This is a table of type quadgram and their frequencies. Use it to search & browse the list to learn more about your study carrel.
quadgram | frequency |
---|---|
the surface of the | 192 |
the bottom of the | 102 |
in the form of | 85 |
in the case of | 78 |
in the course of | 77 |
the top of the | 76 |
the fact that the | 74 |
the temperature of the | 67 |
the level of the | 66 |
on the th of | 66 |
surface of the earth | 63 |
at the bottom of | 63 |
at the end of | 62 |
the floor of the | 59 |
the base of the | 55 |
the greater part of | 54 |
the entrance to the | 52 |
one of the most | 51 |
for the reason that | 50 |
at the same time | 50 |
at an altitude of | 50 |
the end of the | 48 |
the mouth of the | 47 |
at the foot of | 43 |
on the surface of | 43 |
the centre of the | 42 |
the case of the | 42 |
by the action of | 41 |
the action of the | 41 |
the sides of the | 39 |
described in part i | 38 |
the edge of the | 38 |
to the fact that | 37 |
the foot of the | 36 |
at the base of | 36 |
a large part of | 35 |
at the time of | 34 |
as well as the | 34 |
the course of the | 34 |
a part of the | 34 |
the side of the | 33 |
the interior of the | 33 |
from time to time | 33 |
on account of the | 33 |
a good deal of | 32 |
parts of the world | 32 |
in the middle of | 32 |
by the fact that | 32 |
of the cave is | 31 |
in the manner of | 31 |
that part of the | 31 |
greater part of the | 31 |
the history of the | 30 |
is said to be | 30 |
the height of the | 30 |
part of the cave | 30 |
the form of a | 30 |
at the top of | 30 |
to the depth of | 30 |
in the shape of | 30 |
end of the cave | 30 |
is due to the | 30 |
on the other side | 29 |
to be found in | 29 |
feet above the sea | 29 |
the beginning of the | 29 |
the face of the | 29 |
the nature of the | 28 |
the head of the | 28 |
the effect of the | 28 |
the roof of the | 28 |
large part of the | 28 |
is one of the | 28 |
in the history of | 28 |
the upper part of | 28 |
at the rate of | 27 |
in the centre of | 27 |
the middle of the | 27 |
above the level of | 27 |
it is easy to | 27 |
at a depth of | 27 |
the walls of the | 26 |
in the neighbourhood of | 26 |
on the other hand | 26 |
of one of the | 26 |
the waters of the | 26 |
for the most part | 26 |
in a state of | 25 |
from a photograph by | 25 |
as soon as the | 25 |
entrance to the cave | 25 |
the position of the | 25 |
at a distance of | 25 |
an altitude of meters | 24 |
the result is that | 24 |
the time of the | 24 |
in the first place | 24 |
on the top of | 23 |
the ice in the | 23 |
is found in the | 23 |
this part of the | 23 |
to a depth of | 23 |
a portion of the | 23 |
of the ice in | 23 |
the bottom of a | 23 |
in the midst of | 23 |
the end of a | 23 |
the part of the | 23 |
a great deal of | 22 |
an altitude of about | 22 |
the other side of | 22 |
it is probable that | 22 |
rays of the sun | 22 |
the direction of the | 22 |
the depth of the | 22 |
the depths of the | 22 |
the valley of the | 22 |
below the level of | 22 |
at an angle of | 22 |
upper part of the | 22 |
in one of the | 22 |
the shape of the | 22 |
due to the fact | 22 |
at the present time | 21 |
to the action of | 21 |
a certain amount of | 21 |
level of the sea | 21 |
the shape of a | 21 |
the movements of the | 20 |
at a height of | 20 |
floor of the cave | 20 |
ice is found in | 20 |
all parts of the | 20 |
as in the case | 20 |
the rest of the | 20 |
the length of the | 20 |
be found in the | 20 |
in the neighborhood of | 20 |
the heat of the | 20 |
american journal of science | 20 |
the entrance of the | 20 |
the reason that the | 20 |
to a great extent | 20 |
feet below the surface | 20 |
the cold of winter | 20 |
a hole in the | 19 |
of the solar system | 19 |
in connection with the | 19 |
in the state of | 19 |
on the side of | 19 |
that the ice in | 19 |
the fact that they | 19 |
the whole of the | 19 |
at the present day | 19 |
is said to have | 19 |
the formation of the | 19 |
to the end of | 19 |
other side of the | 19 |
the summit of the | 19 |
it is difficult to | 19 |
the movement of the | 19 |
a large amount of | 19 |
of science and arts | 18 |
of the earth is | 18 |
of the cave was | 18 |
journal of science and | 18 |
the water in the | 18 |
that there was no | 18 |
it is impossible to | 18 |
at right angles to | 18 |
to the conclusion that | 18 |
the mean temperature of | 18 |
the top of a | 18 |
that the ice is | 18 |
for a long time | 18 |
cold air of winter | 18 |
at the mouth of | 18 |
of some of the | 18 |
than that of the | 18 |
the lower part of | 18 |
the body of the | 18 |
mean temperature of the | 18 |
of ice in the | 17 |
the formation of ice | 17 |
the course of a | 17 |
it is evident that | 17 |
of the earth which | 17 |
there was no ice | 17 |
to the height of | 17 |
altitude of about meters | 17 |
as that of the | 17 |
the source of the | 17 |
to the bottom of | 17 |
bottom of the pit | 17 |
of the united states | 17 |
there can be no | 17 |
on the floor of | 17 |
parts of the earth | 17 |
different parts of the | 17 |
on either side of | 17 |
ice in the cave | 17 |
to a height of | 16 |
part of the year | 16 |
a depth of feet | 16 |
in a general way | 16 |
vertical section of the | 16 |
the neighbourhood of the | 16 |
said to have been | 16 |
the th of august | 16 |
of the formation of | 16 |
mouth of the cave | 16 |
lower part of the | 16 |
with regard to the | 16 |
as far as the | 16 |
in that part of | 16 |
the bed of the | 16 |
the way in which | 16 |
appears to have been | 16 |
its way to the | 16 |
in different parts of | 15 |
below the surface of | 15 |
the rays of the | 15 |
in the formation of | 15 |
and this for the | 15 |
some of the most | 15 |
it is said that | 15 |
at the head of | 15 |
roof of the cave | 15 |
right angles to the | 15 |
the line of the | 15 |
it is necessary to | 15 |
where there is a | 15 |
on the south side | 15 |
surface of the ground | 15 |
the character of the | 15 |
the edges of the | 15 |
the cold air of | 15 |
with the exception of | 15 |
the th of july | 15 |
parts of the cave | 15 |
from to feet high | 15 |
is to be found | 15 |
on the right hand | 15 |
to account for the | 14 |
the mouth of a | 14 |
in the same manner | 14 |
is easy to see | 14 |
i am inclined to | 14 |
brought about by the | 14 |
to the top of | 14 |
one hundred and fifty | 14 |
under the influence of | 14 |
the effect of this | 14 |
on account of its | 14 |
the side of a | 14 |
side of the cave | 14 |
either side of the | 14 |
the shores of the | 14 |
in this case the | 14 |
the cause of the | 14 |
and at the same | 14 |
the slope of the | 14 |
the bottom of which | 14 |
on the sides of | 14 |
to the formation of | 14 |
the appearance of a | 14 |
of water in the | 14 |
accounted for by the | 14 |
on the edge of | 14 |
in the valley of | 14 |
meters long and meters | 14 |
the fact that it | 14 |
in this part of | 14 |
on each side of | 14 |
of carbonate of lime | 14 |
the limits of the | 14 |
surface of the sea | 14 |
the heart of the | 13 |
the rocks of which | 13 |
a quarter of a | 13 |
the remains of the | 13 |
this for the reason | 13 |
the north side of | 13 |
that it is not | 13 |
are to be found | 13 |
the conditions of the | 13 |
formation of the ice | 13 |
in the direction of | 13 |
in the beginning of | 13 |
the gulf of mexico | 13 |
in contact with the | 13 |
of the existence of | 13 |
an angle of about | 13 |
that the ice was | 13 |
it will be seen | 13 |
a quarter of an | 13 |
as is the case | 13 |
of the most important | 13 |
feet above the level | 13 |
the point where the | 13 |
surface of the water | 13 |
in the fact that | 13 |
in course of time | 13 |
at the depth of | 13 |
