quadgram

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
ethiopian oriental australian sub313
on the other hand195
in the case of170
the distribution of the144
the bottom of the140
at the same time139
the end of the139
one of the most130
at the present day116
have been found in108
the case of the104
the surface of the103
are found in the102
in the same way94
on the distribution of93
in order that the91
the close of the90
the whole of the87
is found in the86
as well as the85
the mouth of the85
the fact that the85
th th th th83
been found in the83
seems to have been78
the rest of the77
the greater part of77
the middle of the76
in the course of75
remarks on the distribution74
are confined to the74
the base of the72
the isle of wight72
of the natural size71
of the upper silurian71
for the most part71
a large number of71
the top of the70
general remarks on the69
at the end of69
one and a half67
is one of the66
parts of the world66
of animals and plants66
an extinct genus of66
of the oriental region65
of the united states65
for the first time64
the nature of the63
to be found in62
in the form of62
and a half feet61
the head of the61
in the first place60
of the present day60
in the middle of59
the beginning of the59
the origin of the58
of the australian region57
as far as the56
to that of the55
the remains of the55
of the lower silurian55
of one of the54
tropical and south africa53
the west indian islands53
all regions but australian53
north and south america53
at the bottom of52
the same number of52
of which are peculiar51
the evolution of the51
the upper part of51
the valley of the51
the history of the50
with the exception of50
the story of the50
a foot and a50
to those of the49
the life of the49
the face of the49
that is to say49
it is probable that48
under the name of48
be found in the48
most abundant in the48
there can be no48
is confined to the48
greater part of the48
of the origin of47
of some of the47
of the old world47
the structure of the46
distribution of the genera45
for the purpose of45
in some of the45
with regard to the44
as well as in44
europe and north america44
all parts of the44
in the shape of44
of a libra of44
of the ethiopian region44
the size of a44
that it may be44
in the same manner43
reason to believe that43
the bones of the42
upper part of the42
cape of good hope41
the interior of the41
of the same age41
seem to have been41
on the one hand41
two and a half41
may be regarded as40
the manner in which40
it is difficult to39
the size of the39
in the history of39
it is impossible to39
of the neotropical region39
in new south wales39
a few of the39
at the close of39
the lower part of39
a considerable number of39
the level of the39
the back of the38
the range of the38
of the rocky mountains38
is that of the38
the formation of the38
it is to be38
the sides of the38
of the genera of38
of the distribution of38
museum of natural history38
of new south wales37
on account of the37
the time of the37
by means of a37
of the isle of37
the heat of the37
the character of the37
new south wales and36
of ethiopian genera of36
of the most remarkable36
with those of the36
the upper miocene of36
of the northern hemisphere35
appears to have been35
can be no doubt35
the length of the35
is to be found35
a great number of34
has been found in34
the second long wall34
the limits of the34
to account for the34
crust of the earth34
some of the most34
as in the case34
the ends of the34
in the united states34
of a number of33
a large part of33
that part of the33
of the existence of33
in the oriental region33
other parts of the33
lower part of the33
the geographical distribution of33
have been able to33
nearly allied to the33
to the present day33
of the remains of33
the shores of the33
so far as we32
the depths of the32
in the distribution of32
in all parts of32
to the conclusion that32
the south of france32
and as many digits32
in the upper miocene32
in accordance with the32
of carbonate of lime32
appear to have been32
in so far as32
it is necessary to32
the same way as32
the order of the32
are to be found32
like that of the31
that some of the31
to the fact that31
other part of the31
and new south wales31
which are found in31
the course of the31
with that of the31
the latter part of31
the old red sandstone31
over the whole of31
in front of the31
with the remains of31
the cape of good31
are peculiar to the31
of the nearctic region30
the age of the30
of australian genera of30
the side of the30
a more or less30
ethiopian and oriental regions30
to the end of30
yielded the remains of30
history of the earth30
means of dispersal of30
as large as a30
seams in the rocks30
of oriental genera of30
part of the world30
of the evolution of30
by the fact that30
the development of the30
this part of the30
as that of the30
in the bottom of29
at a distance of29
a part of the29
the first of these29
it must have been29
in the isle of29
closely allied to the29
to belong to the29
it is true that29
foot and a half29
of the nature of29
the floor of the29
on the surface of28
in order that it28
range of ethiopian genera28
of which we have28
of the higher animals28
the following are the28
in the upper silurian28
surface of the earth28
in the fact that28
of gold and silver28
in this way the28
in the south of28
when it has been28
at the present time28
the crust of the28
as we shall see28
from the fact that28
the waters of the27
the climate of the27
which are peculiar to27
in addition to the27
the discovery of the27
it may be said27
the direction of the27
that they may be27
the group of the27
of many of the27
the oriental and australian27
our knowledge of the27
to have been a27
the centre of the27
face of the earth27
the exhausted liquation cakes27
the weight of the27
the natural history museum26
of a libra and26
it will be seen26
the past history of26
of the th century26
to the bottom of26
each side of the26
part of the globe26
a portion of the26
are peculiar to it26
the second and third26
range of oriental genera26
that there is no26
the whole oriental region26
de ortu et causis26
there is reason to26
the remains of a26
the lower end of26
there can be little26
the upper end of26
have been discovered in26
peculiar to the region26
the great majority of26
as soon as the25
in the old world25
the most important of25
of the cretaceous period25
in the neighbourhood of25
of the genera is25
in such a way25
on the part of25
of the tertiary era25
a libra and a25
past history of the25
by the action of25
species of the genus25
are known as the25
of the tertiary period25
as we have seen25
in the island of25
of the genera are25
some of the more25
