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West Coast Memorial to the Missing of World War II

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The West Coast Memorial to the Missing of World War II is a monument dedicated to missing soldiers, sailors, marines, coast guardsmen, and airmen of World War II . It is a curved wall of California granite set in a grove of Monterey pine and cypress and overlooking the Pacific Ocean. It bears the name, rank, organization and State of each of the 413 members of the Armed Forces who lost their lives or were buried at sea in the Pacific coastal waters.

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28-532: It is located on high ground overlooking Baker Beach along the Pacific Ocean, at the intersection of Lincoln and Kobbe Boulevards, along the western edge of the Presidio of San Francisco , California . The architect was Hervey Parke Clark with landscape architecture by Lawrence Halprin . The sculptor was Jean de Marco , who won the 1965 Henry Hering Memorial Award for his work here. The West Coast Memorial

56-450: A great white shark while he was in water 15 ft (4.5 m) deep. This was the only shark attack recorded on Baker Beach. Large outcrops of serpentine cliffs occur along the Pacific coast near Baker Beach. When rising from the land surface, serpentine produces a low- calcium , high- magnesium soil that can allow for rare species of plants to develop in the vicinity. This may explain

84-721: A nearly constant layer curvature , with the larger octahedral sheet on the convex side. However, such curvature weakens the H-bonding between the layers. H-bonding tries to maintain flat layers, but this competes with the requirements of misfit compensation. As a result, the layers are locally either curved or flat. Antigorite , lizardite and chrysotile have the same chemical composition , but their different layer of curvatures result in lamellar agglomerated antigorite and lizardite and fibrous chrysotile elongated mineral particles. Serpentine minerals are ubiquitous in many geological systems where hydrothermal alteration of ultramafic rocks

112-425: Is a polar layer 0.72 nm thick. A Mg -rich trioctahedral sheet is tightly linked on one side to a single tetrahedral silicate sheet , regardless of the 3–5% larger lateral lattice dimensions of the octahedral sheet . The second level of the structure organized into different serpentine species originates partly to compensate the intra-layer stress due to this dimensional misfit. Good compensation results in

140-669: Is a public beach on the peninsula of San Francisco, California , United States The beach lies on the shore of the Pacific Ocean in the northwest of the city. It is roughly a 0.5 mi (800 m) long, beginning just south of Golden Gate Point (where the Golden Gate Bridge connects with the peninsula), extending southward toward the Seacliff peninsula, the Palace of the Legion of Honor and

168-506: Is easily carved, taking a good polish, and is said to have a pleasingly greasy feel. Less valuable serpentine ores of varying hardness and clarity are also sometimes dyed to imitate jade . Misleading synonyms for this material include "Suzhou jade", "Styrian jade", and "New jade". New Caledonian serpentine is particularly rich in nickel. The Māori of New Zealand once carved beautiful objects from local serpentine, which they called tangiwai , meaning "tears". The lapis atracius of

196-665: Is limited to indoor settings as serpentinites do not weather well. Soils derived from serpentine are toxic to many plants , because of high levels of nickel , chromium , and cobalt ; growth of many plants is also inhibited by low levels of potassium and phosphorus and a low ratio of calcium / magnesium . The flora is generally very distinctive, with specialized, slow-growing species. Areas of serpentine-derived soil will show as strips of shrubland and open, scattered small trees (often conifers ) within otherwise forested areas; these areas are called serpentine barrens . Lamellated antigorite occurs in tough, pleated masses. It

224-408: Is never stable relative to either of the other two serpentine polymorphs. Samples of the oceanic crust and uppermost mantle from ocean basins document that ultramafic rocks there commonly contain abundant serpentine. Antigorite contains water in its structure, about 13 percent by weight. Hence, antigorite may play an important role in the transport of water into the earth in subduction zones and in

252-851: Is one of three war memorials in the United States administered by the American Battle Monuments Commission; the others are the East Coast Memorial to the Missing of World War II in New York and the Honolulu Memorial . 37°47′55″N 122°28′41″W  /  37.79861°N 122.47806°W  / 37.79861; -122.47806 Baker Beach 37°47.592′N 122°29.04′W  /  37.793200°N 122.48400°W  / 37.793200; -122.48400 Baker Beach

