Gravitational waves change the shape of everything.
Circles are distorted into ellipses back and forth like the patterns below.

Laser Beams and Mirrors
Detectors consist of two long vacuum pipes constructed at right angles to
each other. A laser beam is split into two identical beams which travel
down each pipe arm and are reflected back precisely by supermirrors delicately
suspended at the ends of the arms, as shown in the diagram opposite. The
two beams come back together in such a way that they would cancel out if
the two arms were identical. A gravitational wave that passes through the
detector simultaneously shrinks one arm while stretching the other. This
stretching and shrinking alternates between the arms. These differences
in the length of the arms change the perfect cancellation of the beams,
causing a brightness variation that is proportional to the strength of the
wave. These tiny variations in brightness are picked up by light sensors
and amplified. The entire detector is like a supersensitive microphone -
one that is about one billion times more sensitive than a human ear! The
longer the arms, the bigger the changes caused by gravitational waves, so
it is essential that the detectors are several kilometres in length.
Vibration Isolators
Because gravitational waves are tiny vibrations, the first task is to prevent
any sound and ground vibrations from the outside world from reaching the
mirrors. This is achieved with vacuum, and vibration isolators which consist
of chains of masses, springs and pendulums designed to absorb all vibrations
that could otherwise reach the mirrors. The picture below shows a section
of a vibration isolator. Vibration isolators developed for gravitational
wave detection are the most advanced in the world and have many wider applications.
Supermirrors and Vacuum Chambers
Gravitational wave detectors use the most perfect mirrors ever created in
order to measure the tiny vibrations. These mirrors are called ‘test masses’
and they are made out of artificial sapphire and fused silica. The mirrors
must be of a large size - about 30 cm in diameter, and heavy - about 40
kg. Seven such mirrors are required in a detector as shown in the picture
opposite. The laser beams must be very intense - about as bright as a billion
laser pointers! To prevent any disturbance, they must travel in a nearly
perfect vacuum - the pressure must be less than one thousandth of a billionth
of atmospheric pressure! Very carefully prepared stainless steel is required
in order to achieve such a vacuum.

Optical Cavities
The laser beam is built up by resonance inside an optical cavity. Optical
cavities reflect light back and forth between mirrors, building up the light
intensity in the same way that repeated pushing builds up the swinging of
a playground swing. First, intense laser light enters the detector through
a partially transmitting mirror, called the power recycling mirror, and
into a ‘beam splitter’ which separates the light into two beams at right
angles to each other. The beams then enter the long vacuum pipe through
the input test masses, which are partially transmitting mirrors delicately
suspended at each end. They then bounce back and forth between the input
test mass and the end test mass. After several hundred kilometres of travelling
back and forth between the mirrors, the beams become very intense. They
return to the beam splitter where they are recombined. Most of the light
passes back towards the laser, only to be reflected back on itself by the
power recycling mirror. This process repeats itself many times. Overall,
the incoming light combines with light already in the optical cavities,
until the light power inside the instrument has built up by resonance to
be thousands of times brighter than the original beam. A tiny bit of this
light is modified by the passage of gravity waves. This modified light,
which carries the gravity wave signal, is directed towards the signal recycling
mirror, which again reflects most of it back into the instrument. This process
also repeats itself so that the light containing the signal is built up
by resonance. Finally, it is detected by a light sensor, called a photodetector,
at the output where it is measured and processed by a computer.
Earthquakes and Lightning
Earthquakes, lightning and other disturbances are measured separately to
ensure that false signals are recognised. Accurate timing information is
coded with the data so that the arrival times of signals can be compared
with those from other observatories, giving a fuller ‘picture’ of the wave.
The further apart detectors are on the globe, the better their ability to
map a wave.