the continent of europe25
the name of the25
story of the earth25
palms and as many25
a large proportion of25
latter part of the25
in the northern hemisphere25
in which they are25
on each side of24
the force of the24
it must be remembered24
we come to the24
of the more important24
the number of species24
so that it may24
it is clear that24
and at the same24
part of this work24
found only in the24
of the most important24
in connection with the24
can be little doubt24
one of which is24
in the miocene of24
in which there is24
oriental and australian regions24
in other parts of24
forms of animal life24
palm and two digits24
veteribus et novis metallis24
said to have been24
is said to be24
than that of the24
the summit of the24
a palm and two24
to be allied to24
on the shores of24
see note on p24
we find that the24
the total number of24
third of a libra24
the form of a24
half a libra of23
for a long time23
and a half digits23
at the mouth of23
every part of the23
as far south as23
half an uncia of23
and some of the23
the body of the23
the remainder of the23
de veteribus et novis23
we do not know23
it is in the23
the third long wall23
the edge of the23
and the same number23
the study of the23
in the footnote on23
united states national museum23
are most abundant in23
as compared with the23
various parts of the23
the footnote on page23
the family of the23
of de re metallica23
a quarter of a23
the shape of a23
of the species are23
some idea of the23
in footnote on page23
the front of the23
like those of the23
the ethiopian and oriental23
the north of england22
of the earth is22
as those of the22
in various parts of22
the foot of the22
at the time of22
of the glacial period22
there are some who22
which must have been22
a third of a22
the bed of the22
heat of the fire22
a species of the22
on the top of22
the animals of the22
by means of the22
is by no means22
range of australian genera22
the united states national22
range over the whole22
as far north as22
of this kind are22
to a great extent22
the characters of the22
the genera is as22
at the top of22
of the carboniferous period22
in any of the22
quarters of a foot21
order that it may21
in the australian region21
the banks of the21
will be found in21
in the direction of21
the question of the21
in which they were21
similar to those of21
and in this way21
especially characteristic of the21
are characteristic of the21
known to occur in21
of the lower jaw21
in europe and america21
there is no evidence21
may be said to21
foot and a palm21
the exception of the21
lower end of the21
at the beginning of21
they must have been21
from east to west21
of the south american21
any other part of21
in the absence of21
of the fauna of21
so far as i21
genera is as follows21
than those of the21
in regard to the21
from time to time21
highly characteristic of the21
that it is a20
of the geological survey20
the use of the20
the action of the20
is said to have20
as one of the20
feet above the sea20
of the history of20
but it is not20
to be regarded as20
the way in which20
and there is a20
is covered with a20
a great variety of20
to brazil and bolivia20
the distribution of animals20
the hypothesis of evolution20
we have seen that20
taken out of the20
a libra of silver20
that it is not20
in the region of20
by the heat of20
allied to the existing20
the depth of the20
it is possible that20
the south of england20
are represented by the20
the australian and neotropical20
reptiles and amphibia of20
have yielded the remains20
in the southern hemisphere20
the shape of the20
the rocks of the20
to have been the20
of land and water20
as long as the20
the form of the20
the first appearance of20
life of the period20
be no doubt that20
found also in the20
of the mediterranean sub20
they are found in19
there is also a19
in the lower part19
is also found in19
of the shells of19
of the most characteristic19
bottom of the sea19
of thousands of years19
most nearly allied to19
the commencement of the19
a large portion of19
as a matter of19
a great deal of19
of the birds of19
from the rest of19
the west coast of19
the part of the19
in such a manner19
are found in all19
we find in the19
the birds of the19
is reason to believe19
in many parts of19
of land and sea19
to the south of19
the imperfection of the19
some of the species19
of the fact that19
so far as known19
that they have been19
beds of the same19
in view of the19
of life on the19
in some parts of19
have been made by19
the work of the19
in the upper part19
feet and two palms19
in the lower silurian19
from that of the19
the doctrine of evolution19
contain the remains of19
are more or less19
similar to that of19
and that of the19
in the way of19
quarter of a libra19
to the origin of19
is three feet long19
more than half the19
of which there is19
the fourth long wall19
far back as the19
of europe and asia19
and it is not19
at a height of18
the whole of this18
each of which is18
parts of the globe18
about the size of18
so far as the18
at the base of18
on the banks of18
been discovered in the18
as might be expected18
the fact that they18
it is obvious that18
of which i have18
in the number of18
hundreds of thousands of18
a greater or less18
the fossils of the18
and there is no18
from a drawing by18
any part of the18
as well as of18
both in europe and18
there has been a18
to which i have18
is known as the18
the struggle for existence18
in the following way18
it is interesting to18
the oriental and ethiopian18
a large amount of18
and one and a18
like that of a18
in a state of18
of the minor triangle18
be little doubt that18
be seen in the18
west and south africa18
as far back as18
are common to the18
species of animals and18
a good deal of18
in which it is18
in the face of18
that there has been18
in consequence of the18
mouth of the tunnel18
is more or less18
in the miocene period18
arms of the sea18
feet and a palm18
out of the furnace18
on the other side18
that many of the18
three and a half18
from those of the18
are said to be18
will be seen that18
in the nearctic region18
the majority of the18
to a depth of18
heat of the sun18
and many of the18
with which we are18
we now come to17
found in all the17
could not have been17
of the south of17
it is easy to17
in europe and north17
libra and a semi17
and a foot and17
in the museum of17
manner in which the17
the roof of the17
of the coal period17
that there is a17
of the bones of17
and it will be17
there must have been17
is shown by the17
the fauna of the17
the northern and southern17
the old world and17
the miocene deposits of17
in each centumpondium of17
the present state of17
peculiar to this sub17
