By Molly Bentley
in San Francisco
|
Another magnitude 7.9 earthquake in the San Francisco Bay Area would probably produce much stronger shaking than the catastrophic 1906 event of the same size.
The wider region should also expect thousands of fatalities and economic
losses in the billions.
These conclusions are contained in two reports released to coincide with
the 18 April centennial of the great quake that destroyed the city and killed
3,000 people.
The studies will be discussed at a special conference this week.
Scientists say the next big quake - a magnitude 6.7 or larger - will likely come within 30 years.
The first study, When the Big One Strikes Again, was commissioned by conference organisers and provides an estimate range of the death and damage toll for Northern California if an earthquake similar to 1906 hit the region today.
 |
The city was shattered, and what remained then went up in flames

|
The other study, produced by the US Geological Survey (USGS), shows how shaking intensity would change if the San Andreas Fault were to rupture in a
different place to 1906.
USGS scientists believe they have been able to reproduce the ground motion
that occurred 100 years ago fairly accurately, making it a useful model
to estimate the damage caused by the next big quake.
"These studies allow us to model the shaking and fill in the big gap in
the data," said Dr Greg Beroza, a geophysicist at Stanford University
who helped create the USGS simulation. "We can apply the results to
other large earthquakes."
Time differences
The conference-commissioned report was prepared by Charles Kircher, a
private engineering consultant.
 |
The chances of another big Bay Area quake have been assessed

|
One of its shaking scenarios suggests that out of the 10 million
residents in 19 counties, a 7.9 earthquake could kill 1,800 and
seriously injure 8,000 if it hit at night; and kill 3,400 and seriously
injure 13,000 if it hit during the day.
Total economic losses could reach more than $120bn.
"Daytime casualties are typically higher than night-time, when people are
in homes that are less susceptible to collapse than commercial
buildings," said Dr Kircher.
However, the proportion of night-time deaths is raised slightly in San
Francisco itself, where older homes are more vulnerable to collapse.
Roughly one quarter - 800 - daytime deaths and almost a third of
night-time deaths- 574 - would be in SF city districts.
The estimates are based on death by building collapse by shaking alone;
not by fire, which could raise the death toll. Of the city's 400,000 residents in 1906, it is estimated that 3,000 died from both building collapse and the conflagration that swept the city immediately afterwards.
While it was unlikely a fire that size would rage again, smaller fires
were very possible, said Dr Kircher.
 |
"Soft storey" architecture often features an un-reinforced garage
|
"We expect fires to contribute significantly to the total loss," he
added.
Adding in the cost of damage due to fire and lifeline infrastructure -
such as highways - could raise the economic bill to $150bn. And this
does not include long-term economic impact, the sort experienced in New
Orleans after Hurricane Katrina.
The total is 10 times the loss from the 1989 Loma Prieta Earthquake, a
6.7 tremor on the San Andreas Fault centred in a mountainous region
100km (60 miles) to the south of San Francisco.
Steady improvement
Dr Kircher's study estimated loss to the area by using two 7.9 shaking
scenarios that produced two sets of figures.
One set, expressed by the Modified Mercalli Intensity (MMI) scale, is
based on a re-evaluation of the actual ground shaking in the 1906
earthquake. (However, scientists do not expect the ground to shake
exactly like it did in 1906.)
The second set, referred to as M7.9, is based on a standard model of
energy propagation from an earthquake occurring on the segments of the
fault that ruptured in 1906; a sort of generic 7.9 quake.
Death and damage estimates are lower in the MMI model than in the M7.9;
800 night-time and 1,600 daytime deaths for the region, and $90bn
dollars in economic loss.
While the population has increased 10 fold since 1906, when less than a
million people called the greater San Francisco Bay area home, the
number of fatalities does not increase proportionally in the recent
estimates.
"Our knowledge of earthquakes and how they affect buildings have
advanced quite a bit and our seismic codes have been advancing," said Dr
Beroza, "but we're still talking about thousands of deaths. Will the
public say that's acceptable?"
Dr Kircher said that an important finding of the study was that
vulnerable buildings - un-reinforced masonry, older reinforced concrete
and "soft-storey" - made up less than 5% of all buildings in the region but would kill more than half the people.
"Fixing those buildings would cut our casualties in half," said Dr
Kircher.
Moveable epicentre
The second USGS study to be presented to the conference offers scientists a
re-creation of the 1906 shaking, and a how it might change if the fault
ruptured other than where it did, 2km off the coast of San Francisco.
The computer model draws on a new and highly detailed 3D geologic model
of the Bay Area.
 |
USGS SHAKING SIMULATION
For a rupture on the San Andreas Fault in the same place as the 1906 earthquake (100k)

|
While scientists do not know when the next big quake will come or where
it will originate, they do say that a 7.9 quake is unlikely to mirror
1906.
"There is no guarantee that the next big one will begin exactly where
the last big one began," said Dr Beroza. "It will be different and may
not start in the same place."
In the USGS simulations, a rupture at the northern end of the San
Andreas Fault, with the same amount of slip, creates the same or greater
shaking for San Francisco as it did in 1906; while an epicentre at the
southern end of the northern portion of the fault, near San Juan
Batista, creates considerably stronger shaking for the city.
 |
USGS SHAKING SIMULATION
A rupture at the northern end of the San Andreas Fault at the location of Bodega Bay (100k)

|
This is due to variations in local geology and the fact that the energy
from the rupture and seismic waves increase as they propagate toward the
city.
"Things could be worse for San Francisco itself with a rupture that
begins south of the city, than it was in 1906 when the rupture began
very close to it," said Brad Aagaard, a USGS research geophysicist
who ran the simulations.
This, ironically, makes the original 1906 quake, with its epicentre
near the city, a best-case scenario for San Francisco if a 7.9
earthquake were to hit again.
 |
USGS SHAKING SIMULATION
A rupture to the south of San Francisco near the location of San Juan Bautista (100k)

|
But increased shaking in one area means less shaking somewhere else.
Moving the epicentre to San Juan Batista produces more intense shaking
for San Francisco, but milder shaking in the Silicon Valley region.
"The bottom line is that the next large event on the San Andreas Fault
will differ in some ways from the 1906 earthquake," said Dr Aagaard. "We
need to consider many scenarios in order to be prepared for such an
event."
The 100th Anniversary Earthquake Conference continues through to 21
April in San Francisco.
SUMMARY OF DAMAGE AND LOSSES
|
|
SCENARIO
|
1906 MMI
|
M7.9
|
NUMBER OF SEVERELY DAMAGED BUILDINGS
|
Residential buildings
|
80,000
|
120,000
|
Commercial buildings
|
7,000
|
10,000
|
SOCIAL LOSSES DUE TO BUILDING DAMAGE
|
Displaced households
|
170,000
|
250,000
|
Serious injuries - night-time
|
4,000
|
8,000
|
Serious injuries - daytime
|
6,000
|
13,000
|
Immediate deaths - night-time
|
800
|
1,800
|
Immediate deaths - daytime
|
1,600
|
3,400
|
DIRECT ECONOMIC LOSSES DUE TO BUILDING DAMAGE
|
Structural damage
|
$15bn
|
$20bn
|
Non-structural damage
|
$57bn
|
$75bn
|
Contents and inventory damage
|
$14bn
|
$17bn
|
Business interruption
|
$8bn
|
$11bn
|
TOTAL DIRECT ECONOMIC LOSS
|
>$90bn
|
>$120bn
|
Source: When the Big One Strikes Again
|