March 26, 1750.
When so great and unusual a phenomenon,
as an earthquake, and that
repeated, happens among us; it
will naturally excite a serious reflection
in everyone that is capable of thinking.
And we cannot help considering it, both in a
philosophical and a religious view. Any mind
will take the alarm when we perceive a motion
that affects the earth, that bears the whole
city of London, and some miles round it.
And at the same time while it gives us so sensible
a shake, so gently sets us down again; without
damage to any buildings, and without a
life lost.
'Tis hard to say, which is the greater wonder.
But alas in the works of nature, there
are no degrees of great, and little; comparisons
are incompatible. We indeed are more affected
with what seems great in our own apprehensions:
I would rather say, what is rare and
unusual. An omnipotent power admits of
no distinctions. And when prodigious effects
are produc'd from causes imperceptible, it rightly
claims our most serious attention, as well as
wonder. Nor need we lose sight of the theological
purpose of these amazing alarms; whilst
we endeavor to find out the philosophy of
them.
Among all the appearances of nature, which
are the subject of the inquiries of the Royal
Society, none more deserves the regard of a
contemplative mind. And among the very
numerous accounts received there, from all
quarters, being only Observations upon the
manner of it, and its extent: I judg'd, it became
us to inquire into the cause of so extraordinary
a motion: of which we could not form a
proper idea; had we not repeatedly seen, and
felt it.
The moderns have not improv'd upon the
opinions of the ancients, in this matter; any
further than by the fancied analogy of some
chymical experiments. But these chymical
experiments, and all sorts of explosions by gun-powder,
and the like, are to me a very unsatisfactory
solution they are merely artificial
compositions, which can have nothing similar
in the bowels of the earth, and they produce
their effects by violence, by rending and tearing,
by a solutio continui. This is indeed too
often the case of earthquakes, but that is a
partial degree, not at all equivalent to the compass
of the shock; and is very far from being
the constant concomitant of an earthquake.
Quite the contrary. Innumerable such happen,
when there is no breach of the surface;
and of these three or four which we have now
felt, nothing of it has appear'd. But the immensity
of the vibration of the earth which
shook every house in London, with impunity,
and for twenty miles round, can never, in my
apprehension, be owing to so unbridled a cause,
as any subterraneous vapours, fermentations,
rarefactions, and the like; the vulgar solution.
Nor does the kind of motion, which I discern
in an earthquake, in any sort agree with what
we should expect from explosions.
In order then to proceed with some degree
of certainty, in our inquiry after the cause of
earthquakes, it will be useful, in the first place,
to set in one view, the general appearances remarkable
therein; the most usual concomitants:
As we can collect them from our own
observation, or from the relations and writings
of others.
Circumstances.
I. That earthquakes always happen in calm
seasons, in warm, dry, sultry weather; or after
a dry, frosty air.
II. That they are felt at sea, as well as land,
even in the main ocean; and at that time, the
sea is calm.
III. That earthquakes differ very much in
magnitude. Some shake a very large tract of
country, at the same instant of time; nay, sometime
extend to very many countries, separated
by mountains, seas, lakes, the ocean.
IV. That earthquakes differ very much in
the quantity, of their vibratory motion: Whence
in some, tho' largely extended, they are innocuous;
in others, both small and great, they
lay all in ruin and destruction.
V. That a hollow, thundering, unusual
noise accompanies them, or rather seems to
preceed the shock; which rolls in the air like
the noise of cannon.
VI. That they are felt more sensibly in the
upper story of houses than in the lower.
VII. That the shock is more violent upon
more solid buildings, churches, castles, and
stone-houses, than upon those of slighter materials.
VIII. That many people find themselves
sick at stomach, with headake, and pains in
their joints, and the like, which sometime lasts
for the day after, or longer.
IX. That earthquakes generally happen to
great towns, and cities, and more particularly
to those that are situate on the sea.
X. That earthquakes do not cause any damage
to springs and fountains; but the water
in wells becomes foul for a short time.
XI. That they are more frequent in the
neighboring countries of a vulcano.
This last circumstance, in my opinion, has
led all inquirers in this question, out of the
true path; therefore I propose in the ensuing
paper.
I. To shew what it is not; the insufficiency
of the vulgar opinion, of subterraneous fires
and vapours.
II. To shew what it is in reality, as it appears
to me.
III. I shall conclude with the moral use we
ought to make of these prodigies of nature.
I. The struggles of subterraneous winds and
fires, that should heave up the ground like animal
convulsions, seem to me impossible: Their
powers, and manner of acting (if such there be)
is quite incapable of producing the appearance
of an earthquake. That these should
operate instantaneously, in one minute, thro'
a circle of 30 or 40 miles diameter, or more, I
could not conceive. Nor that there should be
any possible, much less ready passage thro' the
solid earth, for such nimble agents, as every
one is apt to imagine that speak of this appearance;
without sufficiently reflecting on the insuperable
difficulties in that hypothesis.
We cannot pretend to deny that there may
be such vapours, and fermentations, inflammable
substances, and actual fires, in the bowels
of the earth; and that there may be some
caverns under-ground, as well as we find some
few above ground: such as Pool's-Hole, The
Devil's-Arse in the Peak of Derbyshire, and
Okey-Hole in Somersetshire. These, I believe,
to have been so from the creation, never were
made by earthquakes. We know, there are
hot springs running continually: There are
some vulcano's frequently belching out flames
and smoke, and to these perhaps some earthquakes
may be owing, tho' not according to
the vulgar notion; as we shall see, by and by.
