   LET THE OCEANS SPEAK

   by Harold Camping

Introduction
1>  The Oceans - A Key to the Past
2>  Time Schedule Based on Ocean Water
3>  A Look at Sediments
4>  Another Look at Sediments
5>  Ocean Sediments Analyzed
6>  Summary
7>  TABLE I - Elements in Sea Water and in the Earth's Crust
8>  TABLE II - Residency Periods for Chemicals in Ocean Solution
9>  References

Copyright 1982 by
Family Stations, Inc.
290 Hegenberger Road
Oakland, California  94621

   INTRODUCTION

   Creationists are certain that the Bible is accurate, authoritative
and trustworthy in every field of knowledge, whether that be
theological, historical, scientific or any other.  The Bible contains a
definite and precise chronological timetable that begins with the
creation of this world and the first man, Adam, and covers the great
historical events of the first 11,000 years  of history.(1)

   Actually, evidence in the secular record is not at all in
disagreement with the sacred record, and the sacred record can be used
to place the secular record in proper perspective.  Because the Bible
is true and accurate in its accounts of people, places and time, men
can use it to distinguish between what is true and false about the
secular viewpoints.

   Data from the observable universe concerning the earth's past
history is becoming increasingly available as men search out the
secrets of the universe.  But is the world far older than 13,000 years
as deduced from Biblical evidence?  Can creationists really expect to
find correlation between the Biblical and secular records if they
insist on the literal interpretation of the creation story and the
flood account?  Isn't the evidence for a world that is billions of
years old so conclusive that it is hardly possible even to expect
complete reconciliation between the Bible and true science?

   A point must be emphasized.  Because this world is under the bondage
of decay, with much of the record confused and obliterated  by storms,
floods, decay, fire, pestilence, etc., modern man cannot expect to
resconstruct the history of the world in a complete and detailed
manner.  But even so, some indication of the timetable of the past
should be obtainable from the secular record.

   The Oceans - A Key to the Past

   In an earlier generation scientists suggested that the oceans might
be of real help in determining the age of the earth.  After all, the
seas completely surround the land masses and thus receive the output of
the rivers that flow into them.  The rivers carry sediment and
chemicals in solution which have eroded from the continents.

   Scientists have assumed, therefore, that most of the chemical
composition of ocean water is derived from the weathering of rocks. 
Sverdrup et al wrote: "According to present theories, most of the solid
materials dissolved in the sea originated from  the weather of the
crust of the earth."(2)

   H.  Kuenen wrote in 1965: "Apart from meteoric dust and gaseous
matter, the ultimate sources of all sediments are igneous  and
metamorphic rocks."(3) And Kuenen continued:

   Ground water containing dissolved matter including
   silica, calcium, sodium, iron, magnesium, phosphorus,
   humic acids, etc., reaches the sea by way of rivers, or
   directly by seepage along the shore.  Apart from gases,
   including carbon dioxide, derived directly from the
   atomosphere, this is the main source of dissolved matter
   in the sea water .  . . A minor contribution comes from
   volcanic exhalations and from the expulsion of sea water
   trapped between the grains of the older marine
   sediments.(4)

   Thus today scientists expect that much of the past history of the
earth can be deduced from the chemical content of the oceans. For
instance, the salt NaCl is the most abundant constituent of sea water,
and both Na and Cl are present in the rocks.

   Therefore scientists have supposed that a knowledge of the amount of
NaCl in the sea, compared with the amount entering the seas each year
by the weathering of the land, would give a close approximation of the
age of the earth.  An earth age of about 100 million years was
estimated by earlier scientists by following this assumption.

   But other dating methods have been developed.  Based on radioactive
decay analysis, scientists have decided that the earth must be
approximately 4.5 billions years old.  The age of millions of years
deduced from the ocean evidence was decisively rejected in favor of the
longer radioactive ages.

   Supposedly a much more acceptabe timetable was gained for all of the
developments imagined by evolutionists.  Very little is heard today
from researchers investigating the content of sea waters as far as
total earth dating is concerned.