280-644: Is possible, in both terrestrial (oceanic hydrothermalism, subduction zones and transform faulting) and extraterrestrial environments. The process of alteration from mafic minerals to serpentine group minerals is called serpentinization . Serpentine minerals are often formed by the hydration of olivine -rich ultramafic rocks at relatively low temperatures (0 to ~600 °C). The chemical reaction turns olivine into serpentine minerals. They may also have their origins in metamorphic alterations of peridotite and pyroxene . Serpentines may also pseudomorphously replace other magnesium silicates. Incomplete alteration causes

308-401: Is the serpentine most frequently encountered in carving and jewelry. The name 'retinalite' is sometimes applied to yellow bowenite. The New Zealand material is called tangiwai . Although not an official species, bowenite is the state mineral of Rhode Island , United States: this is also the variety's type locality. A bowenite cabochon featured as part of the "Our Mineral Heritage Brooch",

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336-567: Is usually dark green, but may also be yellowish, gray, brown or black. It has a hardness of 3.5–4 and its luster is greasy. The monoclinic crystals show micaceous cleavage and fuse with difficulty. Antigorite is named after its type locality, the Geisspfad serpentinite, Valle Antigorio in the border region of Italy / Switzerland . Bowenite , a variety of antigorite, is an especially hard serpentine (5.5) of light to dark apple green color, often mottled with cloudy white patches and darker veining. It

364-516: The Burning Man art festival. In 1990, park police allowed participants to raise the traditional large statue but not to set it on fire , since the beach enforces a limit on the size of any campfires. Subsequent Burning Man events have taken place in Black Rock Desert , Nevada . A fatal shark attack occurred on Baker Beach on May 7, 1959, when 18-year-old Albert Kogler Jr. was attacked by

392-447: The Romans , now known as verde antique , or verde antic, is a serpentinite breccia popular as a decorative facing stone. In classical times it was mined at Casambala , Thessaly , Greece . Serpentinite marbles are also widely used: Green Connemara marble (or 'Irish green marble') from Connemara , Ireland (and many other sources ), and red Rosso di Levanto marble from Italy. Use

420-533: The Sutro Baths . The northern section of Baker Beach is "frequented by clothing-optional sunbathers," and as such it is considered a nude beach . Baker Beach is part of the Presidio , which was a military base from the founding of San Francisco by the Spanish in 1812 until 1997. In 1904, it was fortified with disappearing gun installations known as Battery Chamberlin , which can still be viewed today. When

448-598: The kaolinite -serpentine group in the category of phyllosilicates ) are greenish, brownish, or spotted minerals commonly found in serpentinite . They are used as a source of magnesium and asbestos , and as decorative stone. The name comes from the greenish color and smooth or scaly appearance from the Latin serpentinus , meaning "snake-like". Serpentine subgroup is a set of common rock -forming hydrous magnesium iron phyllosilicate ( ( Mg , Fe ) 3 Si 2 O 5 ( OH ) 4 ) minerals , resulting from

476-596: The metamorphism of the minerals that are contained in mafic to ultramafic rocks . They may contain minor amounts of other elements including chromium , manganese , cobalt or nickel . In mineralogy and gemology , serpentine may refer to any of the 20 varieties belonging to the serpentine subgroup. Owing to admixture, these varieties are not always easy to individualize, and distinctions are not usually made. There are three important mineral polymorphs of serpentine: antigorite , lizardite and chrysotile . Serpentine minerals are polymorphous , meaning that they have

504-550: The physical properties of serpentines to vary widely. Antigorite is the polymorph of serpentine that most commonly forms during metamorphism of wet ultramafic rocks and is stable at the highest temperatures—to over 600 °C (1,100 °F) at depths of 60 km (37 mi) or so. In contrast, lizardite and chrysotile typically form near the Earth's surface and break down at relatively low temperatures, probably well below 400 °C (800 °F). It has been suggested that chrysotile