But these matters are very rare, much rarer
than earthquakes, both as to time and place.
Vesuvius in Italy, and in that part of it abounding
with mines of sulphur: Ætna in Sicily,
and Heckla in Iceland; these are all we know
of, in the old world. In the Andes mountains
of America, there are some. The scarcity of
these appears to me a strong argument against
the common deductions made therefrom, as
to their being the cause of earthquakes.
Nor can I enter into the sentiments of those
that hold the cavernous state of the earth, so
as to contribute to the forming an earthquake
by vapours running from place to place under
ground. How many thousand acres of coal-mines
do they daily work in England, and have done
for ages? I have been myself 2 or 300 feet deep
in a solid rock of native salt: I have walked a
mile lengthwise directly into the earth, and
descending all the way, in the proportion of
one yard in five, 'till we came under the bed of
the very ocean, where ships were sailing over
our heads. This was at Sir James Lowther's
coal-pit, at Whitehaven. We were at this
time deeper under ground by the perpendicular,
than any part of the ocean, between England
and Ireland.
We never hear, from the many hundreds
of thousands of workmen in this kind, at Newcastle,
Nottinghamshire, Yorkshire, Derbyshire,
Staffordshire, Somersetshire, and Wales: from
the infinite numbers of workmen in the mines
of lead, tin, and the like, of the cavernous state
of the earth, so as to give any colour for this
hypothesis of earthquakes. The earth is generally
of solid rock; in which there must be now,
and then, some clefts, and vacuities, small in
compass, as naturally so many heterogeneous
strata of the earth consolidate together. But
there can be no imagination of vapours breaking
through, uniting, traversing so suddenly, a
large space of earth, so as to produce those
earthquakes, we have seen, and felt; much less
such as we read of. The workmen in all sorts
of mines confess by their hard labor, that the
earth is not cavernous; nor are there mines of
sulphur, nitre, and the like inflammable materials
in England. Or if there were, could they
burn, and cause convulsions of the earth, without
proper cavities, pipes, and conveyances of
air; as vulcano's, and coal-pits, when set on
fire. But even from these coal-pits, when fired,
do we ever find any thing like an earthquake
produced. Nor do we find earthquakes frequent
in those countries, that abound with coal-mines,
as certainly would be the case, if that
hypothesis was just. How easy would it be, on
the slightest occasion for earthquakes to happen
in the countries abounding with coal-mines,
which are so full of artificial cavities communicating
with one another, for many miles
together: The very thing supposed, by those
who hold the old opinion, of vapours traversing
the earth for that purpose.
In the coal-pits, some small natural cavities
now and then are found; which when opened,
send forth a pestiferous vapor and a fire-damp
which runs for a long time together.
And tho' there are many substances that may
generate air, within the bowels of the earth;
yet these matters are infinitely unable to produce
an earthquake: Never would have force
to open a passage for themselves thro' the solid
rock, of perhaps many hundred feet in
thickness. Nor did we observe in these last
earthquakes any fire, vapour, smoke, or smell,
any kind of eruption, in the least; as must
certainly have been, in so great a struggle of
the superfice, as affected a circle of so large a
diameter. Were there such, we could scarce
hope any otherwise, than that they would be
too sensibly felt; to the destruction of many
thousands, by their pestiferous qualities.
Indeed this consideration alone, of the extent
of that surface, is sufficient to overthrow any
supposition, of earthquakes being chiefly owing
to subterraneous vapours: They cannot momentarily
fly under so large a tract of ground,
if they were near the outward shell of the earth.
They could not do it without breaking ground,
and discovering themselves to the sight, or
smell; and that for a long time after. It cannot
possibly be imagin'd, they could have so immense
a force, as to lift up the city of London,
and never be perceived by our organs, and outward
senses. We have frequent accounts of a
little fire-ball bursting in the air, at a distance;
yet it instantly propagates a sulphureous smell
around.
If the movement of a superficies of 30 miles
diameter was owing to fumes, and vapours;
we ought reasonably to find some great discharges
of them, belching out smoke and fire,
for a long time after, like vulcano's, and coal-pits
fir'd. The operation of the shock ought
to be of hours continuance, not instantaneous;
and the evaporation of so vast a quantity of
matter, must darken the whole region of the
air for a long time after; or require a long
time, if gradually it discharges itself. We see
how immense a volume of smoke is produc'd
by a very small quantity of gun-powder; and
no vapour could be so subtle, that produc'd
such effects, and not be very obvious to our
senses.
Even in vulcano's, it is the opinion of the
learned Italian philosopher Borelli, and of
other great naturalists, that they are kindled
first from the surface, where there is a possibility
of ventilation from the air. They
imagine, it begins at the top of the mountains;
not by any fancied fermentation of the pyrites
and sulphureous vapours arising from subterraneous
caverns, in the lower parts of
mountains.
There is another consideration, which utterly
overthrows these suppositions, of earthquakes
being caused by anything under-ground; and
that is a due consideration of springs, and fountains
perpetually flowing; and that from the
creation of the world to this day. If we would
form any tolerable idea of their nature, we
must needs conceive, that God Almighty has
laid their pipes, and canals in the earth, from a
great depth, even to the surface; like as he has
planted the veins, arteries, and glands in an
animal body. And likewise that they are more
and more ramify'd, as they nearer approach
the outward shell of the earth; just so our
veins, and arteries, as they come nearer the skin.