a distance of feet | 13 |
it was impossible to | 13 |
can be no doubt | 13 |
that there was a | 13 |
the influence of the | 13 |
the name of the | 13 |
the hands of the | 13 |
in some of the | 13 |
the conclusion that the | 12 |
thousand feet above the | 12 |
i was obliged to | 12 |
to the point where | 12 |
of the lake of | 12 |
it often happens that | 12 |
noted the fact that | 12 |
the present state of | 12 |
surface of the ice | 12 |
the center of the | 12 |
are due to the | 12 |
from the surface of | 12 |
at the beginning of | 12 |
many parts of the | 12 |
in the bottom of | 12 |
in many parts of | 12 |
on the part of | 12 |
seems to have been | 12 |
the way to the | 12 |
temperature of the air | 12 |
portion of the cave | 12 |
be accounted for by | 12 |
the movements of air | 12 |
hour and a half | 12 |
from to feet wide | 12 |
at the height of | 12 |
and from to feet | 12 |
the action of water | 12 |
to have been the | 12 |
be due to the | 12 |
of one of these | 12 |
for the first time | 12 |
on the north side | 12 |
to suppose that the | 12 |
the old red sandstone | 12 |
the existence of the | 12 |
the air in the | 12 |
in the way of | 12 |
in consequence of the | 12 |
the size of the | 12 |
in the same way | 12 |
for the purpose of | 12 |
of the rocky mountains | 12 |
by means of a | 12 |
the weight of the | 12 |
the same time the | 12 |
part of the world | 12 |
of the water which | 12 |
so long as the | 12 |
that there is no | 12 |
the structure of the | 12 |
thousand feet or more | 11 |
note the fact that | 11 |
the people of the | 11 |
the depth of a | 11 |
from meters to meters | 11 |
to the cave is | 11 |
the lower end of | 11 |
the margin of the | 11 |
surface of the land | 11 |
to the surface of | 11 |
sides of the cave | 11 |
the junction of the | 11 |
their way to the | 11 |
the thermometer stood at | 11 |
in some parts of | 11 |
we have already noted | 11 |
of which they are | 11 |
as well as in | 11 |
for a considerable distance | 11 |
from the top of | 11 |
the mean annual temperature | 11 |
the fact that in | 11 |
the thickness of the | 11 |
of the earth are | 11 |
that portion of the | 11 |
a photograph by mr | 11 |
for a distance of | 11 |
an hour and a | 11 |
a visit to the | 11 |
it is in the | 11 |
of ice on the | 11 |
wookey hole photo by | 11 |
that is to say | 11 |
upon the surface of | 11 |
the realm of the | 11 |
north side of the | 11 |
from the fact that | 11 |
idea as to the | 11 |
of the earth and | 11 |
the ice is found | 11 |
interior of the earth | 11 |
a vast amount of | 11 |
the same manner as | 11 |
the mass of the | 11 |
we found that the | 11 |
annalen der physik und | 11 |
of the imperial cave | 11 |
of the surface of | 11 |
ice has been found | 11 |
are said to be | 11 |
in the interior of | 11 |
hole in the roof | 11 |
we were able to | 11 |
the form of the | 11 |
for the sake of | 11 |
the heat of summer | 11 |
in the northern hemisphere | 11 |
appear to have been | 11 |
the ice is formed | 11 |
the seat of the | 11 |
the time when the | 11 |
der physik und chemie | 11 |
the manner in which | 11 |
to the east of | 11 |
reason to believe that | 10 |
part of the earth | 10 |
the course of time | 10 |
near the surface of | 10 |
depths of the earth | 10 |
of the black hills | 10 |
the north and south | 10 |
we came to a | 10 |
from east to west | 10 |
the lake of geneva | 10 |
to show that the | 10 |
the path of the | 10 |
the point of view | 10 |
in proportion to the | 10 |
the fossil bone cave | 10 |
the same as that | 10 |
the banks of the | 10 |
from the point of | 10 |
of which we have | 10 |
the valley of reposoir | 10 |
the melting of the | 10 |
which the ice is | 10 |
the northern part of | 10 |
one side of the | 10 |
as compared with the | 10 |
have already noted the | 10 |
air next the surface | 10 |
it seems likely that | 10 |
time of the year | 10 |
above the surface of | 10 |
in the vicinity of | 10 |
quarter of an hour | 10 |
what is called the | 10 |
the existence of ice | 10 |
into the state of | 10 |
to the present day | 10 |
on the st of | 10 |
we have now to | 10 |
below the freezing point | 10 |
so far as we | 10 |
that it is the | 10 |
already noted the fact | 10 |
it is possible to | 10 |
the larger part of | 10 |
the val de travers | 10 |
in the time of | 10 |
the approach to the | 10 |
of the same material | 10 |
in various parts of | 10 |
some idea of the | 10 |
to the presence of | 10 |
the light of the | 10 |
hundred and fifty feet | 10 |
is about feet high | 10 |
part of the mountain | 10 |
heat of the sun | 10 |
to the amount of | 10 |
some parts of the | 10 |
in the hands of | 10 |
to the existence of | 10 |
bottom of the cave | 10 |
easy to see that | 10 |
the gem of the | 10 |
in the amount of | 9 |
the pressure of the | 9 |
the highlands of scotland | 9 |
inclined to think that | 9 |
is probable that the | 9 |
could not have been | 9 |
a state of thaw | 9 |
to the mouth of | 9 |
it comes about that | 9 |
be explained by the | 9 |
hundred feet above the | 9 |
the west coast of | 9 |
of the gulf stream | 9 |
it would have been | 9 |
the manner of a | 9 |
side of the pit | 9 |
it was possible to | 9 |
the presence of ice | 9 |
to the left is | 9 |
a short distance from | 9 |
the base of a | 9 |
in one or two | 9 |
a pool of water | 9 |
to the time of | 9 |
it may be said | 9 |
the elevation of the | 9 |
of animals and plants | 9 |
from the entrance to | 9 |
the exception of the | 9 |
hundred feet or more | 9 |
to that of the | 9 |
the direction in which | 9 |
the south side of | 9 |
we find that the | 9 |
the farther end of | 9 |
the foot of a | 9 |
that it was not | 9 |
the interstices of the | 9 |
the water of the | 9 |
structure of the ice | 9 |
water in the cave | 9 |
it is interesting to | 9 |
ice on the floor | 9 |
grand cave de montarquis | 9 |
are likely to be | 9 |
in spite of the | 9 |
temperature of the cave | 9 |
level of the entrance | 9 |
that the cold of | 9 |
of heat and cold | 9 |
near the top of | 9 |
to find that the | 9 |
by means of the | 9 |
in this way a | 9 |
finds its way to | 9 |
in the process of | 9 |
that the amount of | 9 |
not far from the | 9 |
from the mouth of | 9 |
the bay of naples | 9 |
the power of the | 9 |
and many of the | 9 |
the owner of the | 9 |
result is that the | 9 |
part of the water | 9 |
and there was no | 9 |
a large number of | 9 |
to the nature of | 9 |
a considerable amount of | 9 |
so far as the | 9 |
in which they were | 9 |
opposite side of the | 9 |
the current of air | 9 |
to be the case | 9 |
portions of the cave | 9 |
of the action of | 9 |
the nature of this | 9 |
that it is a | 9 |
at the distance of | 9 |
the neighborhood of the | 9 |
history of the earth | 9 |
movements of the air | 9 |
a height of feet | 9 |
the site of the | 9 |
mean annual temperature of | 9 |
how the mountains were | 9 |
to the conditions of | 9 |
that some of the | 9 |
in the open air | 9 |
from year to year | 9 |
of the most beautiful | 9 |
in the habit of | 9 |
of snow and ice | 9 |
the story of the | 9 |
to the effect that | 9 |
of the cave and | 9 |
way in which the | 9 |
the formation of a | 9 |
as one of the | 9 |
it seems to me | 9 |
from the centre of | 9 |
the opposite side of | 9 |
farther end of the | 9 |
every now and then | 9 |
set at an angle | 9 |
the close of the | 9 |
it was necessary to | 9 |
on the banks of | 9 |
of the interior of | 9 |
gem of the west | 9 |
which is said to | 9 |
of the ice which | 8 |
it is called the | 8 |
as far as i | 8 |
when we reached the | 8 |
to return to the | 8 |
the size of a | 8 |
beyond the limits of | 8 |
i was able to | 8 |
in the upper part | 8 |
recesses of the cave | 8 |