as i have said17
in de natura fossilium17
in de re metallica17
the warmer parts of17
many parts of the17
of the miocene period17
the existence of a17
a time when the17
must have been a17
the whole region cosmopolite17
far as we know17
the upper and lower17
conclusions as to the17
species have been found17
belong to the same17
in the british museum17
to a height of17
the region of the17
the place of the17
and it has been17
the islands of the17
which is made of17
attained a length of17
in the latter part17
the pliocene deposits of17
australia and new zealand17
as well as to17
large part of the17
the animals and plants17
the atlantic and pacific17
india and ceylon to17
oriental and ethiopian regions17
side of the minor17
it may be that17
so that it is17
the walls of the17
the ancestors of the17
upper end of the17
confined to this sub17
over the greater part17
of those of the16
found in the miocene16
which are known as16
one of the largest16
up to the present16
the great mass of16
the age of reptiles16
are mortised into the16
in this case the16
the following is the16
australia and south america16
it is certain that16
in the centre of16
to the present time16
the geological survey of16
it will be well16
of the zoological society16
in the valley of16
in any other part16
in a similar manner16
geographical distribution of animals16
in a general way16
found in the upper16
in the ethiopian region16
in favour of the16
the lower and upper16
a palm and a16
palms and a digit16
each centumpondium of which16
of the age of16
at a time when16
three feet long and16
in the development of16
been described from the16
the largest of the16
a half feet long16
at the head of16
to say nothing of16
and a palm wide16
a peculiar genus of16
be one of the16
in point of time16
must be remembered that16
in the habit of16
north america and europe16
two palms and as16
now come to the16
to the australian region16
are represented by a16
families and genera of16
found in the same16
the distribution of land16
in the structure of16
the elevation of the16
we have here a16
in the miocene deposits16
species are found in16
is not to be16
we shall find that16
which are confined to16
supposed to have been16
as i have already16
of the furnace is16
the back part of16
in the midst of16
all of which are16
also found in the16
for the space of16
in the caves of16
of a series of16
for the sake of16
in every part of16
to show that the16
of europe and north16
a matter of fact16
at the lower end16
some of them are16
the largest and most16
distribution of land and16
over a large part16
bottom of the tunnel16
the position of the16
we have already seen16
genera and species of16
doubt as to the16
must have been the16
an uncia and a16
may be able to16
to the nature of16
of the oriental and15
the rocky mountains and15
the furnace into the15
in the light of15
in the oriental and15
which there is a15
it is possible to15
as many digits wide15
uncut edges and gilt15
to such an extent15
but it must be15
edges and gilt tops15
sixth of a libra15
we know that the15
there is no reason15
the thickness of the15
of the several regions15
has the range of15
of most of the15
at the back of15
in the evolution of15
most of the genera15
de mensuris et ponderibus15
lead is separated from15
the existence of the15
the case with the15
be regarded as a15
the names of the15
the mammoth and the15
allied to the living15
to the th century15
are distributed as follows15
the relations of the15
is not at all15
beyond the limits of15
it seems to have15
in the natural history15
does not seem to15
of the jurassic period15
no less than genera15
not only in the15
we have now to15
of the geological record15
many of the most15
of the eastern hemisphere15
of a large number15
of the genera and15
of plants and animals15
the same manner as15
range of the family15
the genera and species15
the limestones of the15
of two or three15
there may have been15
the main features of15
brazil and la plata15
rise of the land15
deposits of this age15
it is found in15
of life in the15
the power of flight15
the peninsula of india15
some part of the15
a drachma of silver15
between the mouth of15
information as to the15
which remains in the15
it is poured into15
feet and as many15
a few species of15
the shells of the15
wholly confined to the15
whole region almost cosmopolite15
has one species in15
more or less completely15
is the case with15
in the presence of15
the whole region almost15
in the west indian15
animal and vegetable life15
the lower silurian rocks15
the shells of foraminifera15
is a matter of15
genera are as follows15
the same age in15
may be seen in15
may be said that15
mexico to costa rica15
in the th century15
rocks of north america15
in north america and15
a digit and a15
in one of the15
stones which easily melt15
the succession of life15
of the earth and15
and most of the15
of the upper jaw15
from the size of15
the old and new15
in a similar way15
victoria and new south15
it is evident that15
of the same length15
to occur in the15
the most remarkable of14
of the earth in14
we shall see that14
be said to be14
part of the building14
of the malay archipelago14
there are peculiar genera14
it will be found14
the mind of the14
in the carboniferous rocks14
made up of the14
australian and neotropical regions14
that it must have14
evidence as to the14
university of kansas lawrence14
to say that the14
of the animal kingdom14
spoken of as the14
it appears to have14
seems to be a14
depths of the earth14
have also been found14
south of the equator14
of one of these14
the total absence of14
it would seem that14
the great group of14
by far the most14
rest of the world14
in proportion to the14
to me to be14
a certain amount of14
are fixed to the14
the first and second14
every reason to believe14
so called from the14
found in the lower14
the result of the14
it will not be14
in some cases the14
palms and two digits14
the end of this14
the deposition of the14
a palm wide and14
in each of the14
of the species of14
by the use of14
of the modern world14
with one species in14
distant from each other14
especially abundant in the14
a genus of the14
from the nature of14
may be taken as14
the appearance of the14
are the remains of14
distribution of the families14
old and new worlds14
and three palms long14
to belong to it14
must have been very14
there are a few14
in many of the14
they seem to have14
may be divided into14
of the nineteenth century14
the remains of animals14
victoria and south australia14
to the neotropical region14
it appears that the14
digit and a half14
of gold or silver14
of the story of14