The workmen in coal-mines, and those of
metals, minerals, and stone-quarries, never fail
to meet with springs, and currents of water,
every where. Often they ruin, and divert
springs another way, only by digging into
the earth for foxes, and the like. Whenever
they dig for wells, in any kind of earth, they
commonly find springs. The colliers, and
workers of mines, are oblig'd to drain the
waters off with very great expence.
These are circumstances not favorable to
subterraneous fires being in the earth in abundance;
much less to their being the cause of
earthquakes. And further, we cannot possibly
think of earthquakes doing their work
that way, without absolutely ruining the
whole system of springs, and fountains,
throughout the whole country, where they
pass. But all this is quite contrary to fact;
even where an earthquake has been repeatedly.
For an instance from home.
On Wednesday, April 6, 1580, about six
in the evening, just such another earthquake
was felt in London and around it, as these
two we have seen. Another exactly similar
1692. In all these four, no houses thrown
down, no springs disturb'd thereby, no sensible
eruptions nor smells.
These considerations I apply only to this
little inconsiderable space, of a circle 30 miles
diameter; as with us. But what is that to
the earthquakes we read of in history? In
the year of our Lord 17, no less than thirteen
great and noble cities in Asia minor, were destroyed
in one night. Tacitus, Pliny, and many
other authors mention it. The fact is so notorious,
that some persons here present, have seen a
vast block of white marble now standing near
Naples; being the pedestal of a coloss statue
of Tiberius the emperor; having carv'd on it
the genius's, or pictures of all those cities,
with their names. The accurate Bulifon and
others have wrote treatises upon it. These
cities were rebuilt by that emperor. But
without going so far, we may see another
evidence of it, a coin of that emperor struck
upon the occasion, with this inscription,
CIVITATIBUS ASIAE RESTITUTIS.
I have one of them, in large brass, which
was found at Colchester.
The compass of this earthquake may be
reckon'd to take up 300 miles diameter, as
a circle. Now, we cannot conceive, how
any subterraneous vapour can produce such an
effect, as instantaneously to demolish all these
cities; and that such an accident should never
happen after. That the whole country of
Asia minor should not at the same time be
destroy'd, its mountains be renversed, its
fountains, springs, and rivers broken up and
ruin'd for ever. Instead whereof we find nothing
suffered, but those cities; no kind of
alteration in the surface of the country; it remains
the same as it were in the beginning
of time. In 1586 an earthquake in Peru,
that extended 900 miles.
From these considerations, I cannot persuade
myself, to enter into the opinion of vapours,
and eruptions being the cause sought
for; and, after we have treated the argument
in a superficial view, we must go a little
deeper.
If we would consider things like philosophers,
let us propose to ourselves this problem: Where
is the power to be plac'd, that is requir'd to
move a surface of earth 30 miles in diameter?
To answer this, consult the ingineers, and
those that make mines in the sieges of towns;
they will acquaint us, that the effect of mines
is produced in form of an inverted cone. And
that a diameter of 30 miles, in the base, will
require an axis of 15 or 20 miles to operate
upon that base, so as to shake it, at least.
Now the vapours, or whatever power we
propose to operate, according to the foregoing
requisite, in order to form the appearance
of an earthquake, must be 15 or 20 miles
deep in the earth. But what mind can conceive,
that any natural power is able to move
an inverted cone of solid earth, whose base is
30 miles diameter, whose axis 20? or was
it possible; would not the whole texture of
that body of earth be quite disturb'd and shatter'd,
especially in regard to its springs and
fountains? but nothing like this is ever found
to be the consequence of an earthquake, tho'
fatal to cities.
Apply this reasoning to the earthquake of
Asia minor, and this vigorous principle at the
apex of the cone must lie, at least, 200 Miles
deep in the ground. Enough to show the absurdity
of any moving power plac'd under the
Earth! A cone of 300 miles diameter at
base, 200 miles axis: I dare be bold to say,
that all the gun-powder made since its invention,
if put together and fired, would not be able
to move it; how much less pent up vapours?
what must we say of a circle of 900 miles
diameter?
But, could that be admitted as possible,
would any one be persuaded, that such a subterraneous
tumult, of so vast an extent, will
be no ways injurious to the internal system of
springs and fountains, and that this shall often
be repeated without the least damage? We
may as well imagine, that we can stab a man
100 times and never touch vein or artery.
Since I gave in my two papers to the Royal
Society, a letter of Mr. Flamsted's has been
printed, which abundantly confirms my sentiments.
The whole drift of it is, to show
how invalid is the vulgar idea conceiv'd, of
earthquakes arising from subterraneous vapours
and eruptions: That the earth itself is not
moved to any depth, and that the shock must
arise from the atmosphere. The circumstances
which he has judiciously collected, are extremely
agreeable to mine; many of them
the very same, strongly confirming my hypothesis:
And had that great man known the
properties of electricity, which we are now
masters of, he would have prevented me in
this affair.