   But the oceans still exist.  Since this world is presumably more
than 4 billions years old, and since oceans as well as continents have
existed continuously, certain relationships and equilibriums must exist
between the continents and the oceans.

   Contentions of earlier scientists about an earth-ocean time
relationship should still be valid.  Assuming that present natural
phenomena are a key to the past, examination of the relationship of the
materials of the continents to those of the oceans should result in
some kind of a timetable for geological history.

   Time Schedule Based on Ocean Water

   As noted, geologists concluded that the chemical composition of sea
water and the ocean floor sediments is principally a product of the
weathering of continental rocks.  If this weathering of rocks was a
very short time phenomenon, then one would expect to find far different
proportions of elements in sea water than are found within the average
rocks of the continents.

   This seems logical since some rocks erode more easily than others,
and therefore easily erodable chemicals should be most abundant in sea
water.  Differences in relative chemical proportions would also be due
to other variables, such as the fact that some elements are not as
readily transportable by rivers and ocean currents as others, and some
are less soluble in water than others.

   Nevertheless, if the duration of erosion was long enough, elements
in the sea water and on the sea floor should quite accurately coincide
with the chemical content of continental masses.  Even the hardest of
rocks would be eroded, and even the least transportable of minerals
would ultimately be carried by the rivers to the sea.

   Thus when scientists talk about millions of years, on a world-wide
basis, the proportion of one element in the sea water and on the sea
floor to all other elements in the same environment should be
approximately the same ratio as that element to all other elements in
the continental masses, for in a very general way all the mass must
shomhow be conserved.  For example, if the  percentage of silicon in
the continental masses is 27.5%, then if the oceans were old enough,
the total of all the silicon in the ocean water and on the ocean floor
should be 27.5% approximatey.

   Furthermore, if the total quantities of various elements in the seas
and sea floor and the approximate rate of world-wide erosion could be
known, then the length of time required to bring present elements into
the ocean could be estimated.  In turn, an approximate age for the
earth might be deduced.

   Fortunately, scientists have determined rather accurately the
chemical composition of both the sea water and the land masses.
Sverdrup et al prepared a table (Table I)(5) showing the amounts of
various chemicals that should have entered the oceans during a period
of 260 millions of years.  This is the estimated length of time which
would be required to provide the present quantity of salt in the ocean
water, assuming uniform weathering throughout this period of time.

   He mentions an estimate by Goldschmidt in 1933 that accumulation of
the present concentration of salt (NaCl) in solution would have
required weathering of 600 grams of rock for each kilogram of water in
the ocean.  Thus according to Table I, 17,000 mg.  (17 gr.) of sodium
were released and 165,000 mg. (165  gr.) of silicon were likewise
released for accumulation in the oceans for each 600 grams of rock
weathered.

   With this estimate of potential elements available, one wonders what
is the actual quantity of elements in sea water.  An estimate for each
element is given in the second column of Table I.

   For example, in a kilogram of sea water there is on the average
about .5 mg.  of aluminum in solution. This is only .001% of the
estimated 53,000 mg.  expected if weathering had continued for as long
as 260 million years, the estimated time required to provide the
observed amount of salt.

   In fact, after close examination of all the elements listed in Table
I, one concludes there is a total lack of relationship between the
chemicals in the oceans and the continents.  For example, chlorine is
67 times too prevalent in sea water, nickel is 500,000 times too
scarce.  Silicon, which is one of the most common constituents of
rocks, should be 50,000 times more plentiful in ocean water if it were
in proportion to that in continental rocks.