to be seen in | 8 |
the beauty of the | 8 |
the temperature in the | 8 |
there is also a | 8 |
one hundred and twenty | 8 |
the ways in which | 8 |
the result of the | 8 |
fact that in the | 8 |
the amount of ice | 8 |
height above the sea | 8 |
upper surface of the | 8 |
and that it was | 8 |
in almost all cases | 8 |
in the roof of | 8 |
and some of the | 8 |
the inhabitants of the | 8 |
quarter of a mile | 8 |
on the floors of | 8 |
in which they are | 8 |
the rocks of the | 8 |
in the depths of | 8 |
be regarded as a | 8 |
may be regarded as | 8 |
point of view of | 8 |
that the earth is | 8 |
on the opposite side | 8 |
of the rocks of | 8 |
to which it is | 8 |
at the back of | 8 |
greater part of these | 8 |
the course of his | 8 |
there is reason to | 8 |
the cave is about | 8 |
may be said to | 8 |
near the village of | 8 |
about feet from the | 8 |
in all parts of | 8 |
one end of the | 8 |
short distance from the | 8 |
other parts of the | 8 |
long and meters wide | 8 |
one of the largest | 8 |
into a series of | 8 |
causes of subterranean ice | 8 |
that they did not | 8 |
as we shall see | 8 |
the difference between the | 8 |
will be seen that | 8 |
is made up of | 8 |
the upper surface of | 8 |
to a distance of | 8 |
the th of january | 8 |
surface of the country | 8 |
a large quantity of | 8 |
have been subjected to | 8 |
the borders of the | 8 |
temperature of the rock | 8 |
the difference in the | 8 |
coast of south america | 8 |
it is true that | 8 |
from north to south | 8 |
the existence of a | 8 |
where ice is found | 8 |
the th of september | 8 |
photo by dawkes partridge | 8 |
to the ice floor | 8 |
a hundred feet or | 8 |
it is likely that | 8 |
in many of the | 8 |
some distance from the | 8 |
in the part of | 8 |
found ourselves in a | 8 |
have been able to | 8 |
the motion of the | 8 |
the midst of the | 8 |
of which it is | 8 |
and in some cases | 8 |
no doubt that the | 8 |
to the extent of | 8 |
after the manner of | 8 |
a distance of about | 8 |
we made our way | 8 |
quarters of an hour | 8 |
the floors of the | 8 |
a part of their | 8 |
the effects of the | 8 |
from the foot of | 8 |
the tops of the | 8 |
the edge of a | 8 |
under the name of | 8 |
air in the cave | 8 |
the energy of the | 8 |
was due to the | 8 |
the drainage of the | 8 |
over the surface of | 8 |
the floor is covered | 8 |
the left of the | 8 |
be seen in the | 8 |
is not difficult to | 8 |
that they have been | 8 |
what we may call | 8 |
high up in the | 8 |
the action of heat | 8 |
for a great distance | 8 |
in a few minutes | 8 |
to the left of | 8 |
a more or less | 8 |
to the floor of | 8 |
on a level with | 8 |
is apt to be | 8 |
was found to be | 8 |
this portion of the | 8 |
was to be found | 8 |
the cave is a | 8 |
the materials of which | 8 |
i found that the | 8 |
of two or three | 8 |
to the base of | 8 |
the heavy cold air | 8 |
the development of the | 8 |
the attraction of the | 8 |
the remains of a | 8 |
the whole of this | 8 |
floor is covered with | 8 |
to the state of | 8 |
the causes of subterranean | 8 |
has been found in | 8 |
in two or three | 8 |
a mass of ice | 8 |
the upper end of | 7 |
that there is a | 7 |
would seem to be | 7 |
the northern end of | 7 |
and in so doing | 7 |
with a number of | 7 |
a great part of | 7 |
of which has been | 7 |
about feet above the | 7 |
wall of the cave | 7 |
this is a very | 7 |
be one of the | 7 |
the study of the | 7 |
of the town of | 7 |
on the d of | 7 |
in some cases the | 7 |
at the time when | 7 |
to believe that the | 7 |
the peak of teneriffe | 7 |
the rear of the | 7 |
in the cave at | 7 |
has not yet been | 7 |
cause of the ice | 7 |
we arrived at the | 7 |
as those of the | 7 |
the roof of this | 7 |
two or three feet | 7 |
the case with the | 7 |
on the shores of | 7 |
the width of the | 7 |
for the fact that | 7 |
we came to the | 7 |
on one side and | 7 |
the reason that they | 7 |
the region of the | 7 |
a day or two | 7 |
the floor of which | 7 |
has been removed from | 7 |
it is in a | 7 |
that we could not | 7 |
the front of the | 7 |
may be said that | 7 |
small part of the | 7 |
each side of the | 7 |
on account of a | 7 |
to the point of | 7 |
the right hand side | 7 |
as has been said | 7 |
at the lowest point | 7 |
the ice of the | 7 |
we readily perceive that | 7 |
the back of the | 7 |
the grandeur of the | 7 |
is by no means | 7 |
at the close of | 7 |
it is characteristic of | 7 |
than those of the | 7 |
on the island of | 7 |
at the edge of | 7 |
is known as the | 7 |
two or three times | 7 |
at no great distance | 7 |
in the valleys of | 7 |
hanging from the roof | 7 |
the rocks in the | 7 |
of water from the | 7 |
an opening in the | 7 |
the same kind of | 7 |
but he did not | 7 |
at some distance from | 7 |
surface of the rock | 7 |
or near the surface | 7 |
lower end of the | 7 |
from the base of | 7 |
the time of his | 7 |
it is clear that | 7 |
the discovery of the | 7 |
drip from the roof | 7 |
in a way which | 7 |
in the heart of | 7 |
the use of the | 7 |
as we have noted | 7 |
to the right of | 7 |
the section of the | 7 |
at the far end | 7 |
as well as that | 7 |
the state of the | 7 |
to the entrance of | 7 |
that it was the | 7 |
on one of the | 7 |
they have not been | 7 |
is evident that the | 7 |
great part of the | 7 |
as a matter of | 7 |
it will be well | 7 |
by reason of the | 7 |
and found that the | 7 |
upper end of the | 7 |
is covered with a | 7 |
is brought about by | 7 |
there would be no | 7 |
the chief of the | 7 |
we found ourselves in | 7 |
the cave at the | 7 |
the recesses of the | 7 |
the ice on the | 7 |
due to the action | 7 |
floor of the cavern | 7 |
by far the most | 7 |
a drop of water | 7 |
the reason for this | 7 |
for the formation of | 7 |
be no doubt that | 7 |
the commencement of the | 7 |
which lead to the | 7 |
of a hundred feet | 7 |
are more or less | 7 |
giant of the valley | 7 |
the central portion of | 7 |
on the bottom of | 7 |
it is well to | 7 |
on the borders of | 7 |
from the bottom of | 7 |
is that of a | 7 |
where there are no | 7 |
the cave in the | 7 |
the amount of the | 7 |
proved to be a | 7 |
in the days of | 7 |
the snow and ice | 7 |
that it has been | 7 |
are to be seen | 7 |
the light of day | 7 |
with a view to | 7 |
tens of thousands of | 7 |
as if they were | 7 |
the fact that when | 7 |
the rate at which | 7 |
a couple of meters | 7 |
told us that the | 7 |
end of the cavern | 7 |
hole photo by bamforth | 7 |
about yards from the | 7 |
of winter is the | 7 |
the origin of the | 7 |
know something of the | 7 |
along the line of | 7 |
feet from the floor | 7 |
in front of the | 7 |
branch of the imperial | 7 |
of the stalactites are | 7 |
by the heat of | 7 |
came to an end | 7 |
as long as the | 7 |
and in a few | 7 |
in the production of | 7 |
of the fact that | 7 |
the rate of about | 7 |
with the assistance of | 7 |
at the entrance to | 7 |
of which mountains are | 7 |
the decay of the | 7 |
the slopes of the | 7 |
the wall of the | 7 |
the atmosphere of the | 7 |
the removal of the | 7 |
may be divided into | 7 |
seasons of the year | 7 |
from the roof and | 7 |
to the edge of | 7 |
the first of these | 7 |
at or near the | 7 |
bottom of the sea | 7 |
the earth and the | 7 |
near the mouth of | 7 |
a considerable part of | 7 |
which it is composed | 7 |
of the rock in | 7 |
from the depths of | 7 |
of the coast line | 7 |
of the cold air | 7 |
of the valley of | 7 |
takes place in the | 7 |
to a considerable depth | 7 |
not been able to | 7 |
inclined to believe that | 7 |
in the summer of | 7 |
to the north of | 7 |
as well as to | 7 |