"Considering (says he) what variety of
substances, sand, gravel, stones, rock, minerals,
clay, and mold, our earth is compounded
of, and how little nitre, or explosive
matter, a large quantity thereof will
afford; I cannot think, where we can
find matter enough to move so vast a bulk
of earth, as all the South parts of England,
all the Netherlands, with part of
Germany, all France, and perhaps Italy,
(which were shock'd at once the 8th of
September last 1692;) or part of Asia, and
near all Europe, which trembled together
the same day, 91 years before.
"But, allowing there may have been sufficient
matter prepared for these purposes,
I can hardly think, there are continued cavities,
at any reasonable depth, all under
Europe, wherein an explosion being made,
might shake the whole at once, and yet
make no clefts, or separations, in those
parts where the minerals and mountainous
rocks part from the light mold and clay.
If an hundred barrels of gun-powder could
be fixed in some cave, a thousand yards
under ground; allowing the force of the
explosion sufficient to raise all the weight
of earth incumbent on the cavern; it
would certainly break the loose mold
from any large solid rock we may conceive
adjacent, and leave at least some clefts behind
it. But we seldom or never hear of
such clefts, made in such places, when
earthquakes happen."
Again, he writes thus: "I cannot apprehend,
(if all earthquakes must be made by
explosions in subterraneous caverns) why
sometimes a large country, or whole continent,
should be thereby shook all at once;
why there should be no eruptions in the
neighbourhood?"
From all circumstances consider'd, he concludes,
that the abstruse, effective cause of
them comes from the air; and that a calm is
necessary before an earthquake. And these
two particulars are likewise Dr. Hales's positions:
"The earth-lightning, as he calls it,
is first kindled on the surface, and not at
great depths, as has been thought; whose
explosion is the immediate cause of an
earthquake. He says, long, dry, hot seasons,
are usually the preparatory forerunners
of earthquakes." From all these considerations
I conclude; earthquakes are not
caus'd by subterraneous vapors.
II. We are to inquire, what is the cause of
earthquakes.
In an age when electricity has been so
much our entertainment, and our amazement;
when we are become so well acquainted
with its stupendous powers and properties,
its velocity, and instantaneous operation
through any given distance; when we see,
upon a touch, or an approach, between a
non-electric and an electrified body, what a
wonderful vibration is produc'd! what a snap
it gives! how an innocuous flame breaks
forth! how violent a shock! Is it to be wonder'd
at, that hither we turn our thoughts, for
the solution of the prodigious appearance of
an earthquake?
Here is at once an assemblage of all those
properties and circumstances which we so
often see in courses of electricity. Electricity
may be call'd a sort of soul to matter,
thought to be an ethereal fire pervading all
things; and acting instantaneously, where,
and as far as it is excited. 'Tis every body's
observation, that there never was a winter,
like the last past, in any one's memory, so
extremely remarkable for warmth and driness,
abounding with thunder and lightning,
very uncommon in winter; coruscations in
the air frequent, justly thought electrical by
all philosophers; particularly, twice we had
the extraordinary appearance of that called
aurora australis, with colours altogether unusual;
and this just before the first earthquake:
All the while the wind constantly
south and south-west, and that without rain,
which is unusual with these winds.
This state of the atmosphere had continued
five months before the first earthquake. Is it
not hence reasonable to conclude, that the
earth, especially in our region, must be
brought into an unusual state of electricity;
into that vibratory condition wherein electricity
consists; and, consequently, nothing was
wanting but the approach of a non-electric
body, to produce that snap, and that shock,
which we call an earthquake; a vibration of
the superficies of the earth.
That the earth was in that vibratory and
electric state we have further reason to conclude,
from the very extraordinary forwardness
of all the vegetable world with us.
Every one knows, that, at the end of February,
all sorts of garden-stuff, trees, fruits,
and flowers, were as forward as in other years,
by the middle of April. Conformable to
which, experiments abundantly show, that
electrifying of plants quickens their growth,
equally as in animals it quickens the pulse.
Nor will the unusual driness and warmth of
the weather solely account for such a precipitate
vegetation: because a necessary supply of
rain was wanting, as in the natural Spring-season.
A very long dry frost will produce the
same electrical state of the earth, as it equally
favours electrical experiments. Thus,
March 27, 1076, a frost from the 1st of
November to the middle of April, a general
earthquake in England succeeded. Matt. Paris.
That of Oxford, 17th of September
1683, was after a frost. Jan. 4, 1680, An
earthquake in Somersetshire: The air was very
calm; a frosty night.
Mr. Flamsted concurs with us, in our first
position, That earthquakes always happen in
calm seasons. He adds, "That Keckerman,
a learned author, who wrote on the subject,
affirms, and backs it from the authority
of Aristotle and Pliny."
The 8th of September 1601 was a very
calm day but cloudy: And the Smyrna merchants
observe the earthquakes there happen
in calm, still weather. The remarkable clearness
and calmness of the morning was observed
in that of Oxford 17th of September
1683, and the air continued so for five or six
days after: Therefore we may infer, that it
is not impossible, what has been abundantly
related, that some foreigners from Italy here
in England, some from the West-Indies (in
both which countries earthquakes are more
frequent than with us) did seem to apprehend
our first earthquakes from the apparent temper
of the weather; and observations of this
kind are as old as Aristotle. It is observed
in Jamaica, when the air is extraordinary
calm, an earthquake is always apprehended.
We had lately read at the Royal Society,
a very curious discourse, from Mr. Franklin
of Philadelphia, concerning thundergusts,
lightning, the northern lights, and meteors.