532-446: The EPA states an increased risk of developing benign intestinal polyps can occur. In its natural state, some forms of serpentine react with carbon dioxide and re-release oxygen into the atmosphere. The more attractive and durable varieties (all of the antigorite) are termed "noble" or "precious" serpentine and are used extensively as gems and in ornamental carvings . The town of Bhera in

560-608: The Presidio was decommissioned as a U.S. Army base, it became part of the Golden Gate National Recreation Area , which is administered by the National Park Service . The 160 acres (65 ha) property was settled by John Henry Baker in the 1850s and was known as Golden Gate Milk Ranch. The property location description varied, but is generally described as being approximately 4 mi (6.4 km) west of

588-459: The asbestiform types find use as thermal and electrical insulation (chrysotile asbestos ). The asbestos content can be released into the air when serpentine is excavated and if it is used as a road surface, forming a long-term health hazard by breathing. Asbestos from serpentine can also appear at low levels in water supplies through normal weathering processes, but there is as yet no fully proven health hazard associated with use or ingestion, although

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616-413: The city on the then Point Lobos Road (now Geary Blvd.) Baker died in 1863 and his widow, Maria, lost the property to foreclosure in 1879. In 1897, Baker's grandson, Fairfax Henry Wheelan sued to have the title returned to the heirs of John H. Baker, claiming that Baker's widow did not have the legal power to mortgage the property. From 1986 to 1990, the north end of Baker Beach was the original site of

644-630: The historic Punjab province of the Indian subcontinent was known for centuries for finishing a relatively pure form of green serpentine obtained from quarries in Afghanistan into lapidary work, cups, ornamental sword hilts, and dagger handles. This high-grade serpentine ore was known as sang-i-yashm in Persian , or 'false jade' in English, and was used for generations by Indian craftsmen for lapidary work. It

672-553: The name "false jade" or "Teton jade". Most serpentines are opaque to translucent, light ( specific gravity between 2.2 and 2.9), soft ( hardness 2.5–4), infusible and susceptible to acids . All are microcrystalline and massive in habit , never being found as single crystals . Lustre may be vitreous, silky or greasy. Colors range from white to grey, yellow to green, and brown to black, and are often splotchy or veined. Many are intergrown with other minerals, such as calcite and dolomite . The basic structural unit of serpentine

700-496: The presence of Hesperolinon congestum (the Marin Dwarf Flax, a threatened plant) in surrounding areas. To the north of the beach is Marshall's Beach and was the site of a Japanese Type 93 torpedo embedded in the beach sand in 1946. Historian Mark Felton believes it was fired by Japanese submarine I-15 in 1941, which was sailing near the waters off San Francisco. Serpentine group Serpentine subgroup (part of

728-468: The same chemical formulae , but the atoms are arranged into different structures, or crystal lattices . Chrysotile , which has a fibrous habit , is one polymorph of serpentine and is one of the more important asbestos minerals. Other polymorphs in the serpentine subgroup may have a platy habit . Antigorite and lizardite are the polymorphs with platy habit. Many types of serpentine have been used for jewelry and hardstone carving , sometimes under

756-828: The subsequent release of water to create magmas in island arcs , and some of the water may be carried to yet greater depths. Occurrence is worldwide, notable localities include New Caledonia , Canada ( Quebec ), US (northern California , Rhode Island , Connecticut , Massachusetts , Maryland and southern Pennsylvania ), Afghanistan , Britain (the Lizard peninsula in Cornwall ), Ireland , Greece ( Thessaly ), China , Russia ( Ural Mountains ), France , Korea , Austria ( Styria and Carinthia ), India ( Assam , and Manipur ), Myanmar ( Burma ), New Zealand , Norway and Italy . Serpentines find use in industry for several purposes, such as railway ballasts, building materials, and

784-467: Was presented to U.S. First Lady Mrs. Lady Bird Johnson in 1967. Williamsite is an American local varietal name for antigorite that is oil-green with black crystals of chromite or magnetite often included. Somewhat resembling fine jade, williamsite is cut into cabochons and beads. It is found mainly in Maryland and Pennsylvania . Gymnite is an amorphous form of antigorite. It was originally found in

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