the midst of a | 7 |
are said to have | 7 |
to the summit of | 7 |
hand branch of the | 7 |
through which the water | 7 |
that the cold air | 7 |
was one of the | 7 |
about feet by feet | 7 |
a level with the | 7 |
same manner as the | 7 |
that the cave was | 7 |
we could not see | 7 |
the entrance to which | 7 |
it seems to be | 7 |
a very long time | 7 |
in the summer season | 7 |
on the sea floor | 7 |
in the immediate vicinity | 7 |
the passage of the | 7 |
taken up by the | 7 |
on the lake of | 7 |
the case of a | 7 |
a current of air | 7 |
of a number of | 7 |
that the temperature of | 7 |
in which it is | 7 |
the wall of rock | 7 |
in the cave was | 6 |
by virtue of the | 6 |
entrance of the cave | 6 |
the plane of the | 6 |
the point where it | 6 |
four or five meters | 6 |
in a manner which | 6 |
a mile and a | 6 |
at a lower level | 6 |
is connected with the | 6 |
so far as it | 6 |
for a short time | 6 |
the cave is meters | 6 |
face of the earth | 6 |
the range of the | 6 |
at the moment of | 6 |
the seat of a | 6 |
to be one of | 6 |
of the mont parmelan | 6 |
it is a curious | 6 |
about the formation of | 6 |
we may say that | 6 |
as the result of | 6 |
had been in the | 6 |
the manner of the | 6 |
of the bay of | 6 |
but there is a | 6 |
hole in the ice | 6 |
are found in the | 6 |
that one of the | 6 |
in our own country | 6 |
of a series of | 6 |
up to the surface | 6 |
here and there on | 6 |
the highest point of | 6 |
on the way to | 6 |
in times of heavy | 6 |
we find in the | 6 |
section of the cave | 6 |
two and a half | 6 |
which have been made | 6 |
and much of the | 6 |
of a thousand feet | 6 |
of the sun and | 6 |
the end of this | 6 |
that there was nothing | 6 |
the form of ice | 6 |
when we came to | 6 |
cave is in the | 6 |
one of them is | 6 |
with a mass of | 6 |
only a few of | 6 |
the reason that it | 6 |
are found to be | 6 |
may be considered as | 6 |
northern end of the | 6 |
down to the bottom | 6 |
on the floor are | 6 |
temperature in the cave | 6 |
way to the surface | 6 |
when the sun is | 6 |
the records of the | 6 |
in the light of | 6 |
in all cases the | 6 |
for the uses of | 6 |
which are in the | 6 |
that he had been | 6 |
in the character of | 6 |
the direct rays of | 6 |
it is one of | 6 |
from the village of | 6 |
the more ice is | 6 |
is proved by the | 6 |
taking place in the | 6 |
of the cave are | 6 |
a small part of | 6 |
along the coast line | 6 |
is no doubt that | 6 |
would be difficult to | 6 |
the height of a | 6 |
to a considerable height | 6 |
the southern part of | 6 |
of the earth in | 6 |
is to be seen | 6 |
and at the end | 6 |
where there was a | 6 |
is from to feet | 6 |
ice is formed in | 6 |
on the north slope | 6 |
as the cause of | 6 |
in the val de | 6 |
a photograph by j | 6 |
the appearance of the | 6 |
a thin coating of | 6 |
by means of which | 6 |
the floor of ice | 6 |
and the amount of | 6 |
was to be seen | 6 |
to be called a | 6 |
the lake of thun | 6 |
some of the stalactites | 6 |
two hours and a | 6 |
for a man to | 6 |
above the freezing point | 6 |
was in a state | 6 |
top of the hill | 6 |
of the jenolan caves | 6 |
on hands and knees | 6 |
which must have been | 6 |
is a curious fact | 6 |
feet from the entrance | 6 |
the lowest point of | 6 |
carried away by the | 6 |
the mass of ice | 6 |
parts of the alps | 6 |
every part of the | 6 |
on the roof and | 6 |
of air contained in | 6 |
on the point of | 6 |
we returned to the | 6 |
should expect to find | 6 |
the operations of nature | 6 |
the result of this | 6 |
interior of the mountain | 6 |
cavern photo by e | 6 |
water which has been | 6 |
effect of this action | 6 |
in toward the centre | 6 |
in part to the | 6 |
beyond the fact that | 6 |
of the opinion that | 6 |
called my attention to | 6 |
the middle of a | 6 |
crust of the earth | 6 |
in order to reach | 6 |
near the summit of | 6 |
those parts of the | 6 |
of the armenian church | 6 |
more than a few | 6 |
been the seat of | 6 |
from the point where | 6 |
top of the entrance | 6 |
in the realm of | 6 |
found in the cave | 6 |
of the most interesting | 6 |
of the stratified rocks | 6 |
been found in the | 6 |
where there is no | 6 |
to the foot of | 6 |
is the cause of | 6 |
it is possible that | 6 |
the pores of the | 6 |
that the earth was | 6 |
i have not been | 6 |
side of the valley | 6 |
in such a manner | 6 |
come in contact with | 6 |
on the northern side | 6 |
the flanks of the | 6 |
one of these was | 6 |
of thousands of feet | 6 |
of the whole earth | 6 |
so fortunate as to | 6 |
the cave is in | 6 |
have been discovered in | 6 |
the water at the | 6 |
one part of the | 6 |
as far as possible | 6 |
for the time being | 6 |
a great number of | 6 |
as large as the | 6 |
with a height of | 6 |
the extent of the | 6 |
feet higher than the | 6 |
amount of solid matter | 6 |
died in the year | 6 |
as soon as it | 6 |
it was in the | 6 |
the parts of the | 6 |
is probably due to | 6 |
from sketch by h | 6 |
a depth of about | 6 |
depth below the surface | 6 |
the course of ages | 6 |
of the floor of | 6 |
in the wall of | 6 |
mile and a half | 6 |
of the church of | 6 |
it lies on the | 6 |
and that the ice | 6 |
like that of the | 6 |
with which it is | 6 |
which the caves are | 6 |
only here and there | 6 |
story of the hills | 6 |
the earth in the | 6 |
the amount of rock | 6 |
the lower parts of | 6 |
there is no ice | 6 |
to the south of | 6 |
told me that he | 6 |
larger part of the | 6 |
but it is not | 6 |
below the snow line | 6 |
manners and customs of | 6 |
quarters of a mile | 6 |
of the water is | 6 |
in other parts of | 6 |
the air next the | 6 |
is about feet by | 6 |
it would be very | 6 |
some part of the | 6 |
for the distance of | 6 |
to be accounted for | 6 |
through which it passes | 6 |
the fissures of the | 6 |
the eastern side of | 6 |
seem to have been | 6 |
direct rays of the | 6 |
the place where the | 6 |
our own solar system | 6 |
the farther side of | 6 |
the crust of the | 6 |
time of my visit | 6 |
take place in the | 6 |
than that which is | 6 |
to do with the | 6 |
from end to end | 6 |
of the ice is | 6 |
action of the waves | 6 |
am inclined to think | 6 |
there is no doubt | 6 |
along the side of | 6 |
near to it is | 6 |
is reason to believe | 6 |
in the depth of | 6 |
on the peak of | 6 |
the force of the | 6 |
in regions where the | 6 |
met with in the | 6 |
a foot or more | 6 |
lowest point of the | 6 |
is afforded by the | 6 |
the roof to the | 6 |
the curves of the | 6 |
on one side of | 6 |
or in other words | 6 |
times as great as | 6 |
of the water in | 6 |
we note that the | 6 |
of the turkish empire | 6 |
the circuit of the | 6 |
took place in the | 6 |
height of more than | 6 |
the poles of the | 6 |
in addition to the | 6 |
it is at present | 6 |
toward the centre of | 6 |
greater than that of | 6 |
did not care to | 6 |
direction in which the | 6 |
the process by which | 6 |
for more than a | 6 |
fissures in the rock | 6 |
he did not know | 6 |
of the most remarkable | 6 |
to think that the | 6 |
have been found in | 6 |
it should be noted | 6 |
at the outset of | 6 |
probably due to the | 6 |
the region about the | 6 |
which it is subjected | 6 |
the western side of | 6 |
of the top of | 6 |
less than a hundred | 6 |
as far south as | 6 |
and it may be | 6 |
of the mississippi valley | 6 |
of the great cavern | 6 |
which it may be | 6 |
might have been expected | 6 |
on the coast of | 6 |
the th of october | 6 |
a mile or more | 6 |
the floor is a | 6 |
in the present state | 6 |
within the limits of | 6 |
the caves of the | 6 |
is likely to be | 6 |
in the absence of | 6 |