All which he rightly solves from the
doctrine of electricity. For, if a cloud raised
from the sea, which is a non-electric, happens
to touch a cloud raised from exhalations
of the land, when electrified, it must immediately
cause thunder and lightning. The
electrical fire flowing from the touch of perhaps
a thousand miles compass of clouds,
makes that appearance, which we call lightning.
The snap which we hear in our electrical
experiments, when re-echoed from
cloud to cloud, the extent of the firmament,
makes that affrightning sound of thunder.
From the same principle I infer, that, if a
non-electric cloud discharges its contents upon
any part of the earth, when in a high electrified
state, an earthquake must necessarily
ensue. The ship made upon the contact of
many miles compass of solid earth is that
horrible uncouth noise, which we hear upon
an earthquake; and the shock is the earthquake
itself.
In the relation received from Portsmouth,
and the Isle of Wight, concerning the last
shock there, on the 18th of March, the writer
observes, the Day was warm and serene;
but, upon a gentle shower falling in the evening,
the earthquake came. Here we have
reason to apprehend the electrified state of the
earth, and the touch of the non-electric:
which caused the earthquake.
The learned Dr. Childrey observes, treating
on this subject, that earthquakes happen
upon rain; a sudden shower of rain in the
time of a great drought.
'Tis objected, that, if this was the case,
nothing would be more frequent than earthquakes;
but these two circumstances concurring,
a shower and dry weather, must not
necessarily cause it, any more than touching
a tube before it is electrified causes a snap.
The earth must be in a proper electrified state
to produce it; and electricity has its fits; is
remitted, intended, ceased and recommenced.
It has its bounds. All causes must concur.
And now, with us, all necessary causes did
so apparently. Tho' a shower of rain falling
upon the earth when electrified, may cause
an earthquake, yet too much rain before, will
prevent that state of electricity, necessary.
The day before the catastrophe of Port-Royal,
the weather was remarkably serene and
clear. In that most dreadful earthquake, 1692,
of Sicily, where 54 cities and towns, beside a
great number of villages were destroy'd; but
especially the whole city of Catania: It was
preceded by a most agreeable, serene and warm
season, which was the more observable on account
of its being unusual at that time of the
year.
I have been inform'd, that in the morning
of both earthquakes last past with us, the air
was serene and calm; on the morning before
that 8th of February, the air was observ'd to
be remarkably calm; and that a little before,
a black cloud appear'd over great part of the
horizon. Dr. Hales, in his relation, says, the
Centinels in St. James's Park, and others who
were abroad in the morning of the last earthquake,
observ'd a large black cloud, and some
coruscations, just before the shock, and that it
was very calm weather: And that, in the history
of earthquakes, they generally begin in
calm weather, with a black cloud.
This observation precludes the suspicion of
earthquakes arising from tumults and commotions
in the upper, or under region of the
air. The remarkable clearness of the air before
earthquakes, observ'd by all, shows evidently
how free it is from vapours and the like.
Agreeable to our fifth position, Mr. Flamsted
writes, "A hollow noise in the air always
precedes an earthquake, so near that
it rather seems to accompany them. He
refers us to Philosophical Transactions, No
151. p. 311. The noise was heard by
many that liv'd in the out-streets, and alleys
of London, remote from the noise and
tumult of the greater streets."
This he speaks of that felt in London 1692;
but now the whole city heard the noise, on
both these earthquakes of ours.
The gardener, who gave a relation to the
Royal Society of what he observed in the
Temple-garden, took notice, that first he heard
the most dreadful noise imaginable, which he
thought to be a great discharge of ship-guns,
on the river: and that the noise rolled from
the water-side towards Temple-bar, rather before
the nodding of the houses.
The gentleman who observed it about Hartingfordbury,
says, the noise preceded the
shock. And this is a common observation,
which at once both strengthens our opinion of
electricity, and confutes that of subterraneous
vapours; for, in the latter case, the concussion
must precede the noise.
Agreeable to out second position, Mr. Flamsted
writes, "That earthquakes are felt at
sea, equally as on land. Our merchants
say, that, tho' the water in the bay of
Smyrna lies level and smooth as a pond;
yet ships riding there feel the shocks very
sensibly, but in a very different manner
from the houses at land: For they heave
not, but tremble; their masts shiver, as if
they would fall to pieces and their guns
start in their carriages, though the surface of
the sea lies all the time calm and unmoved."
In Dr. Hook's Philosophical Collections, No 6.
p. 185. we are told, "That a ship felt a
shock in the main ocean; that the passengers,
who had been asleep in their cabins,
came upon deck in a fright, fearing the
ship had struck upon some rock; but, on
heaving the lead, found themselves out of
soundings."
All this is extremely agreeable to our assumption.
The water receives the electrical
touch, and vibratory intestine motion of its
parts, as well as land. And the impression
may be made solely on the writer a non-electric,
by the touch of an electric fire-ball, or
the like; and that seems to have been often
the care. The proper vibratory motion is
impress'd on the water without ruffling its
surface; and so communicated to all the parts
of the ship, gives the sense of a shock to the
bottom, the shivering to the mast, and the
rest of the symptoms: which sufficiently proclaim
the cause of it to be an electrical impression
upon the water. The president mentioned
a relation of a waterman, that felt it
in his boat upon the river; he thought it like
a great thump at the bottom of the boat.
