Glen Canyon Park

Islais CreekEdit

A branch of Islais Creek (named after the wild cherry islay) originates in the canyon. It is the largest remaining creek in San Francisco with public access. The bottom of the canyon, where Islais Creek flows, is irregular but moderate in slope, dropping 350 feet (107 m) over a distance of about 1 mile (1.6 kilometer). The creek is surrounded by willow thickets. In earlier times, the creek had an open water channel sustained by a much larger water flow, and was "more of a river than a creek". Urban development has reduced the watershed of Islais Creek by as much as 80 percent. At the southern end of the canyon, Islais Creek enters a culvert which carries it to its exit into San Francisco Bay.

WildlifeEdit

The creek has a meager but year-round natural flow, and the water and resulting vegetation provide a habitat for animals, including skunks, opossums, raccoons, red-tailed hawks, red-shouldered hawks, great horned owls, coyotes, and the rare native San Francisco forktail damselfly, Ischnura gemina.

Geology and rock outcropsEdit

The scenery of Glen Canyon Park is also distinguished by numerous large outcrops of rock. The most striking of these consist of reddish, layered "Franciscan" chert. These outcrops have clearly visible banding (see photo) which is due to the different weathering of the layers.

The bedrock of the canyon is made up of rocks of the Marin Headlands terrane, which is a large packet of rock that extends diagonally from the Marin Headlands (just north of the Golden Gate), through the Twin Peaks and Glen Canyon area, and on to the southeast. This terrane is from 100 to 200 million years old (i.e. the Cretaceous and Jurassic periods). The bedrock of the lower slopes of the canyon - largely hidden under slope debris/ravine fill - is pillow lava or greenstone; these erupted from fissures in the deep ocean floor when the terrane was located hundreds of miles southwest of its present location.

The upper slopes and cliffs are of layered chert, which hardened into rock from the ooze of remains of countless radiolarian creatures that accumulated on top of the lava. The ooze was colored red by iron from hydrothermal springs. Both lava and chert were formed in the deep ocean near the equator, and were rafted northeast on the gradually-moving ocean floor toward California. Near shore, greywacke accumulated on the chert in some areas, including a small part of the southeast slope of Glen Canyon. Subduction then squeezed the terrane against the continent, and it eventually became part of the Franciscan formation that makes up much of coastal California. During subduction - 160 to 80 million years ago - and the subsequent uplift, the terrane was twisted, broken and disrupted, and the chert was deformed into the tight folds now visible in road cuts along O'Shaughnessy Boulevard (see photo).

These rock outcrops provide some of the best outdoor rock climbing in San Francisco, primarily in the form of bouldering.

Sutro's Gum Tree RanchEdit

The park's history commences with Adolph Sutro's purchase in the 1850s of 76 acres (310,000 m²) of the canyon, which he named "Gum Tree Ranch" after the blue gum eucalyptus trees he had planted. The first commercial manufacturing of dynamite in the U.S. occurred in the canyon; on March 19, 1868, the Giant Powder Company began production at its first manufacturing plant, under exclusive license from Alfred Nobel to produce his new explosive in America. The plant was apparently located near the present recreation center, at the southern end of the park. The factory did not last long. On November 26, 1869, an explosion completely destroyed the entire facility, turning every one of the buildings on the place, and the surrounding fencing, into "hundreds of pieces", according to a newspaper account. Two people were killed, and nine injured; the plant was later rebuilt in the sand dunes south of Golden Gate Park. The site of the plant has been designated as California Historical Landmark #1002, although no marker has been placed on the site yet.

The Crocker eraEdit

In 1889, the Crocker Real Estate Company bought the canyon to develop a neighborhood that would attract homebuyers. As Jeanne Alexander has written,

Crocker installed a mini-amusement park with an aviary, a mini-zoo--bears, elephants and monkeys, a bowling alley, and, for extra thrills, hot-air balloon rides, and an intrepid tight-rope walker who performed on a wire stretched across the canyon. From 1907-1922, Glen Canyon Park was operated as a picnic ground -- mainly for adults. Crocker Real Estate added tables and benches, a baseball diamond and a running track. It was fenced and rented to organizations for company picnics that often turned into boisterous drinking brawls. Neighborhood children had to find other places to play. Concerned residents urged the San Francisco Recreation Commission to acquire the property for use as a playground, and in 1922, the city bought the 101-acre (0.41 km²) Glen Canyon Park and Recreation site.