the time of my | 6 |
same as that of | 6 |
the summit of a | 6 |
over which the ice | 6 |
the deeper parts of | 6 |
to the village of | 6 |
the earlier part of | 6 |
some idea as to | 6 |
the water from the | 6 |
seems likely that the | 6 |
on the one side | 6 |
bottom of the slope | 6 |
that they do not | 6 |
to the head of | 6 |
now and then a | 6 |
the outlet of the | 6 |
the third magnesian limestone | 6 |
are of the same | 6 |
a curious fact that | 6 |
in those of the | 6 |
of the hill is | 6 |
of three or four | 6 |
various parts of the | 6 |
the agents of denudation | 6 |
a few years ago | 6 |
in the manner in | 6 |
on the ice floor | 6 |
there is a cave | 6 |
of the stream is | 6 |
the first great chamber | 6 |
the falling in of | 6 |
is a mass of | 6 |
on the western side | 6 |
the attitude of the | 6 |
to go to the | 6 |
that i was obliged | 6 |
with here and there | 6 |
the last glacial period | 6 |
the air of the | 6 |
which they are composed | 6 |
be said to be | 6 |
about one hundred and | 6 |
due to the presence | 6 |
more than one hundred | 6 |
in the line of | 6 |
as far as we | 6 |
by the falling in | 6 |
the effect that the | 6 |
high up on the | 6 |
composed of materials which | 6 |
a careful study of | 6 |
an account of the | 6 |
feet from the ground | 6 |
the ice in these | 6 |
owing to the fact | 6 |
i have met with | 6 |
there was nothing to | 6 |
with that of the | 6 |
in the face of | 6 |
is more or less | 6 |
which it has been | 6 |
nothing to do with | 6 |
on the ground that | 6 |
is supposed to be | 6 |
nature of the rocks | 6 |
of new south wales | 6 |
one of the great | 6 |
the north slope of | 6 |
it must have been | 6 |
it is only a | 6 |
in the region of | 6 |
manner in which the | 6 |
three or four meters | 6 |
waters of the sea | 6 |
the wonders of the | 6 |
a considerable quantity of | 6 |
from the face of | 6 |
may or may not | 6 |
to be in the | 6 |
his account of the | 6 |
highest point of the | 6 |
fact that it is | 6 |
in process of time | 6 |
of the entrance is | 6 |
central portion of the | 6 |
the grand cave de | 6 |
snow at the bottom | 5 |
the account of the | 5 |
from the edge of | 5 |
the present writer has | 5 |
a hundred million years | 5 |
in the region about | 5 |
that the student should | 5 |
on which we stood | 5 |
only in the case | 5 |
the flooring of ice | 5 |
the same way as | 5 |
of the present day | 5 |
the left is a | 5 |
it is hard to | 5 |
is a small cave | 5 |
the air at the | 5 |
that it may be | 5 |
melting of the snow | 5 |
to be met with | 5 |
the bulk of the | 5 |
the termination of the | 5 |
source of the loue | 5 |
feet from the top | 5 |
on the west coast | 5 |
the central parts of | 5 |
about feet below the | 5 |
taken place in the | 5 |
will see that the | 5 |
the entrance is a | 5 |
of the hills is | 5 |
and that of the | 5 |
of not more than | 5 |
are not more than | 5 |
first half of the | 5 |
which leads to the | 5 |
have been formed by | 5 |
the box work is | 5 |
the heat which it | 5 |
feet above the floor | 5 |
i have not seen | 5 |
of the materials of | 5 |
it has been found | 5 |
this is not the | 5 |
action of the water | 5 |
it is important to | 5 |
the centre of a | 5 |
an extension of the | 5 |
to the farther end | 5 |
my brother and i | 5 |
the stalactites and stalagmites | 5 |
is formed by the | 5 |
there seemed to be | 5 |
part of the town | 5 |
we have seen that | 5 |
one of the two | 5 |
at the mouths of | 5 |
it was not until | 5 |
the far end of | 5 |
farther recesses of the | 5 |
a very small part | 5 |
we were unable to | 5 |
the volume of water | 5 |
the state of vapour | 5 |
by the supposition that | 5 |
a series of caverns | 5 |
which we have already | 5 |
must have been a | 5 |
the floor of this | 5 |
in many cases the | 5 |
part of the palace | 5 |
the lowest part of | 5 |
in a straight line | 5 |
coast of new england | 5 |
about two hundred and | 5 |
the proprietor of the | 5 |
of our own solar | 5 |
a floor of ice | 5 |
the axes of the | 5 |
and there is a | 5 |
is a sort of | 5 |
it seems as if | 5 |
part of the whole | 5 |
cold currents of air | 5 |
the east side of | 5 |
in a sort of | 5 |
in the cave in | 5 |
on the same level | 5 |
the scene of a | 5 |
the presence of a | 5 |
of the nature of | 5 |
of heat from the | 5 |
the abode of the | 5 |
on top of the | 5 |
and a half to | 5 |
which is about feet | 5 |
one of the greatest | 5 |
by the assistance of | 5 |
for the same reason | 5 |
the case of our | 5 |
in regard to the | 5 |
to one of the | 5 |
that there might be | 5 |
side of the river | 5 |
in the estimation of | 5 |
so that it is | 5 |
fissures of the rock | 5 |
was covered with a | 5 |
a map of the | 5 |
that the hotter the | 5 |
to the student of | 5 |
from this point the | 5 |
have now to consider | 5 |
the crevices of the | 5 |
it is certain that | 5 |
of the rocks and | 5 |
much the same as | 5 |
at the expense of | 5 |
the th of june | 5 |
to the west of | 5 |
is found in summer | 5 |
it is about feet | 5 |
on a large scale | 5 |
from the roof to | 5 |
was by no means | 5 |
well as that of | 5 |
the names of places | 5 |
parts of the ice | 5 |
mouth of the pit | 5 |
only a few inches | 5 |
by the presence of | 5 |
all sorts of shapes | 5 |
is found to be | 5 |
a little to the | 5 |
or may not be | 5 |
that which has been | 5 |
movements of the atmosphere | 5 |
in the district of | 5 |
by the weight of | 5 |
have the habit of | 5 |
nothing for it but | 5 |
in the interstices of | 5 |
the space between the | 5 |
seems to be a | 5 |
two hundred and fifty | 5 |
from top to bottom | 5 |
and you will see | 5 |
of the giant of | 5 |
the shore of the | 5 |
side of the town | 5 |
next the surface of | 5 |
of a visit to | 5 |
surface of the soil | 5 |
course of a few | 5 |
of the great lakes | 5 |
the rocks over which | 5 |
no ice in the | 5 |
in the immediate neighbourhood | 5 |
came in contact with | 5 |
the use of a | 5 |
with respect to the | 5 |
of the air which | 5 |
to the plane of | 5 |
by the fall of | 5 |
the landlord of the | 5 |
there had been a | 5 |
very much greater than | 5 |
in the mountains of | 5 |
for it but to | 5 |
three or four hundred | 5 |
lower parts of the | 5 |
in the solar system | 5 |
that the formation of | 5 |
the extent to which | 5 |
soon as the temperature | 5 |
of rain and rivers | 5 |
the centre of gravity | 5 |
rock has been removed | 5 |
in which the water | 5 |
in the movement of | 5 |
to a point where | 5 |
in the valley below | 5 |
was nothing for it | 5 |
the irregularities of the | 5 |
as we have seen | 5 |
strong enough to blow | 5 |
which led to the | 5 |
there must be a | 5 |
only a portion of | 5 |
the rock in which | 5 |
the distance of a | 5 |
from side to side | 5 |
in order that the | 5 |
by the agency of | 5 |
there was nothing for | 5 |
in the remote past | 5 |
which we may observe | 5 |
eastern side of the | 5 |
is interesting to note | 5 |
of the caves in | 5 |
the sides of a | 5 |
about a quarter of | 5 |
cracks in the rocks | 5 |
of the air at | 5 |
at which the ice | 5 |
of the state of | 5 |
and there were no | 5 |
an inch in diameter | 5 |
than the outside air | 5 |
not more than one | 5 |
the earth from the | 5 |
hours and a half | 5 |
that in which the | 5 |
have not been able | 5 |
the depth of some | 5 |
washed away by the | 5 |
that the process of | 5 |
among the mountains of | 5 |
been formed by the | 5 |
water finds its way | 5 |
on a true scale | 5 |
there was less ice | 5 |
great mass of the | 5 |
hung from the roof | 5 |
in the direction in | 5 |
the column of water | 5 |
the same as the | 5 |
the cave has been | 5 |
time of his visit | 5 |