and as many palms14
it is quite possible14
that one of the14
it is one of14
in the interior of14
and a half wide14
new zealand and the14
be referred to the14
the old stone age14
it is believed that14
parting gold and silver14
the edges of the14
of each of the14
by the force of14
of the glacial epoch14
in the order of14
large proportion of the14
the rise of the14
and a digit thick14
is believed to have14
from san josecito cave14
is placed in the14
same number of digits14
and the mascarene islands14
the families and genera14
to believe that the14
in the vicinity of14
a small amount of14
the neotropical region is14
from the mouth of14
back part of the14
in the second place14
a vast number of14
there is a great14
the space between the14
and a digit wide14
of the skeleton of14
from the upper miocene14
one hundred and fifty14
one of these is14
and two digits wide14
university of kansas publications14
the earlier portion of14
are known to have14
ranging back to the14
it may be well14
furnace into the forehearth14
palm and a digit13
foot and three palms13
of the life of13
to the age of13
this is the case13
and a half long13
allied to those of13
temperate and tropical regions13
of the interior of13
been detected in the13
be remembered that the13
which lies between the13
characteristic of the oriental13
but it may be13
a distance of about13
and it is a13
eorum quae effluunt ex13
a single species of13
so that we have13
which is to be13
one or other of13
in an earthen crucible13
the owners of the13
as large as the13
of the same kind13
by a series of13
remains are found in13
the northern part of13
one and the same13
to conclude that the13
the duke of argyll13
in comparison with the13
as well as by13
species of the same13
all the rest of13
are about fossil species13
in the hands of13
the caves of brazil13
what is now the13
be borne in mind13
of the old stone13
in the matter of13
the beds of the13
one end of the13
a height of a13
and one foot wide13
in the character of13
i will now speak13
all over the world13
animals and plants are13
the tip of the13
in the neotropical region13
mode of formation of13
the line of the13
with an iron shovel13
of which it is13
america east of andes13
the other end of13
a sixth of a13
in the upper eocene13
of genera and species13
well as in the13
in common with the13
natura eorum quae effluunt13
to return to the13
earlier portion of the13
large portion of the13
are especially characteristic of13
a study of the13
of the geological society13
the extinction of the13
the third and fourth13
the great series of13
is made in the13
in the coal period13
will be well to13
a great series of13
it is said that13
drawn out of the13
of the new zealand13
of the north of13
chili and la plata13
there are about fossil13
do not seem to13
at a comparatively recent13
to the old world13
in the lower jaw13
and those of the13
drum made of rundles13
in the same direction13
in the arctic regions13
from west to east13
there seems to be13
to some of the13
so that they may13
common to the two13
at the foot of13
antiquity of the genera13
which is in the13
the front part of13
and on the other13
those of the modern13
is a palm and13
the presence of the13
costa rica to brazil13
there is in the13
one of the best13
it has been shown13
as to the origin13
australia and new guinea13
south america east of13
de natura eorum quae13
natural size and enlarged13
of the size of13
which are composed of13
the straits of magellan13
set of middle rafters13
lines of migration of13
of the animals of13
the evidence of the13
with a wooden scrubber13
to the north of13
the higher forms of13
than it is now13
of the shell is13
such a way that13
the greater number of13
the same time the13
the seas of the13
of the manchurian sub13
with the bones of13
for a distance of13
to be able to13
of animals inhabiting the13
not seem to have13
is by far the13
parts of north america13
about the same time13
quae effluunt ex terra13
the southern part of13
and it is probable13
and two digits long13
the fishes of the13
mexico to brazil and13
of the families and13
of the most interesting13
the teeth of the13
believed to be of13
more or less closely13
surface of the body13
the genera are as12
one of the great12
part of the tertiary12
in the space of12
of the head and12
in the state of12
few of the more12
are very abundant in12
closely related to the12
have led to the12
the occurrence of the12
but to return to12
in the blast furnace12
and the fact that12
of the same family12
is six feet long12
we may be sure12
the occurrence of a12
in the lower cretaceous12
between it and the12
of the same species12
have been unable to12
life on the globe12
the story of evolution12
the beams of the12
to suppose that the12
zoological characteristics of the12
the particles of gold12
parting gold from copper12
of the philippine islands12
manner in which they12
is characteristic of the12
there is only one12
of the north american12
the plants of the12
confined to the west12
of the crust of12
has not yet been12
part of the furnace12
is supposed to be12
division of the earth12
and a palm thick12
are placed in the12
the eocene and miocene12
surface of the globe12
in the rocks of12
all united states and12
the influence of the12
it is important to12
the record of the12
and half a foot12
on the face of12
a little more than12
in the story of12
forms of this group12
the tops of the12
in the north of12
from the surface of12
temperate and tropical seas12
to which they are12
feet long and one12
is allied to the12
from the miocene of12
the valleys of the12
the fourth part of12
they are most abundant12
we have been able12
before the end of12
the bodies of the12
of ethiopian families of12
nd rd th th12
genera are distributed as12
the remains of these12
such a manner that12
in the seas of12
warmer parts of the12
it seems to me12
early part of the12
as we have already12
so far as it12
and in the upper12
and a palm and12
the conclusion that the12
in the pliocene of12
feet long and a12
are the most important12
end of the first12
to that of a12
of oriental families of12
seems to be the12
is common to the12
that it was a12
in order that they12
very characteristic of the12
with a few species12
on the borders of12
families of animals inhabiting12
the lower eocene of12
south wales and queensland12
the life succession theory12
it seems to be12
is a foot and12
of a centumpondium of12
appears to be the12
the number of genera12
to be wondered at12
table of oriental families12
more nearly allied to12
the period of the12
great majority of the12
the story of life12
belong to the genera12
the upper eocene of12