City parkEdit

O'Shaughnessy Boulevard defines the western perimeter of Glen Canyon Park. This street was built in 1935 using roadcuts and filled slopes on the canyon's steep slopes, and was named after Michael O'Shaughnessy, who was for many years the Chief Engineer of the City. The recreation center at the south end of the park was built by the Works Progress Administration in 1937. An undeveloped, very steep area just west of O'Shaughnessy Boulevard was purchased by the City of San Francisco in the 1990s, and named O'Shaughnessy Hollow.

In 1958, the California State Highway Department proposed a plan to widen O'Shaughnessy Boulevard as part of a Crosstown Freeway. Some work was done at the southern end of the park, and homes and businesses were demolished along Bosworth Street to permit its widening. Further work ceased following opposition by several groups; the conflict over the freeway was among the earliest incidents in the Freeway and expressway revolts of the 1960s and 1970s.

Future managementEdit

The city government of San Francisco mandated the development of management plans for all the "natural areas" under the city's control, and this process culminated in release of the Significant Natural Resources Areas Management Plan in February 2006. The plan favors the re-establishment of native species and species diversity in the city's parks. Some aspects of the plan have been controversial. For example, the plan envisions the removal of some large, mature trees (often eucalpytus, which was imported from Australia) to favor smaller native plants. The plan also includes new restrictions on recreational use of the park, such as the closure of some trails and of some areas for rock climbing, and prohibitions against unleashed dogs.

In Glen Canyon Park, about 20 mature eucalpytus trees were removed in 2004 as part of an effort to increase the diversity of species living along Islais Creek. The plan envisions the removal of an additional 120 trees (of the total of 6000 trees in the park) to further improve the creek, to increase the extent of the park's grasslands, and to promote forest understory plants. The plan also seeks to restore some open-water areas along the creek, which is nearly totally obscured by the willow thickets. The change in the creek would be established both by re-planting sections of the creek's banks with different plants and by the introduction of "scouring" structures.

Glen Canyon Park used to support populations of two rare species: the "vulnerable" San Francisco forktailed damselfly and the "endangered" Mission blue butterfly. The plan proposes changes in the management of the park that would promote self-sustaining populations of these insects. The damselfly population in the park was studied by John Hafernik and his colleagues in the 1980s prior to its local extinction; they re-introduced a population of these damselflies in 1996 that persisted for two seasons. The damselflies need open water habitat, which has proven difficult to maintain.

There has been a declining population of Mission blue butterflies at the nearly contiguous Twin Peaks Natural Area; while park employees logged about 150 butterflies in the 1980s, only four were found between 2001 and 2007. A reintroduction was done in April 2009. Reintroduction may also be possible in Glen Canyon Park. Here the main issue appears to be re-establishing the native plant "silver bush lupine", whose leaves are the larval food of these butterflies. A substantial fraction of Glen Canyon Park is now covered by non-native species including eucalyptus forest (17 acres), French broom (6 acres), and field mustard, but no specific proposal for re-introduction of the lupine was included in the Management Plan.

Urban planningEdit

The importance of Glen Canyon Park to its surrounding neighborhoods is indicated by a recent community plan for Glen Park that contains the following statement: "The Glen Park community’s special character is created by the unique combination of eclectic building styles, pedestrian scale, the layering of green space and buildings climbing into the canyon, public spaces, walkable streets, a compact village, and proximity to transit and the canyon. Every new development project, whether public or private, must incorporate these features based on principles of good design and human scale."

A section of Bosworth Street connects the southern entrance to Glen Canyon Park with the central commercial district of Glen Park that lies about a third of a mile east. This section presents an important opportunity for urban design because the properties along the north side have remained undeveloped since their acquisition by the City in the 1950s. The community plan proposes that this land be developed into a greenway and pedestrian plaza. The plan also suggests that Islais Creek, which runs underneath this section of Bosworth Street, be "daylighted" in this section. The plan was formally endorsed by the San Francisco Planning Commission in 2004, but implementation has not been funded as of 2007.