in the white mountains | 5 |
of ice in summer | 5 |
it might have been | 5 |
greater than it is | 5 |
here and there the | 5 |
of the ohio and | 5 |
what we may term | 5 |
the farther recesses of | 5 |
on the occasion of | 5 |
in the lower part | 5 |
some of them are | 5 |
to the absence of | 5 |
it would not be | 5 |
there seems to be | 5 |
be divided into two | 5 |
something to do with | 5 |
the distance from the | 5 |
from the end of | 5 |
of the prismatic structure | 5 |
of the materials which | 5 |
temperature of the ground | 5 |
was formed by the | 5 |
on the left side | 5 |
of the cave the | 5 |
appears to be the | 5 |
of this room is | 5 |
that the air is | 5 |
surface of the glacier | 5 |
bed of the stream | 5 |
entrance to which is | 5 |
is the same as | 5 |
of the great basin | 5 |
which one of the | 5 |
the foire de fondeurle | 5 |
in one part of | 5 |
in this state of | 5 |
one or two places | 5 |
on the eastern side | 5 |
de chimie et de | 5 |
body of the cave | 5 |
the amount of heat | 5 |
feet or more in | 5 |
cave is about feet | 5 |
the formation of subterranean | 5 |
of plants and animals | 5 |
the earth and water | 5 |
left side of the | 5 |
it can not be | 5 |
edge of the pit | 5 |
in the floor of | 5 |
it would seem that | 5 |
the next chamber is | 5 |
in the summer months | 5 |
that it is in | 5 |
the most important of | 5 |
has been taken in | 5 |
conception as to the | 5 |
a few hundred feet | 5 |
to be due to | 5 |
the left side of | 5 |
to and fro in | 5 |
the slope of ice | 5 |
fertility of the soil | 5 |
on its way to | 5 |
to see that the | 5 |
no part of the | 5 |
in the bed of | 5 |
we observe that the | 5 |
explained by the fact | 5 |
deeper parts of the | 5 |
of about the same | 5 |
to a great height | 5 |
in view of the | 5 |
in the united states | 5 |
animals and plants which | 5 |
the earth to the | 5 |
which the water is | 5 |
to the north and | 5 |
no trace of the | 5 |
only a short distance | 5 |
side of the road | 5 |
the wife of the | 5 |
readily perceive that the | 5 |
which is to be | 5 |
the continuation of the | 5 |
as if it were | 5 |
the earth may be | 5 |
from the coast line | 5 |
were formed by the | 5 |
farther side of the | 5 |
part of the floor | 5 |
at the point of | 5 |
in this way we | 5 |
of many of the | 5 |
of several thousand feet | 5 |
more than a thousand | 5 |
the face of a | 5 |
the trunk of a | 5 |
with the history of | 5 |
them that dwell in | 5 |
which mountains are composed | 5 |
the end of which | 5 |
been able to find | 5 |
a mountain in the | 5 |
and it was not | 5 |
into the interior of | 5 |
i do not know | 5 |
should be noted that | 5 |
is the case at | 5 |
of ice and snow | 5 |
not be able to | 5 |
as well as for | 5 |
feet from the surface | 5 |
he told us that | 5 |
mass of the hill | 5 |
to the open air | 5 |
certain parts of the | 5 |
walls of the cave | 5 |
mass of the earth | 5 |
of the cave were | 5 |
up and down the | 5 |
mammoth cave of kentucky | 5 |
must be due to | 5 |
more than three feet | 5 |
and on the other | 5 |
at a short distance | 5 |
roof to the floor | 5 |
may be sure that | 5 |
as great as that | 5 |
by which it is | 5 |
the expansion of the | 5 |
in the possession of | 5 |
be added to the | 5 |
to the level of | 5 |
and i am inclined | 5 |
the waves of the | 5 |
other portions of the | 5 |
it will be possible | 5 |
meters wide and meters | 5 |
the top of which | 5 |
lowest part of the | 5 |
an hour or two | 5 |
be met with in | 5 |
in the side of | 5 |
into the cave from | 5 |
the aspect of the | 5 |
a long way off | 5 |
at a higher level | 5 |
large masses of ice | 5 |
the water of which | 5 |
from all parts of | 5 |
cold in the cave | 5 |
may be in the | 5 |
and it is not | 5 |
and customs of the | 5 |
of the outside air | 5 |
of the caves of | 5 |
it would be well | 5 |
from the roof of | 5 |
it turned out that | 5 |
is the case in | 5 |
the garden of eden | 5 |
the foot of which | 5 |
may be called a | 5 |
the particles of air | 5 |
a piece of rock | 5 |
along the banks of | 5 |
the greatest amount of | 5 |
along the sides of | 5 |
it is to be | 5 |
that in summer the | 5 |
on account of their | 5 |
shore of the lake | 5 |
a foot or two | 5 |
the circle of the | 5 |
bottom of which is | 5 |
that it does not | 5 |
a series of holes | 5 |
of the air in | 5 |
falling in of the | 5 |
of the hills and | 5 |
side of this room | 5 |
south side of the | 5 |
the giant of the | 5 |
it is well known | 5 |
to the cave mouth | 5 |
it would be difficult | 5 |
the people in the | 5 |
it is doubtful whether | 5 |
the water on the | 5 |
is said that the | 5 |
the upper parts of | 5 |
and the valley of | 5 |
of our solar system | 5 |
is caused by the | 5 |
the solid mass of | 5 |
heat of the earth | 5 |
of the mammoth cave | 5 |
of which is a | 5 |
in the manner before | 5 |
the case in the | 5 |
to believe that it | 5 |
as shown in the | 5 |
told me he had | 5 |
to it is a | 5 |
much in the manner | 5 |
the east of the | 5 |
by the study of | 5 |
formation of subterranean ice | 5 |
with the help of | 5 |
had some difficulty in | 5 |
it was to be | 5 |
the friction of the | 5 |
the bodies of the | 5 |
at least a hundred | 5 |
weight of the cold | 5 |
of the air is | 5 |
down to the sea | 5 |
the hotter the summer | 5 |
it is a large | 5 |
hundred feet below the | 5 |
the hole in the | 5 |
it is said to | 5 |
it would be possible | 5 |
stalactites and stalagmites of | 5 |
two or three meters | 5 |
come to the conclusion | 5 |
at an elevation of | 5 |
the ice in this | 5 |
than the rest of | 5 |
of this kind is | 5 |
reminded me of the | 5 |
to which we have | 5 |
temperature of the district | 5 |
to bring about a | 5 |
edge of the ice | 5 |
that he was a | 5 |
at a little distance | 5 |
the roots of the | 5 |
in the cave and | 5 |
farther on is a | 5 |
of a mass of | 5 |
side of a mountain | 5 |
the right of the | 5 |
with the result that | 5 |
the remainder of the | 5 |
base of the hill | 5 |
the particles of the | 5 |
in the hope that | 5 |
in relation to the | 5 |
i visited it on | 5 |
which occur in the | 5 |
of a mile or | 5 |
the rise of the | 5 |
and in the course | 5 |
the different kinds of | 5 |
by the side of | 5 |
existence of ice in | 5 |
opening in the roof | 5 |
and here and there | 5 |
ice does not form | 5 |
part of the cavern | 5 |
the base of this | 5 |
the door of the | 5 |
five feet high and | 5 |
is a marvel of | 5 |
of the old red | 5 |
a height of about | 5 |
a very important part | 5 |
and the surface of | 5 |
may be called the | 5 |
western side of the | 5 |
of the inhabitants of | 5 |
be the result of | 5 |
and there on the | 5 |
which we have noted | 5 |
stalactites on the roof | 5 |
temperature of the water | 5 |
has the appearance of | 5 |
that in his time | 5 |
of feet below the | 5 |
that a large amount | 5 |
over which it flows | 5 |
been made by the | 5 |
there was a great | 5 |
the mammoth cave of | 5 |
of the fixed stars | 5 |
is quite clear that | 5 |
at the commencement of | 5 |
a large piece of | 5 |
are by no means | 5 |
floor was covered with | 5 |
was discovered in by | 5 |
water in the basin | 5 |
annual temperature of the | 5 |
the most of the | 5 |
effect arising from the | 5 |
is shown by the | 5 |
they appear to be | 5 |
at the farther end | 5 |
it is quite clear | 5 |
which is covered with | 5 |
is so great that | 5 |
and the fact that | 5 |
it appears that the | 5 |
when the sunne is | 5 |
and a number of | 5 |
when the temperature of | 5 |
the antiquity of the | 5 |
the coast of new | 5 |
times of heavy rain | 5 |
a general way the | 5 |
were a number of | 5 |
from the sides of | 5 |
such as may be | 5 |