And so the ships at sea fancy, they strike upon
a rock.
This makes us apprehend, the reason of
the fishes leaping up out of the canal in Southwark,
of which we had an account. So in
that of Oxford, 1683, one fishing in the
Charwell felt his boat tremble under him, and
the lesser fishes seem'd affrighted by an unusual
skipping. That electricity is the cause
sought for, seems deducible from this consideration.
Several writers on earthquakes assimilate
these vibrations of the earth to those
of a musical string. Experiments have shown,
that fishes in water may be killed by the particular
tone of a musical string; and 'tis
known, that electricity will kill animals. They
assuredly felt the vibratory motion in the water,
which they were absolutely strangers to
before. No doubt it made them sick; as
those of weak nerves on land. And this circumstance
alone precludes any suspicion of
subterraneous fires under the ocean. Or, if
we were to admit of it, would the boiling of
the water exhibit any appearance, like what
we are speaking of, either to the water, or to
the ship?
Mr. Flamsted likewise concurs in our eighth
position, "That many people found themselves
suddenly sick at stomach, and their
heads dizzy and light; so that those that had
formerly fits of apoplexies, dreaded their
return; particularly, one gentleman, a surgeon,
feeling himself so affected, and fearing
a return of his apoplexy, resolved to
be let blood, without suspecting the earthquake."
After these two shocks which we felt, many
people had pains in their joints and back, as
after electrifying; many had sickness, headakes,
hysteric and nervous disorders, and
colicks, for the whole day after, and some
much longer, especially people of weak
nerves, weak constitutions; some women
miscarry'd upon it; to some it has prov'd
fatal.
To this we must attribute, that relation we
had, of the dog lying asleep before the fire;
but upon the earthquake, he suddenly rose
up, run about the room, whining, and endeavouring
to get out.
Any solid matter is capable of being put
into a state or electricity, such as iron guns;
and the more so, by reason of their solidity.
And in proportion to it, is the greatness of
the snap, and of the shock; and a kind of
lambent flame issues from the point of contact;
and likewise somewhat of a sulphureous
smell: So that if both flame and smell were
discernible in an earthquake; 'tis to be found,
without going to the bowels of the earth.
Dr. Hales mentions, that solid bodies are
the best conductors of aereal lightning; whence
oaks are rent, and iron melted. And in
our earthquakes in London, the loudest noise
was heard near such large stone buildings, as
churches, with lofty steeples. From the top
of these we must apprehend, that the electrical
explosion goes off into the open air; as
in our experiments, from the point of swords,
and the like.
The electrical shock is proportionate to the
solid electrified, agreeable to our seventh position.
This fully accounts for earthquakes in
general, and for many in particular. What
can be imagin'd greater than a shock of the
body of the earth? 'Tis greater, or less in
proportion to the state of electrification. And
now we can account for several appearances.
In the first earthquake, the Lord Chancellor,
Masters in Chancery, and several Judges, were
sitting in Westminster-Hall, with their backs
to the wall of the upper-end, which is of a
vast thickness. They all relate the severity of
the shock, from the wall seeming to push towards
them with great violence.
And thus in the earthquake of 1692, Deal
castle is one of them built by Henry VIII.
the walls are of immense thickness, and
strength; yet they shook so sensibly, that the
people living in it, expected it was falling on
their heads. And this is the case in all earthquakes:
the more substantial the building, the
more violent is the shock: exactly the mode of
electrical vibration. And this Dr. Hales takes
notice of and others; that an earthquake shatters
rocks of marble, more easily than the
strata of sand, earth, or gravel. In the earthquake
here of 1692, a great cliff fell down
near Dover; and part of Saltwood-castle
wall.
'Tis from hence we account for that observation,
that when we electrify any person;
upon a touch, the pain and blow of the shock
is felt at the joints, the wrist, elbow, and
shoulder, for instance, more than in the intermediate
parts; because there is the greatest
quantity of solid.
At the same time, that the force of electricity
in solids, is as the quantity of matter:
we see most evidently, by innumerable experiments,
that water is equally assistant in
strengthening, and conveying the force of electricity;
and that in proportion too to its quantity.
And hence is to be deduc'd the reason
of my observation; that the most frequent
and dreadful earthquakes have fallen upon maritime
places. And I find the same is taken
notice of in some degree, by Acosta, by Dolittle,
who wrote on that in 1692, and others.
In the dreadful catastrophe at Port-Royal
then, 'tis notorious, that its violence was chiefly
near the sea. So Lima could not suffer without
its port of Callao. Even in those so lately
felt by us, they were sensibly more violent
towards the river, than farther from it.
In that earthquake which was felt in England,
in the year 1692, (which was very
much like these with us) there were no
houses thrown down, nor persons kill'd: but
it reach'd more particularly Sheerness, Sandwich,
Deal, Dover, Portsmouth, and the maritime
parts of Holland, Flanders, and Normandy.
In this that happened on Sunday the 18th
of March last, at Bath; it was felt particularly
and strongly at Portsmouth, seven miles
above and below it, on the sea-side; all round
the isle of Wight, at Southampton, the sea-coast
of Selsey, south of Chichester, Arundel,
and the whole coast of Sussex, without going
up the land; and across the sea to the islands
of Jersey and Guernsey.