a foot and three12
in the pliocene deposits12
changes of physical geography12
of the development of12
the nozzles of the12
of the southern hemisphere12
which belong to the12
on the origin of12
the inhabitants of the12
it is a curious12
hole of the furnace12
by which it is12
and this is the12
have been formed by12
appears to be a12
is most abundant in12
tables of distribution of12
on the one side12
nozzles of the bellows12
the temperature of the12
than in any other12
of which the first12
table of ethiopian families12
for the use of12
names in italics show12
it would not be12
to the south american12
in the eocene of12
the strength of the12
the forests of the12
those of the present12
the vegetation of the12
the plains of india12
of the geographical distribution12
and the absence of12
of the mexican sub12
from side to side12
the south of europe12
as will be seen12
with reference to the12
in most of the12
with a hooked bar12
the height of the12
two feet and as12
in the life of12
within the limits of12
after they have been12
by the possession of12
but there is no12
some of which are12
properly to belong to12
the material which has12
are among the most12
many of the genera12
so many of the12
the type of the12
by the side of12
the fact that it12
the furnace in which12
to the oriental region12
abundant in the oriental12
is made up of12
feet and three palms12
may be considered as12
for the same reason11
in the depths of11
the width of the11
and one of the11
is given in the11
the same way that11
in the place of11
the proceedings of the11
that there was a11
far as i know11
the genera are distributed11
six feet in length11
in addition to these11
from north to south11
borne in mind that11
as to the nature11
is impossible to say11
in parting gold from11
at a later period11
of the eocene period11
genera of terrestrial mammalia11
and it would be11
birthplace and migrations of11
the lower miocene of11
is found only in11
we have in the11
to be in the11
of these are peculiar11
bolivia and la plata11
old red sandstone of11
when we consider the11
is represented by a11
the facts of the11
the cape verd islands11
a few years ago11
and a sicilicus of11
a peculiar form of11
rag and chain pumps11
as a general rule11
front part of the11
the geology of the11
the most important being11
that it is impossible11
and the philippine islands11
of this kind is11
three palms and two11
that it can be11
in place of the11
there is not a11
long and a foot11
great mass of the11
by a species of11
in the middle devonian11
identical with those of11
the appearance of a11
so far as they11
as that of a11
the natural size and11
by the distribution of11
it was found that11
the gulf of mexico11
of terrestrial mammalia and11
of the same number11
animal life of the11
may be found in11
number of peculiar genera11
the lower cretaceous of11
in this part of11
order that they may11
of each of these11
blast of the bellows11
i will speak of11
two feet long and11
in spite of the11
of the forms of11
the impressions of the11
the species of the11
which is known as11
in the highest degree11
the indian and pacific11
of the presence of11
washing ore or alluvial11
to the level of11
on the west coast11
are represented in the11
the origin of life11
is mixed with the11
there are also a11
with some of the11
the mouths of the11
of the british museum11
in this manner the11
and the number of11
long and one foot11
not considered properly to11
does not appear to11
little more than a11
a number of peculiar11
in the nature of11
that there may be11
the temperate regions of11
which has settled in11
in accordance with this11
the arrangement of the11
of succession of the11
it is necessary that11
species is found in11
and that it is11
are found on the11
if it is not11
the subject of the11
is that of a11
beams of the crane11
careful study of the11
to be of the11
be taken as a11
rd th th th11
in the mind of11
for washing ore or11
of animal and vegetable11
if there is a11
are not known to11
are by no means11
first side of the11
it is not so11
five feet in length11
are also found in11
may have been a11
covered with a lid11
the theory of evolution11
evidence of the existence11
as shown by the11
are of the same11
coast of south america11
it must be admitted11
of the theory of11
believed to have been11
the owner of the11
a small quantity of11
are not to be11
in the geological record11
of north and south11
will now speak of11
taken place in the11
considered properly to belong11
the account of the11
interior of the earth11
when they have been11
in point of fact11
the presence of a11
have occurred in the11
are not considered properly11
to the existence of11
of the human race11
is placed in a11
to new zealand and11
as belonging to the11
and some of them11
nearly related to the11
survey of great britain11
number of species of11
go back to the11
the same time as11
the west of the11
are a group of11
been recorded from the11
the fresh waters of11
of which are found11
may be due to11
of the same genus11
of a species of11
the former of these11
with a number of11
of these is the11
that most of the11
known to have existed11
in the struggle for11
which occur in the11
be regarded as the11
than any of the11
the view that the11
the early part of11
we shall have to11
and a half thick11
that it has been11
on either side of11
the first mention of11
at right angles to11
of the families of11
as a sort of11
europe and north africa11
bear in mind that11
the southern united states11
order of succession of11
are of two kinds11
to the oriental and11
an extinct order of11
of mammalia and birds11
the early history of11
of the middle ages11
the south of the11
it may have been11
has settled in the11
which it has been11
indian and pacific oceans11
belonging to the genera11
the cakes of copper11
terrestrial mammalia and birds11
a few species in11
it would have been11
characteristic fossils of the11
deposits of north america10
and a half of10
found in the pliocene10
are said to have10
is made of rundles10
composed of carbonate of10
it will be remembered10
of any of the10
in a few words10
to which it is10
the other genera are10
the american museum of10
the time when the10
the existing distribution of10
of the shaft and10
the entire absence of10
the nature of these10
almost confined to the10
genera peculiar to the10
which it would be10
what are now the10
either side of the10
in which there are10
of a single species10
is due to the10
and the bottom of10
the meaning of the10
a curious fact that10
west coast of america10
as it is now10
exhausted liquation cakes are10
very abundant in the10
all regions but ethiopian10