the bed of a | 5 |
by some of the | 5 |
good deal of the | 5 |
in place of the | 5 |
the mouth of this | 5 |
one of which is | 5 |
other part of the | 5 |
on the sea bottom | 5 |
we know that the | 5 |
the morning of the | 5 |
the foot of mount | 5 |
the changes in the | 5 |
it was found that | 5 |
that they may be | 5 |
it had not been | 5 |
cold of winter is | 5 |
by the pressure of | 5 |
the heads of the | 5 |
of the rocks which | 5 |
he had never seen | 5 |
at the entrance of | 5 |
of the earth may | 5 |
the head of a | 5 |
in the county of | 5 |
a point where the | 5 |
the peak of derbyshire | 5 |
found that the ice | 5 |
so it is with | 5 |
means of determining the | 5 |
it is in this | 5 |
in which the earth | 5 |
meters from the entrance | 5 |
of a glacial period | 5 |
in the duchy of | 5 |
the place of the | 5 |
and as soon as | 5 |
on the upper surface | 5 |
the first half of | 5 |
along the coast of | 5 |
the strength of the | 5 |
the speed of the | 5 |
a large pit cave | 5 |
has been converted into | 4 |
must not be supposed | 4 |
southern part of the | 4 |
difficult to understand how | 4 |
the possession of the | 4 |
of which can be | 4 |
the great mass of | 4 |
the law of the | 4 |
soon as the snow | 4 |
was nothing to be | 4 |
course of the stream | 4 |
the crown of the | 4 |
temperature of the place | 4 |
portion of the water | 4 |
way to the cave | 4 |
the annales de chimie | 4 |
the blocks of stone | 4 |
outer part of the | 4 |
are a number of | 4 |
as the temperature of | 4 |
the spring of youth | 4 |
in the world about | 4 |
the summits of the | 4 |
the light and heat | 4 |
a number of places | 4 |
found that it was | 4 |
jahrbuch des schweizer alpen | 4 |
guide said he had | 4 |
that the water is | 4 |
it may well be | 4 |
those who have not | 4 |
ozarks and black hills | 4 |
they are composed of | 4 |
order to reach the | 4 |
of some of these | 4 |
are of the utmost | 4 |
of two of the | 4 |
the height of this | 4 |
very small part of | 4 |
some four or five | 4 |
to the left hand | 4 |
by far the greater | 4 |
in those parts of | 4 |
the presence of the | 4 |
in almost every part | 4 |
has been subjected to | 4 |
its name from the | 4 |
the first chamber is | 4 |
of a few inches | 4 |
to the surface on | 4 |
feet below the level | 4 |
above the bottom of | 4 |
of which have been | 4 |
is a place of | 4 |
the phenomena of the | 4 |
to me that the | 4 |
worthy of a visit | 4 |
of the water from | 4 |
east side of the | 4 |
the further end of | 4 |
any part of the | 4 |
is found on the | 4 |
quarter of an inch | 4 |
such as those which | 4 |
by way of the | 4 |
the protection of the | 4 |
since the days of | 4 |
as if it had | 4 |
the middle of august | 4 |
is occupied by a | 4 |
the production of the | 4 |
it is not easy | 4 |
the drops of water | 4 |
the good old times | 4 |
the lower portions of | 4 |
side of the aequator | 4 |
the science of geology | 4 |
takes place when the | 4 |
of the sea water | 4 |
is covered by a | 4 |
have been formed in | 4 |
it is not improbable | 4 |
of them have been | 4 |
the reason of this | 4 |
is a large cave | 4 |
people of the district | 4 |
des schweizer alpen club | 4 |
of the air on | 4 |
the point where they | 4 |
a long period of | 4 |
the rotation of the | 4 |
for a quarter of | 4 |
the cave is not | 4 |
for more than two | 4 |
cities of the plain | 4 |
it will be understood | 4 |
it was time to | 4 |
to be in a | 4 |
to the growth of | 4 |
roof and floor of | 4 |
it is reported that | 4 |
fissure in the roof | 4 |
in which it lies | 4 |
greater part of this | 4 |
have more than once | 4 |
in the development of | 4 |
height of about feet | 4 |
a few feet to | 4 |
which is found in | 4 |
portions of the earth | 4 |
of the cone is | 4 |
far the greater part | 4 |
the coast line the | 4 |
to account for it | 4 |
the internal heat of | 4 |
but it is only | 4 |
the energy of position | 4 |
two or three hours | 4 |
interior of the cave | 4 |
very long time ago | 4 |
from floor to ceiling | 4 |
four and a half | 4 |
level of the top | 4 |
is contributed to the | 4 |
des sciences de st | 4 |
is produced by the | 4 |
that the ice must | 4 |
one of the caves | 4 |
cave there is a | 4 |
this is the most | 4 |
had been unable to | 4 |
it may be as | 4 |
than two hundred feet | 4 |
explanation of the phenomenon | 4 |
most of them are | 4 |
in the autumn of | 4 |
in the southern part | 4 |
as seen from the | 4 |
many of the caves | 4 |
the point at which | 4 |
it is doubtful if | 4 |
the case of this | 4 |
if it were a | 4 |
the last of the | 4 |
by the expansion of | 4 |
a sheet of ice | 4 |
to know something of | 4 |
way in which this | 4 |
foot of the rock | 4 |
by the cold of | 4 |
it is curious that | 4 |
the descent of the | 4 |
i was unable to | 4 |
that the mean temperature | 4 |
the ice in caves | 4 |
on a small scale | 4 |
in the higher regions | 4 |
the atmosphere in the | 4 |
to be made for | 4 |
regions of the atmosphere | 4 |
the south of the | 4 |
a few hundred miles | 4 |
and out of the | 4 |
so great that the | 4 |
being found in the | 4 |
of the deeper seas | 4 |
far as we can | 4 |
but there is one | 4 |
part of the house | 4 |
this stage in the | 4 |
out of the hole | 4 |
of one hundred and | 4 |
covered with a thin | 4 |
as we have described | 4 |
caves where the temperatures | 4 |
the life of the | 4 |
and is about meters | 4 |
often happens that the | 4 |
table of relative masses | 4 |
in the act of | 4 |
the manner before described | 4 |
current of cold air | 4 |
there are a number | 4 |
there was ice in | 4 |
from the beginning of | 4 |
a depth of or | 4 |
under the head of | 4 |
in the manner indicated | 4 |
well as in the | 4 |
the whole cave was | 4 |
of the same kind | 4 |
it is not so | 4 |
that of the air | 4 |
the details of the | 4 |
appearance of having been | 4 |
for four or five | 4 |
for the study of | 4 |
as to the conditions | 4 |
of several hundred feet | 4 |
there were no draughts | 4 |
off to one side | 4 |
he assured me that | 4 |
and the roof is | 4 |
alpine regions of switzerland | 4 |
comparable to that which | 4 |
with those of the | 4 |
in the manufacture of | 4 |
the agents of decay | 4 |
the help of the | 4 |
so slow that it | 4 |
elevation above the sea | 4 |
in several places in | 4 |
deposits of volcanic ash | 4 |
that the water in | 4 |
to pieces by the | 4 |
more than a foot | 4 |
is derived from the | 4 |
distance of hundreds of | 4 |
out of the sea | 4 |
its way into the | 4 |
in the same time | 4 |
part of its course | 4 |
cases it has been | 4 |
to a place where | 4 |
the dominions of the | 4 |
assumes the form of | 4 |
by which the water | 4 |
the drip from the | 4 |
a piece of ice | 4 |
which the water flows | 4 |
is about four feet | 4 |
from this point to | 4 |
he found ice in | 4 |
be as well to | 4 |
varying from a few | 4 |
to note the fact | 4 |
have been lost in | 4 |
and at the top | 4 |
these may be briefly | 4 |
the beginning of a | 4 |
in passing from the | 4 |
about the size of | 4 |
pores of the soil | 4 |
in the path of | 4 |
hundred miles from the | 4 |
in the lowest part | 4 |
been carved out by | 4 |
to understand how the | 4 |
changes in the form | 4 |
part of the work | 4 |
the formation of rain | 4 |
see that there is | 4 |
caves and the causes | 4 |
we were obliged to | 4 |
of a sort of | 4 |
a cave in the | 4 |
near the margin of | 4 |
the only way to | 4 |
found myself in a | 4 |
from the interior of | 4 |
meters to meters wide | 4 |
for a couple of | 4 |
in the winter of | 4 |
the true explanation of | 4 |
lair photo by bamforth | 4 |
in the nature of | 4 |
the geology of russia | 4 |
