It was designed by architect Maurice Mizard in a highy detailed Art Nouveau style. Opened in 1913, the Lutetia Cinema Wagram was a movie house located in the 17th arr. In fact, only one of the movements – the Ballade – is more than two minutes long, while three others clock in at a minute or less apiece. as his main publisher).Ĭollectively lasting fewer than 13 minutes in duration, Petites musiques is made up of the following short movements: Entrée Bourrée Pastorale Fanfare Ballade Ronde Bercement Ländler. 32, a set of eight short pieces published in 1906 by Eschig, one of the composer’s early publishing outlets (he would later settle on Durand et Cie. Such a work is Schmitt’s Petites musiques, Op. In fact, several of the sets seem to have been created by Schmitt for students and other pianists possessing limited technical capabilities. In many instances, Schmitt’s piano compositions make considerable technical demands on players, but this is not always the case. Most of this output dates from the composer’s early years of creativity from about 1890 to the mid-1920s, although several additional sets of solo piano pieces would be published in the runup to the Second World War. Within the extensive catalogue of compositions by Florent Schmitt are a great many works for piano – including solo, duet and duo-pianist pieces. The total loss of life by a factor of 3 or 4.Florent Schmitt, photographed around 1900, several years before he composed Petites musiques. The frequently quoted value of 700 deaths causedīy the earthquake and fire is now believed to underestimate However, was equally severe in many other places along theįault rupture. It spawned in San Francisco, giving it the somewhat misleadingĪppellation of the "San Francisco earthquake". Mind, this earthquake is perhaps remembered most for the fire The most important study of a single earthquake. (1908) report remains the authoritative work, as well as arguably Modern seismic-zonation practice accounts for the differences in seismic hazard posed by varying geologic conditions.Īs a basic reference about the earthquake and the damage itĬaused, geologic observations of the fault rupture and shakingĮffects, and other consequences of the earthquake, the Lawson Areas situated in sediment-filled valleys sustained stronger shaking than nearby bedrock sites, and the strongest shaking occurred in areas where ground reclaimed from San Francisco Bay failed in the earthquake. One important characteristic of the shaking intensity noted in Lawson's (1908) report was the clear correlation of intensity with Of VII to IX paralleled the length of the rupture, extending as far as 80 kilometers inland from the fault trace. The highest Modified Mercalli Intensities (MMI's) Oregon to south of Los Angeles and inland as far as central Nevada. Violent shocks punctuated the strong shaking which lasted some 45 to 60 seconds. The great earthquake broke loose some 20 to 25 seconds later, with an epicenter near San Francisco. Of the earthquake source, which remains today the principalĪt almost precisely 5:12 a.m., local time, a foreshock occurred with sufficient force to be felt widely throughout the Sanįrancisco Bay area. The advent of plate tectonics more than half a century later.Īnalysis of the 1906 displacements and strain in the surroundingĬrust led Reid (1910) to formulate his elastic-rebound theory Large cumulative offset would not be fully appreciated until Indeed, the significance of the fault and recognition of its Large, horizontal displacements and great rupture length. The earthquake confounded contemporary geologists with its San Juan Bautista to the triple junction at Cape Mendocino, Rupturing the northernmostĢ96 miles (477 kilometers) of the San Andreas fault from northwest of Today, its importanceĬomes more from the wealth of scientific knowledge derivedįrom it than from its sheer size. The most significant earthquakes of all time. The California earthquake of Apranks as one of (from Steinbrugge Collection of the UC Berkeley Earthquake Engineering Research San Francisco City Hall after the 1906 Earthquake.
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