   Perhaps one reason for this total disproportion between the expected
volumes of elements in the sea water and their actual occurrence is
that sea water will hold in solution only a tiny bit of each element. 
In other words, most of the silicon goes out of solution to the sea
bottom either by precipitation or by the action of organisms.  That sea
water is not saturated with silicon is supported by F.A.J.  Armstrong:

   Sea water is undersaturated with respect to silica,
   although since reported values for its solubility are
   somewhat inconsistent, it is not possible to say how
   much.(6) And Kuenen has written:
   Under normal conditions sea water is not supersaturated
   with any product, and circulation is automatically set up
   in areas of excess evaporation, preventing the formation
   of excessive concentrations.(7)

   Apparently, then, many elements are far too insufficient in ocean
water as compared with the quantities that should be present if the
oceans were millions of years old.  And further, the sea water in
general is not saturated with chemical elements.

   Therefore the oceans could be very young, because if the oceans had
existed long enough, those elements which are especially soluble would
have reached a saturated condition in many parts of the world.

   Using the unsaturated condition of the oceans, researchers should be
able to measure the age of oceans since an estimate can be made of the
average annual quantity of chemicals flowing into the ocean from the
rivers.  Dividing the total quantity of an element existing in an
unsaturated condition in ocean solution by the quantity of the same
element flowing into the ocean should result in some concept of the
ocean's age.

    This information is found in Table II.(8) Evidently 2.0 x 10^7 (20
million) years of continental weathering would have been required to
supply all the lithium (Li) presently found in ocean solution. 
Presumably, sodium (Na) would have been accumulating for some 2.6 x
10^8 (260 million) years.

   Nevertheless, a very strange fact becomes evident upon careful study
of Table II.  Some of the elements are in very short supply in the
oceans.  Therefore only 100 years of continental weathering would have
been required for accumulation of the tiny quantity of aluminum in
ocean solution.  In fact, nineteen of the elements in sea water are
found in such small amounts that the concentrations could have
accumulated in 1,000 years of continental weathering. Two conclusions
are possible from this startling information:

   l.  The oceans must be very young because small quantities of many
of the elements are in solution.

   2.  The oceans must be very young because of the wide discrepancy of
residency periods of various chemicals. Differential erosion over a
relatively short period of time together with other variables, such as
water transportability and solubility of elements, could account for
this wide spread in residency times.

   One other fact should be noted in this regard.  Chlorine, sulphur,
bromine and boron exist in much larger amounts (See Table I) than those
which would be supplied while the elements, such as sodium, with which
they are normally associated, were being weathered from rocks into the
ocean waters.  Therefore a third conclusion is possible:

   3.  That salt (NaCl) and perhaps a number of other chemicals are in
the oceans completely apart from normal rock weathering.

   A Look at Sediments

   But the question concerning the paucity of elements in sea water
still persists.  Because of the paucity of so many of the chemicals in
the oceans, one might conclude that they must have been taken out of
solution in some manner, even though sea water does not appear to be
with many, if any, of the chemicals that enter it.

   Now the mechanisms of solution in, and the removal from, sea water
are rather complex.  Scientists are busily engaged in attempting to
understand them.  But if the chemicals are not in the sea water, they
must be on the sea floor.

   Therefore, even though the chemicals in the water are not
proportional quantitatively to those in the rocks, surely the remainder
would be found on the sea floor, with the overall chemical content
reflecting an ancient ocean.  Such expectation, however, cannot be
supported by the facts.

   Obviously much more work must be done before a complete analysis of
the quantity and composition of the sea floor sediments can be known. 
However, many cores have been taken already, and there is much
literature available concerning this question.

   Present knowledge is summed up perhaps in the comment of H. Kuenen:
"The differences in composition between oceanic and continental
sediments, both as to major constituents and trace  elements are
large."(9) In other words, whether the composition of sea water or the
composition of the ocean sediments is studied, no data has been
collected yet to substantiate a long time relationship between the
oceans and the continents.  Wilson sets forth these problems:

   The failure to recover any rocks older than Creataceous
   from the ocean floors suggests that the ocean basins may
   be younger than the continents.  It has also become
   evident that the petrology, sedimentations, and
   structural geology of ocean chasms are quite different
   from these of continents .  . .the ocean basins and
   oceanic islands are dramatically different from
   continents in crustal thickness, age, composition, ore
   deposits, structures, magnetic anomalies, and in the
   patterns and characteristics of their active mountain
   belts and earthquakes.  Several continents have rocks at
   least 3.2 x 10^9 years old, which is 20 times the age of
   the oldest oceanic island, dredging, or core.(10)

   Thus, because of the tremendous chemical disproportions between the
oceans and the continents, the most probable conclusion is that the
oceans are very young.