of the bottom of10
like those of a10
islands of the pacific10
genera and species are10
the following is a10
and it is therefore10
a large quantity of10
northern and southern hemispheres10
two digits wide and10
it is found that10
one of the chief10
by the discovery of10
to the cupellation furnace10
confined to the temperate10
from the pliocene of10
remains have been found10
during the miocene period10
an account of the10
of the coal formation10
have been described by10
the number of peculiar10
in the time of10
which easily melt in10
it is not necessary10
will be found to10
a distance of two10
different from those of10
some parts of the10
between the second and10
all regions but nearctic10
is quite possible that10
three palms wide and10
japan and north china10
the rock of the10
rocks of this age10
a way as to10
no less than species10
animals and plants which10
changed the reference for10
from the back of10
and a drachma of10
is mortised into the10
the fossil remains of10
to the formation of10
in the opposite direction10
the dawn of the10
the earlier part of10
far as we are10
the last part of10
also been found in10
the silver from the10
which are characteristic of10
is put into the10
they may have been10
and also in the10
is composed of a10
by means of which10
in the immediate vicinity10
genera are confined to10
as well as a10
on the right side10
and when it has10
would appear to be10
the great family of10
as is the case10
the absence of any10
of life upon the10
the most important and10
is derived from the10
the head of a10
palm and three digits10
are a pair of10
it is advisable to10
the borders of the10
a libra of the10
such as might be10
by the remains of10
the result of a10
if the ore is10
by the study of10
forms of life which10
this view of the10
to prevent it from10
the whole series of10
confined to the region10
down to the present10
american museum of natural10
the body of a10
it appears to me10
close of the cretaceous10
to which the name10
for millions of years10
is three palms and10
to one of the10
bowels of the earth10
state of new york10
that there must have10
to the sandwich islands10
species of this family10
the works in which10
the whole region oriental10
being confined to the10
mexico to bolivia and10
as if it were10
form one of the10
from the study of10
belonging to the family10
of the continent of10
in spite of all10
in south america and10
are found also in10
that they were not10
frames for washing ore10
the foundations of the10
in the proceedings of10
bottom of the crucible10
head of the bellows10
no doubt as to10
and a half centumpondia10
many of the species10
a hole in the10
the depth of a10
the same length as10
they appear to have10
the first part of10
and other parts of10
of the major triangle10
we may conclude that10
the flora and fauna10
and in this manner10
all that can be10
all the great continents10
which i have spoken10
close of the mesozoic10
in any part of10
is interesting to note10
most of these are10
in the oamaru series10
but also in the10
different parts of the10
proceedings of the zoological10
by the name of10
a genus of trilobites10
some of these are10
the nature of a10
the state of new10
of the peculiar genera10
it seems probable that10
from the eocene of10
are believed to be10
supposed to be the10
marine beds of the10
of the permian period10
ranges over the whole10
which the water flows10
mouth of the furnace10
a half feet wide10
have settled in the10
north america in the10
of the new world10
a drawing by j10
most of the species10
of the pliocene period10
in which silver is10
will be found that10
confined to the australian10
flora and fauna of10
and a digit long10
it is not a10
they appear to be10
that they did not10
the long series of10
divisions of the earth10
in the fossil state10
not to be wondered10
fathoms and two feet10
to have been made10
of which there are10
is poured into the10
one hundred and twenty10
of the land and10
the general character of10
it is at present10
the evolution of man10
with a pair of10
the first side of10
before the close of10
in genera and species10
the mammals of the10
and two palms long10
as the result of10
be allied to the10
if it does not10
to be seen in10
we are able to10
in order to make10
the seams in the10
remains of the mammoth10
but a single species10
such a way as10
as soon as it10
be said that the10
same length as the10
a great quantity of10
a thickness of feet10
the animal life of10
by far the richest10
the exception of a10
is supposed to have10
is very rich in10
of the skeletons of10
bottom of the shaft10
during the tertiary period10
general character of the10
is a curious fact10
the study of fossils10
the margins of the10
generalised section of the10
to form a distinct10
of the cambrian period10
there is a large10
than it is at10
the course of time10
if they had been10
not known to occur10
the birds of prey10
the distance between the10
in the cupellation furnace10
by this method the10
of the paris basin10
of europe and america10
character of the fauna10
the whole region n10
the hole in the10
in the words of10
the north american continent10
the skeleton of a10
very closely allied to10
belong to the genus10
to the study of10
it is well known10
pliocene deposits of the10
no doubt that the10
climate of the earth10
and one in the10
have been described from10
the margin of the10
a very large number10
to be one of10
at the surface of10
the vast majority of10
the other side of10
by the occurrence of10
the water of the10
it is sufficient to10
with an iron rod10
in the sense of10
the former existence of10
the value of the10
in the third furnace9
the devonian rocks of9
celebes to new guinea9
most important of the9
interesting to note that9
and many of them9
greater or less extent9
europe and western asia9
as far as we9
part of the continent9
is thrown into the9
a vast amount of9
have originated in the9
have been recorded from9
of the mesozoic period9
there is every reason9
in the series of9
in the next chapter9
in order to prevent9
close of the carboniferous9
not exposed to the9
to guiana and brazil9
a centumpondium of copper9
placed in the furnace9
a glimpse of the9
one hundred and one9
is the result of9
been able to find9
have the power of9
the fore part of9
the immediate vicinity of9
of which they are9
say a few words9
exposed to the fire9
the hearth of the9
both north and south9
total number of species9
may be sure that9
doubt but that the9
which appears to be9
there is some reason9
and it is only9
it is doubtful if9
both sides of the9
of this group are9
the remains of fishes9
from the furnace into9
in the eocene and9
