Visitors hiking in the hidden gem of Torrey Pines Reserve Extension will likely wonder about the giant wire baskets of rocks that don't seem to do anything. Were they part of a building foundation? What was their purpose? How long have they been there? Well, before we get to the answer, let's travel back in time a little bit.
In The Beginning
The earliest aerial photo of the area that I've found is from 1953, and it's perfect. It shows exactly what the area looked like before much of the construction was done around what is now Torrey Pines Reserve Extension.
The "valley" in 1953 was a gently sloped u-shape that emptied out into a large outwash plain that was being used for farming. Sand movement and erosion was minimal due to the large amount of mature vegetation. There is also a noticeable lack of roads, paths, and other human intervention.
Torrey Pines Reserve Extension Area in 1953 |
Note: to help with orientation, all of the aerial photographs have two points of interest. The orange star is where the Sea Village tennis courts are today, and the yellow star is the junction of two existing trails in the Extension.
Del Mar Heights Run-off
The 1960s were a time of great expansion of Del Mar, with the streets and neighborhood of Del Mar Heights being built out. Del Mar Heights School was built in 1964, and families moved in as houses were built. The biggest issue from this build out was that all the rain that fell on Del Mar Heights was funneled all at once by roads and gutters directly into the Del Mar Terrace canyon. This newly created flash flood farm needed remediation.
Looking at the following aerial view comparison, it is easy to see that something dramatically changed between 1964 and 1966. During that time an access road was cleared through the extension all the way through to Del Mar Heights, and significant sandy areas were primed for the erosion and gullies that soon followed.
Aerial view comparison of 1964 and 1966 |
The First Attempt at Erosion Control
About 1970 the situation was clear, and local residents took matters into their own hands. They got whatever approvals they needed, and they build a series of earthen dams throughout the canyon. By covering the mounds of dirt with sheets of plastic, they were able to create basins to catch the flood waters and prevent the increasing erosion. What was nice about this system was that every year they could push the newly deposited sand up onto the dam, making it higher, and put the plastic back over the top.
1973 photo of first erosion dams by Jessica La Grange, Torreyana #235, Dec 1995 |
The Reserve
During the Del Mar Heights build-out, a growing concern started at the grass-roots level to protect some of the green space and natural habitats in the area. In 1970, with money from dances, bake sales, and national media attention, citizens were able to raise enough to get a $900,000 grant in matching funds to purchase the 197 acres that now make up the Torrey Pines Reserve Extension.
1972 Flood
The storms of November 1972 brought a tremendous amount of rain to the freshly graded area that was soon to become Sea Point and Sea Village. The area had never recovered from the bulldozing and trenching a few years earlier, so the rain water cut wide gullies through the canyon sand. Without any vegetation to stop it, water and sand made its way down the hill to completely cover the intersection of Carmel Valley Road and McGonigle/Del Mar Scenic Parkway. This was a wake-up call to the city and developers. Not only was the lagoon filling up with sand, but the forthcoming townhouse owners certainly wouldn't want to be dealing with sand every time in rained.
1973 Sea Point and Sea Village
Between 1972 and 1974, two townhouse communities were built directly on the outwash plain of the canyon. Read my post on Sea Point and Sea Village for more on that.
And the answer is... Gabions
So, the answer to what those large wire and rock structures are is finally here. You've been patient, so here's what they are: hey are flood/erosion control gabions (GEY-bee-uhnz) that were installed in 1977 to help control run-off from the Del Mar Heights neighborhood. And yes, while it seems strange when you're hiking there in the summer, massive amounts of water do run through the reserve about once a year (whether we need it or not).
Torreyana #235, Dec 1995 |
Who Built The Extension Gabions?
Walking up the trail into the Extension from the south entrance, one sees small dam-like structures that consist of rocks contained by what appears to be fence material. These are called gabions. (American Heritage Dictionary - gabion 1. A cylindrical wicker basket with earth and stones, formerly used in building fortifications. 2. A hollow metal cylinder used especially in constructing dams and foundations. ; from Italian gabbia, cage.) These are actually the second structures to be built to control erosion in this area.
Prior to about 1960 the bottom of the Extension "valley" was covered with shrubs and plants. A fire in 1962, removal of brush a few years later, and then installation of water and sewer lines and a dirt access road up the center of the valley all led to serious erosion, with deep gullies formed by water runoff. About 1970 some of the local residents, with tacit approval of the rangers, started building small dirt dams to reduce erosion. These were over 6 feet high and covered with plastic with rocks on top to hold the plastic. Over the next few years about a dozen residents, with help at times from scout groups, built a number of these dams.
In 1977-78 these were replaced with the present gabions, built by the Youth Conservation Corps (YCC) and the California Department of Forestry. According to Ranger Chris Platis, who worked with the YCC, about 35 gabions were built.
Many of the gabions are now in need to rebuilding, and additional retaining structures appear to be need, which shows the power of rain runoff in even a small area such as the Extension.
1977 The Gabions are Built
In 1977 the make-shift dam system was replaced with concrete forfeited gabions -- wire cages filled with large rocks. These were built by the Youth Conservation Corps (YCC) and the California Department of Forestry (as reported in Torreyana #235 above). While 35 gabions were built, only 18 remain visible today. When installed, these appeared to be a formidable and permanent solution to a growing erosion problem.
