Other constructions can follow the same indications with the proviso that a design .. Construction parasismique des maisons individuelles aux Antilles «Guide. Règles de Construction Parasismiques PS-MI 89 révisées 92(NF P). En zones de sismicité 3 Les Maisons Individuelles appartenant à la catégorie d’ importance II remplissant les conditions des règles CP-MI Antilles. 2. Conditions d’. Maisons IDEA est importateur et maître constructeur de maison en kit à ossature choix dans la construction de maisons individuelles à ossature bois (MOB).

Author: Vudokora Malami
Country: Belarus
Language: English (Spanish)
Genre: Art
Published (Last): 1 July 2008
Pages: 131
PDF File Size: 11.91 Mb
ePub File Size: 17.71 Mb
ISBN: 561-7-41985-489-8
Downloads: 88216
Price: Free* [*Free Regsitration Required]
Uploader: Mishura

Solution en matière d’habitation. Du sur mesure à votre mesure.

A second MOE building near the waterfront appeared intact was unable to gain access. Indeed, two-thirds of the buildings in Port-au-Prince were unsafe before the Jan. Along the boundaries, the relative eastward movement of the Caribbean plate, at the rate of less than an inch a year, creates strike-slip faults, shallow fissures whose sides slide in relation to one another in an earthquake. Of the 22 structures surveyed: The following bureaus, offices, inividuelles ministries were surveyed: A long segment in the Dominican Republic, not the entire fault, has consttuction without a quake for years.

Earthquakes and landslides along the Puerto Rico Trench, an undersea fault zone, have the potential to cause tsunamis. Wikipedia Commons12 mars Par Michel CorbeilLe Soleil.

Those buildings still standing will need to be tested for safety. Last Thursday, the geological survey issued a statement estimating that there was a 3 percent likelihood of a 7 magnitude aftershock in the individueles 30 days, and a 25 percent constrution of one of magnitude 6. Note from the author.

Countless other homes, stores, office buildings and more churches have been reduced to rubble. Debris will need to be cleared before new structures can take their place.

The Haitian quake itself might have added to the risks, researchers say.

Construction de la Tour Pearl River. Much of what is known about the seismic activity around Port-au-Prince has been gleaned from historical accounts of previous quakes.

The Amisons York Times To scientists who study seismic hazards in the Caribbean, individuellex was no surprise in the magnitude 7 earthquake that devastated the Haitian capital, Port-au-Prince, two weeks ago. Additionally, there are more than one thousand internally displaced persons camped on the property. Il y a aussi de bons ouvrages.


That raises the possibility that the Jan. But about miles to the northeast is a long segment of a similar fault, the Septentrional, that has not had a quake in years. After the tsunami in Indonesia, recent mudslides in Columbia, earthquakes in Mexico, in rural China and in Nicaragua—not to mention the devastation of Hurricane Katrina on the Gulf Coast of the United States—a template for rebuilding in poor countries has begun to take shape.

Rebuilding Haiti will be a tough haul. Researchers said that more study was needed on the Septentrional and Enriquillo faults and elsewhere in the Caribbean, and that governments needed to prepare better for the inevitable.

Researchers have estimated that a rupture along that segment — and again, they have no idea when one might occur — could result in a magnitude 7. But the bureaucratic silos that plagued the immediate efforts to save lives in New Orleans appear to be present in the Haitian relief effort as well. Stress to joints, window and door frames were effected and cracking on walls on lower floor. The study involved digging trenches across the fault construxtion looking for rupture lines in the sediments.

Victoria Harris, CEO of Article 25, a nonprofit architectural consulting maidons whose name derives from the United Nations charter naming the built environment as a human right, discussed the opportunity for Haiti to build a truly modern city on the ruins of what came before.

Constructeur de maison en kit à ossature en bois Martinique, Guadeloupe | Maisons IDEA

They were alternately conducted by Mess. Calais and others had warned in that a quake could occur along that segment, part of what is called the Enriquillo-Plantain Garden fault zone, although they could not predict when. Mais ils nous disaient, c’est pire chez eux! All those things have put the whole country on edge.

John McAslan, a partner for the architecture firm sponsoring the competition, said: Et je fais mienne cette affirmation de Jean Rostand: Prentice, a geologist with the geological survey in Menlo Park.


Le Coin de Pierre – Génie civil: février

There are already signs that the Haitian quake has prompted concern elsewhere in the region, at least among the general population. Such sequences have been observed on other faults, including the North Anatolian in Turkey. Although the results are preliminary, the work shows that stresses have increased just west of the segment and just east, within three miles of Port-au-Prince.

January 27, An article on Tuesday about seismic hazards conztruction the Caribbean referred incorrectly to the Septentrional fault, where some experts had thought an earthquake might indivoduelles occur on the island of Hispaniola.

While there were workers on the premise egress into the building was limited.

Si vous voulez allez droit au but, cliquez sur: And one building, the Ministry for Youth and Sport appeared to have suffered only minimal damages. This is a subduction zone — where the North American plate is sliding under the Caribbean, creating the potential for earthquakes and undersea landslides that can set off tsunamis. Major institutions—the national cathedral, the presidential palace—lie toppled.

Prentice and others have done basic research on a segment in the Dominican Republic. La taille du fichier pdf est de 58 Meg. Haiti, for example, has no seismometers, meaning there has been no way to measure all the small tremors that might help characterize the Enriquillo fault.

Unable to gain access because of rubble to egress areas. Of some construcion, researchers said, was that none of the aftershocks have occurred in the area of increased stress nearer to Port-au-Prince, where ordinarily some might have been expected.

On Wednesday, the area experienced a strong aftershock that was initially rated at 6. Researchers have relied on a network of 35 benchmarks to measure fault movement.