On Monday night, the 2d of this instant
April, 1750, at ten o'clock, at Leverpool, a
shock of an earthquake. And felt in several
other places in the neighbourhood; but particularly
at Chester, and Warington.
If we look into ancient history, we find
197 years before Christ, an earthquake shook
terribly the isle of Rhodes, damag'd many
cities: and some quite swallow'd up.
Seventeen years before Christ, many cities
in the isle of Cyprus destroy'd.
Six years before Christ, the isle of Coos
vehemently afflicted.
During the Peloponnesian war among the
Greeks, the isle of Delos shaken, and the most
beautiful temple of Apollo thrown down.
Soon after, the city of Lacedæmon totally
destroy'd.
A. D. 79. Three cities in Cyprus overthrown.
A. D. 82. The city of Smyrna ruined.
In the time of Valens the emperor, a terrible
earthquake in Crete, whereby 100 cities
were destroy'd.
Feb. 13, 1247, An earthquake, chiefly felt
in the Thames. Matt. Paris.
May, 1382, A general earthquake, which
did much mischief; the Friday following one
less; the Saturday following, one felt mostly
by water. Henry de Knyhton. Holinshed.
A. D. 1456, In the city of Naples, 40,000
people lost.
Constantinople has often suffer'd; particularly
in 1509, 13,000 people overwhelm'd.
1531, At Lisbon, 1400 houses thrown
down; as many shatter'd.
April, 1690, The Leeward-Islands, Montserat,
Nevis, and Antigua: At Martinico,
and the French islands, at St. Lucia, &c. a
violent earthquake.
Dec. 8, 1703, An earthquake at Hull, a
perfect calm.
1702, At Stroution, in Argyleshire, which
extended all along the west coast of Great-Britain;
but to no breadth on land.
Oct. 25, 1734, At Havant, in Sussex, considerable,
the air perfectly calm.
But instances enough, to show what I
aim'd at, that maritime places are most subject;
which is a strong argument in favour of
electricity; when both the solid of the earth,
and the quantity of the water concur, to
make the shock; exactly as in electrical experiments;
when the bottle of water is held in
the hand.
Thus when our mind is discharged of the
prejudices of former notions, we discern,
that every appearance favours the principle we
go upon. That, agreeable to Mr. Flamsted,
subterraneous explosions, could they pervade,
and traverse the earth at pleasure, must at last
burst, and disperse every thing in their way.
Yet 'tis not possible for us to imagine, such
a kind of vibration should follow, either by
sea or land, as that we are treating of. But
electricity compleatly answers it. This accounts
for that superficial movement of the
earth, that universal instantaneous shock,
which made every house in London to tremble,
none to fall: That quivering, tremulous,
horizontal vibration, highly different from any
motion we must conceive, to be produc'd
from subterraneous evaporations. Hence authors
tell us, Dec. 30, 1739, describing an
earthquake in the west-riding of Yorkshire:
It seem'd as if the earth mov'd backward and
forward horizontally; a quivering, with reciprocal
vibrations.
Mr. Flamsted rightly accounts the motion
of earthquakes to be undulatory; and by being
continued, causes a like motion to a great
distance. As when you strike a long stretch'd
string of wire at one end, the motion is immediately
continued to the other. So far he
entered into the nature of electricity.
Tho' he be in the right, thinking the cause
comes from the air, yet what follows, contradicts
his own hypothesis. For if a calm be
necessary before an earthquake; then 'tis not
produc'd by any turbulence in the air. Nor
can we imagine that any aerial commotion,
tho' it may shake windows, chimneys, and
the like, shall reach 500 miles distance, split
the solid earth, destroy whole cities, and cause
those dire desolations we hear of.
Mr. Flamsted mentions a circumstance, that
the earthquake here in 1692, was not felt in
the north of England, nor in all Scotland:
for rain fell that day in both. We may very
readily conceive, the earth there was not in
an electrified state; and the rain would sufficiently
prevent it. We hence understand,
how the southern regions should be more subject
to them, than our northern; where the
warmth, and driness of the air, so necessary
to electricity, is more frequent than with
us.
From electric vibration only can we account
for our tenth position, of springs, and
fountains being no ways damag'd by earthquakes:
The motion goes no deeper into the
earth, than the force and quantity of the
shock reaches; which generally is not far;
yet it proceeds lower down when the ready
passage of a well offers, and there affects the
water contained in it; puts it into an intestine
vibration, as to foul it, and raise mud from
the bottom.
It may seem difficult to conceive, how a large
portion of the earth's surface should be thus
capable of electrification. This difficulty is
lessened by reflecting on the nature of electricity,
and of the electrical, ethereal fluid pervading
all things: how it is excited by the
little motion of a small revolving glass globe.
By this we electrify the most solid bodies, to
the greatest distance, and with a velocity equal
to that of lightning.
Dr. Hales observes, that the usual explosion
of the cannon on great days, in St. James's-Park,
is observ'd to electrify the glass, in the
windows of the Treasury.
We must conceive, that when the electric
shock is communicated to one part of the
earth, it extends itself proportionably to the
force of the shock, and to the quantity of
electrified surface; and to the quality of the
matter more or less susceptible of it, more or
less apt to propagate it.
Set 1000 men in a row; let every one
communicate with those next him by an iron-wire
held in their hands: on an electrical
shock they all feel it alike, at the same instant;
and this gives us a very good idea of
the earthquake.
