mountain Parkway, with Soledad Canyon Road, Newhall Ranch Road, Copper Hill Drive and Golden Valley Road as other thoroughfares. Soledad Canyon Road also runs through Canyon Country, along with Sierra Highway, which divides the community's two ZIP codes.
Old Town Newhall has older, tighter lots than the master-planned parts of the city; Canyon Country, the largest area east of Golden Valley Road, mixes neighborhood tracts with the growing Vista Canyon area.
The city runs a yearly Road Rehab program of slurry seal (maintenance) and overlay (grind and replace). Its 2022 release described a data-driven selection using traffic volume and Pavement Condition Index, 76 lane miles (nearly 6.8 million square feet) rehabilitated in 2021, and an overall city PCI of 71. Residential slurry days mean no driveway access and posted no-parking zones, with parking available within about 1,000 feet. The 2026 street list is posted on the city's Road Rehab page.
Before you bid
Permits, drainage and winter maintenance
California regulates stormwater at three levels: the state Construction General Permit during work, the Los Angeles County municipal permit that the city implements after work, and the city's own code. Routine resurfacing is treated differently from new or expanded pavement. None of this is legal advice; confirm with the City before a project is bid.
The state's Construction General Permit (Order 2022-0057-DWQ, effective September 1, 2023) generally covers projects that disturb one acre or more of soil, or less than one acre if part of a larger common plan of development. Coverage requires registering with the State Water Board and following a stormwater pollution prevention plan.
Santa Clarita's post-construction stormwater rules are in Chapter 17.95 of its Unified Development Code, which implements the Los Angeles Regional Water Board's municipal stormwater permit. The chapter's priority projects include parking lots with 5,000 square feet or more of impervious surface or 25 or more spaces, and street and road construction of 10,000 square feet or more.
The same chapter treats a rebuild as redevelopment when it adds or replaces 5,000 square feet or more of impervious surface on a developed site, or reworks more than half of an existing development's paved area. Routine maintenance, including repaving an existing road on its current alignment, falls outside that definition.
A qualifying project must prepare a low-impact-development plan under the County's LID Standards Manual, which generally means retaining or treating runoff on site. Whether a parking lot rebuild crosses the line depends on how much pavement is replaced rather than resurfaced, so ask the City's Planning and Engineering staff for a determination before design.
Work in or near the Santa Clara River, its tributary creeks or a mapped significant ecological area is subject to additional state and federal review. Check before disturbing any lot that drains directly to those waters.
Local answers
Santa Clarita pavement questions
Why do Santa Clarita parking lots crack when there is no freeze?
Mostly heat, age and water rather than ice. Years of sun and 90- to 100-degree days oxidize the asphalt binder until the surface is stiff and brittle, and the winter rains then enter the cracks and soften the base. Add clay-rich ground in some hillside areas that shrinks and swells, and fatigue cracking in the wheel paths from heavy trucks, and a lot can crack well before it wears out.
How hot and dry is Santa Clarita for pavement purposes?
NOAA's 1991-2020 normals for the Newhall 5NW station, about 3 miles from the city center, show roughly 87 days a year at or above 90 degrees and about 20 at or above 100. Almost no rain falls from June through September, and December through February brings about two-thirds of the 16.76-inch annual total. The two-thirds figure is our own division of published normals.
Does Santa Clarita have expansive clay?
It does in places. Local geology descriptions document expansive clay in the Mint Canyon Formation around Vasquez Canyon and a landslide complex at Plum Canyon, and the Saugus Formation that underlies much of the valley contains clay lenses. Alluvium along the river is generally sand and gravel and behaves very differently. The Web Soil Survey and a geotechnical report are how a specific lot is checked.
Does resurfacing a parking lot in Santa Clarita trigger stormwater requirements?
Not usually for routine maintenance. The City's Chapter 17.95 treats redevelopment as creating, adding or replacing 5,000 square feet or more of impervious surface, and does not count routine maintenance or repaving an existing road on its current alignment. Rebuilding most of a lot, changing its footprint or adding pavement can bring in the low-impact-development rules, and a project that disturbs an acre or more needs state construction stormwater coverage. Confirm with the City first.
How does the City of Santa Clarita decide which streets to resurface?
Its annual Road Rehab program uses traffic volume and the Pavement Condition Index, which scores cracking, potholes and other distress. Streets in the same area are grouped so they can be treated together, and the treatment is slurry seal for maintenance or overlay for rehabilitation. The current year's street list is on the City's Road Rehab page.
Sources and how this page was prepared
Last reviewed October 16, 2026. This is general information about Santa Clarita compiled from the public sources below, not engineering advice or a finding about any particular property. Soil, drainage and permit requirements vary parcel by parcel and by project, so confirm them with the town, the state agency and a qualified professional before work is scoped.
Geology of the Santa Clarita Valley: Saugus — Saugus, Mint Canyon and Castaic formations; expansive clay and landslides at Vasquez Canyon and Plum Canyon; uncontrolled creeks
Much of California has long, hot, dry summers and mild, wet winters. In summer, the sun dries out and ages asphalt. In winter, the rain arrives all at once and tests drainage. Inland and valley areas get the most heat and sun, while the coast stays milder but damper. So two things matter most here: sealcoating for sun protection, and good drainage for the wet season.
Summer UV oxidation and heat
Months of strong, dry sun bake the binder out of asphalt, graying and embrittling the surface — especially in inland and Central Valley heat.
Concentrated winter rain
Most rain falls in a short wet season, so drainage systems face heavy demand all at once. Poorly graded lots flood and water works into every summer-formed crack.
Crack growth between wet and dry cycles
Pavement dries and shrinks through summer, then takes on water in winter. That swing widens cracks, so sealing them before the rains matters.
Before you hire: The Pavement Directory does not guarantee contractor performance, pricing, licensing, insurance, or availability. Business information may be submitted by contractors or gathered from public sources and should be independently verified before hiring. Always confirm licensing, insurance, references, scope of work, and written contract terms.