The Flood of March 1978
Just after completion of the official final gabion system, they were faced with their first big test. After many years of drought, the first few months of 1978 in Southern California were wet. Very wet. A drought-breaking winter that filled up the reservoirs that had been empty for most of the 1970s. There was a ton of rain in February that completely saturated the ground and had already started eroding away and filling the newly built gabion basins in the Extension.
At 11:00am on Saturday, March 4th 1978, an extremely heavy rain came down all at once in a very short period time over Del Mar Heights. It was calculated to be at least 1 inch per hour.
Report on Floods of Feb & Mar 1978 in So. Calif., U.S. Army Corps of Engineers, pg 5 |
It was a lot of rain, and many papers reported on it in exhaustive detail nationwide. Here's a local headline example with accompanying photo.
Escondido Times-Advocate the next day |
Water came rushing down from the Extension canyon, flowed right over the tennis courts and emptied out onto Del Mar Scenic Parkway on its way down to the lagoon. It carried a great deal of sand with it, jamming up the storm drain system and flooded at least one house downhill (at the corner of Del Mar Scenic Parkway and Caminito Mar Villa).
Photo taken about noon on March 4, 1978, courtesy K. Oesterreicher |
The Gabion Flood Control System in Detail
In 2003, Michael Furtaw wrote a very detailed paper for San Diego State University called, Maintaining Erosion Control at the Torrey Pines Reserve Extension. The following summary is an excerpt from his work, along with his numbering system that I use for the updated report that follows.
- Located at the mouth of the channel. It is holding back a large mass of sand behind it. Most likely maintained. A drain is located after it that takes the water underneath Del Mar Scenic Parkway.
- Filled to the top
- Concrete wall with three 3inch diameter drains that are all clogged.
- Filled to the top. Secondary drainage forming around East side.
- Filled to the top. Drainage is completely routed around East side.
- a) Filled to the top. Small step before 6b. b) Filled to the top and tilted forward on East side. Measured at the center of the wall for average height. West side of gabion eroded and exposed, but still erect.
- Not filled. Drainage completely routed around East side.
- a) Filled to the top. Small step before 8b. Steep cliffs carved out. b) Filled to the top. Drainage completely routed around East Side. Steep
- Filled to the top. Drainage completely routed around East Side. Steep
- Concrete footing of wall remains. Looks to have been removed by man. Drainage routed around west side of the destroyed gabion.
- East side of gabion failed due to channel erosion around the concrete footing . Drainage routed around East side of of gabion. Steep cliffs carved out.
- Filled to the top. There is a small rock pile at the base, but not a gabion.
- Filled to the top. The channel had previously meandered around the East side of the gabion (widening the entire channel to 50ft), but it was later filled in with sediments as a fix. Current channel width is 20ft.
- Filled to the top.
- Not filled. Drainage routed around West side. Created a deep narrow cut due to a change in lithology.
- Completely buried with sediment, but still erect. Drainage routed around East side. No longer has an effect on the gradient.
- Not filled. Tipped over completely Southward. Drainage routed around West side of gabion. It carved a narrow and deep channel, cutting underneath the West footing of the gabion causing it to fail.
- Not filled. Erect.
Gabion impact on Torrey Pines Reserve Extension |
Here's a really important image of the surrounding area in 1966 as the Del Mar Heights build out was underway. Highway 5 is newly finished, and there appears to be a construction road that connects Mar Scenic at the top of the hill to what will become Del Mar Scenic Parkway to the south. This road would make bringing in the large amount of rocks used in the gabion system much easier.
1966 aerial view of Torrey Pines Reserve Extension |
Aerial view of Torrey Pines Reserve Extension 2021 |
The Remaining Gabions
#12 in 2022 |
Heavy erosion around Gabion #11 in 2022 |
The remains of Gabion #10 |
#9 |
Climbing on Gabion #8 in 1978, courtesy K. Oesterreicher |
Gabions #7 & #8 in 2022 |
Gabions #6, 7, and 8 |
Gabion #5 in Torrey Pines Reserve Extension, 2022 |
Gabion #4 |
Gabion #3 in 2022 |
Gabion #2 in good repair but completely filled in 2022 |
Rangers digging out basin in April 2020 |
This basin does its job, and prevents a great deal of sand from running into the storm drain system that starts directly behind the stone wall.
Gabion #1 at lower flash flood basin, Feb 2022 |
Partially dug out basin (facing south from Gabion #2 in Feb 2022) |
With annual maintenance, this last basin is large enough to hold a great deal of water and prevent a runaway flash flood. It is also big enough that maintenance of any other gabion basin up-stream is unnecessary.
Flood Basin filling with water in Feb 2019 |
The Last Stand: The Siltation Basins
The final step in the flood control system is the siltation basin at the bottom of the hill, across the street from the lagoon. In 2001, Maryruth Cox wrote a great article about in Torreyana.
Article from Torreyana, May 2001 page 9 |
Today the homeowners at Sea Point have a beautiful park for walking their dogs and enjoying the sun in private. It's clearly prime real estate that would have been an amazing place for beachside houses. If you were wondering why it's left open, wonder no more. It's a sand basin!
Sea Point Dog Park, aka the Siltation Basin in 2022 |
The final step in the current flood control system is the outflow into the lagoon catch basin. This was dug-out on state property across the street from Sea Point. It catches any remaining silt, and joins the lagoon out to its mouth on Torrey Pines State Beach.
Final outflow into Los Peñasquitos Lagoon |
Sources:
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