When the earth is broken up in any large
degree, 'tis by the sea-side; where sometimes
on a bold shore, whole streets tumble into the
sea, or into the gaping earth, now falling toward
the sea. Sometimes on a flat and sandy
shore, whole streets are rolled along the level
into the sea.
I am not sensible of any real objection
against our hypothesis, but this, being the
eleventh of my positions, or circumstances.
It seems true, that earthquakes are more frequent
in Italy, near Vesuvius, and by Ætna,
in Sicily. And the cause seems apparently
owing to these vulcano's. At first sight, every
one would think so, but not from the true
reason. This has given the great prejudice to
the judgments of the curious, even at this
day. But consider the matter impartially, and
it will appear, so far from being a strong argument
in favour of subterraneous eruptions,
that it ought to be esteem'd a convincing proof
to the contrary, and most cogent in favour of
my principle. In strictest logic, there is no
inference to be made from particulars to generals.
Quite the contrary. We have but
these two or three vulcano's on one quarter
of the globe, and two of them toward the
warmer climate of it; whereas earthquakes
are innumerable, especially in those of a warmer
clime. That there are no vulcano's, no
discharges of fire and smoke for a continuance,
and abundance, after earthquakes; no suspicion
of it either from sight or smell, as we
know by innumerable examples, as well as in
our own country, and experience: is demonstration,
that this is not the cause. If
the vulcano's were the real cause of earthquakes,
we ought assuredly to expect, that in
the countries thereabouts, the earthquakes
ought to be far more extensive than those in
other countries, where are no vulcano's; but
this is altogether contrary to experience. For,
as the celebrated naturalist Buffon observes,
such are not extensive, as are near Ætna and
Vesuvius. He further adds: Histoire naturelle,
tom. I. p. 508. speaking, among many
others, of a vulcano in the island of Ternate,
he remarks, "That this burning gulph is less
agitated when the air is calm, and the season
mild, than in storms and hurricanes;"
and says, "This confirms what I have said in
my foregoing discourse, and seems evidently
to prove, that the fire which makes vulcano's
comes not from the bottom of mountains,
but from the tops, or at least from
a very little depth; and that the hearth (or
floor) of the fire is not far from the summit
of the vulcano's; for, if this was not
the case, great winds could not contribute
to their conflagration." And this, in general,
is a corroborative proof of my whole hypothesis.
For there can be no great fire in
the earth, where there is no great conveyance
of air.
We have one vulcano in the cold region of
Iceland, and there is sometimes an earthquake
there; but, in the countries of that northern
latitude, and those of lesser, 'tis obvious in
all history, that earthquakes are less frequent
than in the more southern. Therefore 'tis
easy, and very natural to conclude, from all
considerations weighed together, that these
vulcano's help to put the earth about them,
into that vibratory state and condition of electricity,
which is the requisite in my hypothesis,
and by that means only, promote a frequency
of earthquakes there.
I have only one circumstance to add, which
may seem not inconsiderable; probably perceived
by many, tho' not taken notice of.
For a whole week before the first earthquake,
the partition wainscot of my house (between
the forward and backward rooms) made an
odd kind of tremulous, crackling noise continually,
as if the wainscot would split; or
as if some damage was apprehended to the
house. This was observ'd by the family,
with a good deal of concern. That in the
chamber crackled more than that below. We
never perceiv'd it before, nor since; and apparently,
it shows the vibratory state of the
surface of the earth, at that time.
But whether our conjectures upon this important
subject be well founded or no, it certainly
becomes a christian philosopher, whilst
he is investigating material causes, to look
up, and regard the moral use of them. For
in reality, every thing, the whole world, was
ultimately for that purpose made. When
we see such a kind of spirituality impress'd
on mere matter, as this amazing property of
electricity, it should kindle in us a high ambition
of asserting, and exerting the infinitely
superior value, and powers, and excellency of
the spiritual part of us, destin'd to an immortal
duration. And of all the great and public
calamities, which affect us mortals, earthquakes
claim the first title to the name of
warnings and judgments. None so proper to
threaten, or to execute vengeance upon a
guilty people. Nor has any other, those annexed
terrors, so much of the unusual, the
unavoidable, the sudden and the horrible apprehension
of being crush'd to death, or buried
alive. And when in our own sight, these
rare and extraordinary phænomena appear, it
cannot but be a lesson to us, to do our duty
toward that great Being, who, by a drop of
water, can produce effects so prodigious.
That earthquakes proclaim themselves to
mankind in this light, is further deducible
from this observation, the ninth in our recapitulation
of circumstances; that they are peculiarly
directed to great cities, and maritime
towns, those nurseries of wealth, luxury, and
of all the evils naturally flowing therefrom.
It would be childish to rehearse from old history,
or modern, a proof of it. We have
no other notices of them. Look upon these
two shocks we have here felt. We own
that Hampsted-heath, and Finchley-forest, and
Kennington-common were affected with it;
yet it is notorious, that London was the center,
the place to which the finger of God was
pointed.
And this leads us in the third place, to
consider the moral use and purpose of these
magnalia naturæ, and prodigies of the agency
of material causes. For nothing sure, but
an electrical shock, and that from a divine
hand, could have been so well adjusted, as
twice, nay four times, so sensibly to shake
every house in London, and not throw one
down. This duty we will endeavour to execute,
from the words of that great man, king
David.