of a century ago | 4 |
the rate of a | 4 |
the grains of the | 4 |
base of the mountain | 4 |
the risk of being | 4 |
which may have been | 4 |
it is at the | 4 |
of which is about | 4 |
it must not be | 4 |
of the wonders of | 4 |
much of the ice | 4 |
lying on the ground | 4 |
has been given to | 4 |
into the hands of | 4 |
this is the case | 4 |
commonly known as the | 4 |
at once to the | 4 |
height of the cave | 4 |
the materials of the | 4 |
the majority of the | 4 |
worn away by the | 4 |
in the level of | 4 |
in the ice floor | 4 |
foot or more in | 4 |
of land and sea | 4 |
it is believed that | 4 |
our illustration of the | 4 |
of a kind of | 4 |
by supposing that the | 4 |
as in many other | 4 |
meters in diameter and | 4 |
the early part of | 4 |
me that he had | 4 |
there was no ladder | 4 |
the prismatic structure of | 4 |
the remains of animals | 4 |
the water which is | 4 |
true explanation of the | 4 |
all of which are | 4 |
in the weight of | 4 |
of the eagle ford | 4 |
has been made to | 4 |
interesting to note that | 4 |
the centre of our | 4 |
of the palace is | 4 |
quite clear that the | 4 |
and which may be | 4 |
on the lower side | 4 |
rocks of which they | 4 |
is so small that | 4 |
to make use of | 4 |
in which case the | 4 |
be seen at the | 4 |
the extremity of the | 4 |
that in winter the | 4 |
and the ural mountains | 4 |
on the fact that | 4 |
i found myself in | 4 |
the valleys of the | 4 |
the eagle ford at | 4 |
and on the th | 4 |
earlier part of the | 4 |
taken place since the | 4 |
of hundreds of feet | 4 |
in the province of | 4 |
attention to the fact | 4 |
of a hundred miles | 4 |
during the passage of | 4 |
may be due to | 4 |
of the land is | 4 |
of the ice on | 4 |
ice floor meters long | 4 |
broken up by the | 4 |
the rocks of mountains | 4 |
the manners and customs | 4 |
to that part of | 4 |
mountains as they are | 4 |
find their way to | 4 |
were in some cases | 4 |
in the rear of | 4 |
we may term the | 4 |
of the ice was | 4 |
the white mountains of | 4 |
is a part of | 4 |
it is not difficult | 4 |
wall during the passage | 4 |
it has not been | 4 |
only two or three | 4 |
i do not think | 4 |
feet in length by | 4 |
in the memory of | 4 |
distance of feet from | 4 |
motion of the earth | 4 |
if he had been | 4 |
source of the axe | 4 |
of matter in the | 4 |
of hundreds of miles | 4 |
turned out to be | 4 |
we should expect to | 4 |
in the rocks of | 4 |
has been brought about | 4 |
on the margin of | 4 |
may be explained by | 4 |
edge of the great | 4 |
in the condition of | 4 |
and it is a | 4 |
side of the hill | 4 |
water in the tube | 4 |
distinction is by the | 4 |
that of the moon | 4 |
it is like a | 4 |
in which the caves | 4 |
higher than that of | 4 |
such as we have | 4 |
there is said to | 4 |
the erosion of the | 4 |
in summer than in | 4 |
the depth of ten | 4 |
the most beautiful of | 4 |
is a descent of | 4 |
important part in the | 4 |
as soon as i | 4 |
the mountains of the | 4 |
of from to feet | 4 |
floor of the sea | 4 |
it should be remembered | 4 |
the amount of solid | 4 |
and in a way | 4 |
the mountains as they | 4 |
a member of the | 4 |
a little more than | 4 |
by the falling of | 4 |
into the waters of | 4 |
a thousand feet or | 4 |
of ice are found | 4 |
or more in length | 4 |
at a place called | 4 |
the end of an | 4 |
the development of organic | 4 |
took us to the | 4 |
the climatal conditions of | 4 |
of cold in the | 4 |
distance of a mile | 4 |
and a half miles | 4 |
a small cave containing | 4 |
far away from the | 4 |
the north of the | 4 |
we should have to | 4 |
and there is no | 4 |
of the external air | 4 |
dryness of the air | 4 |
of which is the | 4 |
regions of the ozarks | 4 |
hundred miles or more | 4 |
and on the sides | 4 |
the bottoms of the | 4 |
part of the day | 4 |
the mouths of the | 4 |
and thence to the | 4 |
it is situated in | 4 |
there are many other | 4 |
the whole length of | 4 |
and feet above the | 4 |
by a sort of | 4 |
it is very difficult | 4 |
in a kind of | 4 |
to it from the | 4 |
there is a little | 4 |
brought down by the | 4 |
of the earth were | 4 |
that at one time | 4 |
most of the year | 4 |
on the left hand | 4 |
with a flooring of | 4 |
more than ten feet | 4 |
it lies in the | 4 |
of which may be | 4 |
as it is called | 4 |
of the bottom of | 4 |
as a sort of | 4 |
beneath the surface of | 4 |
from the state of | 4 |
at one time the | 4 |
when the air is | 4 |
is at the base | 4 |
knew nothing of the | 4 |
of the bed rocks | 4 |
be remembered that this | 4 |
in the village of | 4 |
in the peak of | 4 |
by the force of | 4 |
chimie et de physique | 4 |
by the aid of | 4 |
with a thin coating | 4 |
of the edge of | 4 |
that there was any | 4 |
at this stage in | 4 |
the town of vesoul | 4 |
fall of rock from | 4 |
the field where the | 4 |
at a high temperature | 4 |
had no means of | 4 |
the rock on which | 4 |
cave regions of the | 4 |
heavy cold air of | 4 |
a foot or so | 4 |
and a half from | 4 |
that the water which | 4 |
comes about that the | 4 |
the average rate of | 4 |
by the decay of | 4 |
a portion of it | 4 |
eruption of vesuvius in | 4 |
he told me that | 4 |
ice which formed the | 4 |
the higher parts of | 4 |
a few feet of | 4 |
it is not surprising | 4 |
north slope of the | 4 |
as much as possible | 4 |
in the mines of | 4 |
that a portion of | 4 |
found in the fact | 4 |
about half an hour | 4 |
or at least the | 4 |
can not well be | 4 |
the great series of | 4 |
of light and heat | 4 |
those of our own | 4 |
the beauties of the | 4 |
summer than in winter | 4 |
reached a point where | 4 |
in accordance with the | 4 |
here and there a | 4 |
of our sphere at | 4 |
a hundred and fifty | 4 |
show that the ice | 4 |
was no ice in | 4 |
the same level as | 4 |
the process of decay | 4 |
a huge mass of | 4 |
are found in many | 4 |
that he did not | 4 |
my guide said he | 4 |
there will be a | 4 |
to the labours of | 4 |
in the measure of | 4 |
an inch or two | 4 |
central part of the | 4 |
has been formed by | 4 |
the ice which is | 4 |
the bowels of the | 4 |
the name of a | 4 |
in the highlands of | 4 |
formation of ice in | 4 |
the question of the | 4 |
that it is impossible | 4 |
of the truth of | 4 |
a host of other | 4 |
the ice is not | 4 |
the theory of the | 4 |
since the time of | 4 |
through a series of | 4 |
to the cave and | 4 |
at the cave of | 4 |
did not seem to | 4 |
have forced their way | 4 |
fact that they have | 4 |
fact that when the | 4 |
than two or three | 4 |
it is due to | 4 |
it has ever been | 4 |
depths of the sea | 4 |
the ozarks and black | 4 |
the rocks have been | 4 |
at the same rate | 4 |
in the work of | 4 |
up and down through | 4 |
in the month of | 4 |
of the cave house | 4 |
mountains of new hampshire | 4 |
a large area of | 4 |
to the place where | 4 |
found in the hottest | 4 |
down to the cave | 4 |
of the utmost importance | 4 |
is a series of | 4 |
the curator was lowered | 4 |
the corner of the | 4 |
raise the temperature of | 4 |
and at the bottom | 4 |
would probably have been | 4 |
the air which they | 4 |
would have been impossible | 4 |
many thousands of years | 4 |
of this action is | 4 |
the house of the | 4 |
in the bay of | 4 |
parts of great britain | 4 |
part of the great | 4 |
at that time the | 4 |
the middle of july | 4 |
the existence of which | 4 |
as big as a | 4 |
meters to meters high | 4 |
a yard or two | 4 |
the surface of a | 4 |
way back to the | 4 |
time of the first | 4 |
those which have been | 4 |
which are to be | 4 |
axes of the prisms | 4 |
in the year the | 4 |
which make up the | 4 |
marke out a point | 4 |