of one or two9
have been subjected to9
that they must have9
is every reason to9
and a half unciae9
upper miocene of the9
a distance of three9
so that the water9
on the canvas strakes9
as to the age9
are represented by two9
said to be allied9
a knowledge of the9
tropical regions of the9
to have taken place9
in the upper jaw9
exclusively confined to the9
it has been found9
a genus of brachiopods9
the southern extremity of9
strata of this age9
of such a nature9
after the manner of9
on account of their9
a number of the9
for the purposes of9
of south temperate america9
of the doctrine of9
of the sun and9
be placed in a9
so characteristic of the9
in the position of9
they have been found9
in the present state9
west of the island9
to the group of9
of this kind of9
when we consider that9
of which i will9
it has been suggested9
compared with that of9
to be confined to9
have seen that the9
take the place of9
when it has cooled9
that the climate of9
as we are aware9
it is a very9
the possession of a9
are absent from the9
upper miocene deposits of9
the north temperate zone9
are especially abundant in9
the same as that9
have been produced by9
tabular view of the9
the class of birds9
a small portion of9
foot of the himalayas9
in the proportion of9
new species have been9
same number of rafters9
units of four siliquae9
shown to have been9
part of the old9
into a number of9
hole is always open9
great group of the9
the side of a9
species occur in the9
to belong to this9
from island to island9
nearctic and neotropical regions9
one side of the9
the hands of the9
at the other end9
and in the middle9
from the top of9
is melted in the9
miocene deposits of the9
as much as possible9
series of new zealand9
to the west coast9
first part of the9
the blast of the9
of these belong to9
in the one case9
upper surface of the9
region as far as9
from which it is9
for a length of9
in the modern seas9
the belief that the9
the furnaces in which9
characterised by the possession9
lead is liquated from9
upon the surface of9
so as to form9
geological survey of great9
to the eocene period9
a great thickness of9
and half an uncia9
in mind that the9
of the type of9
in which it was9
the groups of the9
the death of the9
is seen to be9
which are made of9
at an elevation of9
species have been described9
in the lower miocene9
the class of the9
is probable that the9
have been derived from9
the number of the9
so as to be9
the first is the9
is the distribution of9
to the nearctic region9
to the depth of9
and tierra del fuego9
above the level of9
the slope of the9
the bowels of the9
and a species of9
three palms and as9
all temperate and tropical9
the discovery of a9
occur in the upper9
from the point of9
the classification of the9
is made of a9
on the continent of9
the introduction of the9
the under surface of9
resemble those of the9
the effect of the9
a consideration of the9
accounted for by the9
mexico to la plata9
of the ethiopian and9
a careful study of9
and mode of formation9
the whole of it9
where there is a9
in allusion to the9
depth of the shaft9
strictly confined to the9
at a depth of9
south america and australia9
is certain that the9
to the absence of9
level of the sea9
primary divisions of the9
from which tin is9
more than half a9
they belong to the9
wading and swimming birds9
which is turned by9
cut off from the9
under the influence of9
of the secondary period9
the whole region ethiopian9
all over the globe9
the remains of which9
is to be remembered9
to be observed that9
the conditions under which9
quarters of a libra9
of the tunnel and9
it may be mentioned9
separated from the silver9
are identical with those9
being found in the9
at a very early9
are found only in9
of millions of years9
in the days of9
centumpondium of which there9
far the most important9
large number of the9
for our present purpose9
which i will speak9
the reduction of the9
have been detected in9
there is no such9
it is not improbable9
the gold and silver9
will be seen by9
and it is also9
is added to the9
in proportion to its9
the number of its9
found in the coal9
and of these are9
an uncia of silver9
far south as the9
by the presence of9
the case of a9
of a mass of9
end of which is9
by a number of9
the middle eocene of9
evidence to show that9
species of this genus9
the right side of9
here we have a9
liquation cakes are made9
to the family of9
of the cape verd9
the museum of the9
hearth of the furnace9
these are found in9
of this group is9
they are absent from9
andes of peru and9
they are confined to9
out of the sea9
is separated from the9
most important of these9
the advent of man9
the veins and stringers9
a longer or shorter9
in the upper cretaceous9
may have been the9
animals and plants of9
with a species in9
the mouth of a9
the gold or silver9
be said to have9
settles at the bottom9
end of the second9
and two digits thick9
in the tertiary era9
on page from to9
to the dispersal of9
the forms of animal9
most of them are9
three feet and two9
only a single species9
to the mouth of9
a palm and three9
mexico to peru and9
has been discovered in9
the method of making9
form part of the9
much larger than the9
the cause of the9
to borneo and java9
date back to the9
the pressure of the9
lower silurian rocks of9
the marine beds of9
of the most striking9
so far as to9
and in north america9
as soon as they9
parts of the skeleton9
confined to the oriental9
which seems to have9
within the arctic circle9
central and south europe9
one of the smaller9
in the lower eocene9
the head of this9
been found fossil in9
of the series of9
gold and silver by9
is separated from silver9
the general succession of9
the order in which9
the second set of9
the condition of the9
of an inch in9
feet distant from the9
which we have been9
generalized section of the9
and it may be9
when we come to9
the absence of the9
as far east as9
of animals in the9
and in many cases9
of the lesser weights9
probable past history of9
may be seen at9
four and a half9
fourth part of this9
to a greater or9
the whole region all9
in the first instance9
the power of the9
the seventh transverse wall9
above the sea level9
arm of the sea9
in the formation of9
part of the oriental9
regions of the earth9
only found elsewhere in9
following is the distribution9
represented at the present9
it is not the9
the point of view9
the destruction of the9
as if they were9
from the shores of9
and in the same9
as we have been9
have a wide range9
it is necessary for9
on account of its9
which is confined to9
and a palm long9
point of view of9
in some of these9
ortu et causis subterraneorum9
palms and the same9
at the point where9
number and variety of9
