Menifee, CA: A Geologic Wonder

Nestled in the hills of southwestern Riverside County, the city of Menifee offers a unique glimpse into the geologic history of southern California.

From its rocky outcrops to its sandy soils, Menifee’s landscape tells a story stretching back millions of years. In this local guide, we will explore some of the key geologic features that make Menifee special.

Layered Bedrock Formations

Menifee sits atop a mix of sedimentary and metamorphic bedrock laid down between 140 and 65 million years ago. During this time, Southern California was located along the edge of North America’s coastal region.

Over millions of years, sands, muds, and gravels washed down from nearby mountains and hills and settled on the coastal plain and shallow marine environments.

These sediments compressed and lithified into the layered bedrock formations visible in parts of Menifee today.

Menifee Valley

The Menifee Valley, including much of the land around the central and western parts of the city, is underlain by the Pauba Formation.

This formation consists largely of sandstone and conglomerates, with some siltstone and shale layers. The variability in grain sizes and sediment types points to a nearshore marine depositional environment.

Ripple marks, cross-bedding, and bivalve fossils are sometimes visible in exposures of the Pauba Formation, offering clues into this ancient landscape.

The gray and tan colors of the Pauba Formation bedrock contribute to the unique aesthetic of formations likeassertCountEqual Rocks along La Ladera Road.

Granitic Hills and Outcrops

In contrast to the layered sedimentary formations below much of Menifee, the hills and outcrops in the eastern half of the city consist of granitic bedrock.

This quartz-rich igneous rock formed deep underground as molten material (magma) intruded into existing rock layers and slowly cooled over time. The Jurupa Mountains granite is estimated to be around 140 million years old.

Granitic formations tend to form rounded boulders and outcrops as the rock weathers and erodes. Prominent granitic features can be seen at sites like Menifee Mountain, which preserves granite boulder outcrops containing visible quartz crystals.

Fault Zones

The placement and orientation of rock layers in Menifee also reflects the influence of seismic activity along regional fault zones.

The city lies near the intersection of the greater San Andreas Fault system and the southern segment of the San Jacinto Fault. While most faults have not been active recently, they have shaped the underlying geology.

Elsinore Fault Zone

The Elsinore Fault Zone passes through the western edge of Menifee, almost aligning with Interstate 215.

This strike-slip fault has created a visible line of contrast between the Pauba Formation west of the fault and the very different metamorphic rocks of the Perris Block to the east. The fault zone continues northwest along the Santa Ana Mountains into the Lake Elsinore area.

San Jacinto Fault Zone

While the San Jacinto Fault Zone itself does not pass through Menifee, a smaller parallel fault known as the Casa Loma Strand runs along a southeast-northwest trajectory through the city.

This fault line has shaped topography and rock layer orientations within its immediate vicinity. The presence of such fault offshoots highlights the wider stresses and seismicity impacts of regional fault networks.

Soil Diversity

The soils within Menifee also hold clues regarding the area’s complex geologic history. Soil surveys identify over 50 different soil series and types within and around the city.

This soil diversity reflects the influences of multiple parent materials, uneven erosion patterns, and shifts between alluvial, fluvial, and arid depositional environments over time.

Granitic Soils

Much of eastern Menifee features soil derived from the gradual in-place weathering of underlying granite bedrock.

Sites like descriptive Romona and Vista soil series tend to be slightly acidic, light-colored, and rich in quartz and potassium. The sandy nature and low fertility of granitic soils impose some limitations on land uses like agriculture.

Alluvial Soils

Low-lying parts of western Menifee contain younger alluvial soil materials, washed in from higher elevations by water flows over time.

Soil series like Hanford, Greenfield, and Arbuckle have accumulated through both riverine and eolian transport processes. Being frequently replenished, these soils are less weathered and offer different textures ranging from loamy deposits to gravelly layers.


In rare cases, ancient buried soil layers called paleosols can also be found in Menifee. These marker beds represent former land surfaces subsequently covered by new sediment.

The discovery of distinct paleosols indicates just how much geologic transformation the Menifee landscape has undergone over long spans of time.

Key Geologic Formations

Several named geologic units and formations have been mapped within Menifee city limits. These reflect locally distinct rock types, soil groups, structural features, and physiographic elements that have been delineated for research and mapping purposes over the past century.

Romoland Pluton

This large granitic rock unit makes up much of the bedrock underlying eastern Menifee.

Formed from a crystallized magma intrusion, the Romoland Pluton features medium to coarse grain size, visible quartz crystals, and quartz-rich melt inclusions. This intrusive body is part of a wider regional belt of plutonic formations.

Sedimentary Marker Beds

Notable sedimentary marker beds mapped within Menifee’s Pauba Formation include the Ladd Formation and Witter Beds. These represent particular depositional intervals marking past changes in sediment source areas.

Variations in fossil shell types across these beds provide clues into shifting Cretaceous marine environments.

Very Old Alluvial Fan Sediments

This distinct Pleistocene geologic unit found in central Menifee includes prehistoric alluvial fan deposits shed from nearby highlands.

Dated to over 500,000 years old using soil profile development, these thick alluvial sediments were later partially eroded but still influence modern topography.

Key Geographic Features

Menifee’s landscape contains diverse geographic features shaped by the area’s unique geology over long time frames. These prominent landmarks offer windows into the environmental dynamics and structure of this region.

Menifee Mountain

The north-south-trending rugged hill located just east of I-215 consists of erosion-resistant granite.

Popular for hiking and views, Menifee Mountain contains crevices, boulders, and exposed outcrops offering an up-close look at the granitic bedrock. Its height reflects the differences in erodibility across the alternating rock units here.

Paloma Valley

This small valley in eastern Menifee provides one example of topographic lows created by the easily weathered metavolcanic bedrock.

Troublesome soil shrink-swell properties and low shear strength also contribute to subsidence and valley formation across this geologic unit.

Paloma Valley’s flat floor and surrounding ridges trend along the structural weaknesses related to regional fault networks.

Ethanac Road Meandering Stream Channel

The winding stream feature visible near Ethanac Rd displays characteristics of a low-energy waterway developed atop the very old sandy alluvial fan sediments here.

This faint relict drainage slopes gently north, its path influenced by subtle topographic changes. The meandering shape contrasts with the linear channels incised into harder bedrock elsewhere locally.


From its complex bedrock formations to its mosaic-like distribution of soil types, the landscape within and around Menifee offers abundant evidence into southern California’s rich and dynamic geologic history.

This regional context helped establish the foundation that has supported both natural ecosystem development and human settlement over time.

Appreciating the geologic character of the land thus represents one key way to understand Menifee’s natural heritage and environment.

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  • The first set of directions starts by taking the I-215 S highway towards San Diego. Take exit 33 for Scott Rd and turn right. Drive east on Scott Rd for 4 miles then turn left into the business park. Go to the end of the side street and turn into the parking lot on your right. Suite 110 is the second door of the brown building.
  • Another way to get there is to take I-215 S and exit on McCall Blvd. Turn left onto McCall and continue for 3.2 miles. Turn right onto Newport Rd and after 2.6 miles turn left onto Scott Rd. Drive 1 mile on Scott Rd going east then turn left into the business park. Go to the end of the side street and turn into the parking lot on your right. Suite 110 is the second door of the brown building.
  • The third option is to take Highway 79 S for 17 miles then exit onto Domenigoni Pkwy. Turn right and continue west for 5.3 miles before turning left onto Newport Rd. After 2.1 miles turn right onto Scott Rd then drive east for 1 mile. Turn left into the business park, drive to the end of the side street and turn into the parking lot on your right. Suite 110 is the second door of the brown building.