we have been unable9
may be separated from9
the skeleton of the9
have been made to9
it can be shown9
east of the andes9
as if they had9
will speak of the9
east and south africa9
a member of the9
by the researches of9
is composed of two9
imperfection of the record9
to enable them to9
in the book of9
in the rivers of9
now speak of the9
end of the th9
is the occurrence of9
the first description of9
the length of a9
higher forms of life9
the mass of the9
general succession of the9
for some of the9
form a distinct family9
is difficult to see9
elevation of the land9
on some of the9
by one of the9
the first half of9
which i have described9
ranging over the whole9
to the number of9
madagascar and the mascarene9
the rim of the9
the geological record is9
in speaking of the9
of sand and mud9
of a total of9
as early as the9
that some of them9
in the pliocene and8
between australia and south8
the exterior of the8
the general features of8
but there are also8
the present condition of8
the peculiar forms of8
be shown to have8
of which the tap8
a thickness of about8
of phosphate of lime8
known to the ancients8
from the number of8
central and south america8
list of australian genera8
region as a whole8
the larger and more8
in which they occur8
found north of panama8
in making nitric acid8
it was not until8
part of the region8
the north and south8
the affinities of the8
of this group of8
it is not in8
which the greeks call8
as a result of8
if they are not8
the various kinds of8
bones have been found8
australian and oriental regions8
of the most ancient8
to the west indian8
of the stratified rocks8
on the bottom of8
by an appeal to8
rubbed on the touchstone8
and in some of8
there appears to be8
and oriental regions to8
other side of the8
on the side of8
the deposits of the8
of this family are8
the habits of the8
into the head of8
on one side of8
and the whole of8
have now to consider8
the most remarkable and8
to do with the8
characteristic of the ethiopian8
hebrew tradition by thomas8
formed part of the8
science and hebrew tradition8
six feet long and8
the ethiopian region has8
most nearly related to8
the greeks call greek8
now confined to the8
those who wish to8
evidence in favour of8
in such a case8
the contents of the8
at the time when8
to mexico and the8
the tropical parts of8
and the woolly rhinoceros8
same way as the8
off the coast of8
by reason of the8
be separated from the8
of more or less8
parts of the oriental8
the shell of the8
of living and extinct8
a foot and two8
from the face of8
supposed to belong to8
the north of the8
very large number of8
through which it flows8
are wholly confined to8
the disappearance of the8
have taken place in8
is seen in the8
is taken out of8
all regions but austral8
in the books of8
in a letter from8
is found also in8
has a species in8
the present order of8
separated from each other8
by some of the8
more closely related to8
general observations on the8
is fixed to the8
the hangingwall or footwall8
to the upper part8
the temperate parts of8
oriental and neotropical regions8
the royal college of8
distant from one another8
the property of the8
that they are not8
in the atlantic and8
sunk in distinct sockets8
the series of the8
is found to be8
is not in the8
the extensive family of8
two palms long and8
the book of the8
by thomas henry huxley8
present day by the8
of the skull of8
south europe and north8
miles from the coast8
to the arctic regions8
the inside of the8
the upper surface of8
which may be regarded8
the minor triangle is8
has the appearance of8
chronicle of the earth8
far as i can8
but it was not8
the middle part of8
widely distributed over the8
in the later tertiary8
the new zealand fauna8
which i have already8
drum which is made8
the growth of the8
mouth of the shaft8
is two palms and8
genera of the same8
belong to existing species8
met with in the8
the first time in8
the miocene and pliocene8
one species in the8
that they do not8
the more important groups8
sold only in sets8
through which the water8
prior to the th8
it may not be8
on the birds of8
under surface of the8
between them and the8
stones from which tin8
and temperate south america8
study of geographical distribution8
the east and west8
mammalia and birds of8
in a sort of8
or very characteristic genera8
range of oriental genus8
of the higher forms8
of the arctic regions8
and the falkland islands8
in deposits of this8
which is found in8
yet it is not8
of the bellows is8
must be borne in8
and are not considered8
are not found in8
to the order of8
from science and hebrew8
are placed in a8
the higher types of8
of the group of8
been found in a8
peculiar or very characteristic8
in the upper end8
the lower ends of8
are highly characteristic of8
in the eastern states8
to tierra del fuego8
united states and neotropical8
to the upper miocene8
are some of the8
to the height of8
fresh waters of the8
are known to be8
the extent of the8
range beyond the region8
which the name of8
these belong to the8
uncia and a sicilicus8
feet from the second8
came to the conclusion8
illustration of zoology of8
in the last chapter8
represented by a species8
united states geological survey8
right angles to the8
of a foot and8
a peculiar species of8
i have already said8
the present day by8
on the left is8
the reader is referred8
in different parts of8
be considered to be8
are supposed to be8
the new stone age8
appears to me to8
and the rocky mountains8
the study of geographical8
melt in the fire8
after it has been8
in the philippine islands8
well developed in the8
and that it was8
the shore of the8
but not in the8
is not the case8
it might have been8
of four siliquae each8
can be said to8
three feet in length8
of the vertebral column8
in a position to8
to speak of the8
the plants and animals8
and three digits thick8
seems to me that8
general conclusions as to8
than they are now8
of the foregoing chapter8
to the rocky mountains8
in the permian period8
palms wide and thick8
three palms and a8
to the region are8
all continents but australia8
of the animals which8
which constitutes this family8
nearly the whole of8
was one of the8
it has been already8
is represented in the8
seems to be no8
imperfection of the geological8
similar to that which8
possessed the power of8
to have been found8
the copper and lead8
the same height as8
number of species in8
the crucible with a8
a foot in diameter8
as a means of8
of three or four8
the same time that8
the origin of man8
are very characteristic of8
is not necessary to8
the water which has8
some of them were8
of silver and copper8
in the pliocene period8
which they have been8
if there is any8