   Another Look at Sediments

   But let us now examine the ocean sediments from another aspect.  If
the annual amount of sediments flowing by rivers into the ocean basins
and some idea of the volume of sediments on the ocean floor are known,
division of the second quantity by the first should result in an
approximate age of the oceans.  Or to put it another way, if the annual
quantity of sediments flowing into the ocean is known, this figure
could be multiplied by, say,  100 million years, 4.5 billions years, or
any other length of time which supposedly approximates the age of the
earth, and then the average thickness of sediments on the ocean floor
could be estimated.

   Let us compute the thickness of sediment that should be found if the
oceans were 260 million years old as deduced in accordance with the
salt content.  Calculations of the quantities added to the oceans by
the rivers of the world will be considered first.

    Clarke (11) has estimated that the rivers contribute 2.73 x 10^15
grams of dissolved solids to the sea each year.  A total of  7.1 x
10^23 grams of solids would have been dissolved in the 2.6 x 10^8 years
required presumably for the present sodium to accumulate.  Of this
total, 5 x 10^22 grams are presently in solution (12) in the ocean
water.

    Therefore (71.0 x 10^22 ) - (5 x 10^22 ), or 66.0 x 10^22 grams,
should have gone out of solution and become part of ocean sediment.  A
small part of this may have been recycled due to  ocean spray, etc.,
but the major part must still be present somewhere in the oceans.

   This estimate of 66 x 10^22 grams of sediment might be checked by
approaching the question from another viewpoint.  Sverdrup et al
reported (13) some estimates by Goldschmidt.  According to Goldschmidt,
for the present concentration of salt (NaCl) to accumulate in ocean
solution, a total of 600 grams of rock has been weathered for each
kilogram of water in the ocean.  This is the basis upon which Table I
was developed.

   Since there are 278 kg.  of water for each square centimeter of  the
earth's surface, and the area of the earth's surface is 5.1 x  10^18
cm^2 , the total weight of water equals 278 x 5.1 x 10^18 kg., or 1.42
x 10^21 kg.

   Goldschmidt estimated further that for every 600 gr.  of rock that
have been weathered, 65% or 390 grams actually should have become
available for solution in the oceans or as sediment on the ocean floor.
 This equals 390 x 1.42 x 10^21 grams = 5.53 x 10^23 grams.

   Since 5 x 10^16 metric tons or 5 x 10^22 grams are in  solution, the
amount that must have become sediment equals (55.3 x 10^22) - (5 x
10^22) or 50 x 10^22 grams.  This is very close to the 66 x 10^22 grams
based on Clarke's estimate of river sediments.

   With the knowledge that there are presently an estimated 5 x 10^22
grams of chemicals in ocean solution and at least another 50 x 10^22
grams in sediments (based on an ocean age of 260 million years), let us
determine what the ocean floor should look like. Sverdrup (14)
estimated that, if the 5 x 10^22 grams of chemicals, which are
presently in ocean solution, could be extracted, then a layer of salts
45 meters thick over the entire earth would result.  Since the oceans
cover 70.8% of the earth's surface, this hypothetical layer would be
63.5 meters thick on the ocean floor.

   Since sediments equal to a minimum of 50 x 10^22 grams would
accumulate in an ocean 260 million years old, then one could  expect an
average sediment depth of ten times 63.5 or 635 meters or 2,100 feet
(with the ocean area the same), that is, if the continents had been
weathering uniformly for 260 million years.

   Since the continents presumably have been here far longer (minimum 3
billions years), one could expect logically that the sediments should
be far deeper than 635 meters.  In fact, in that time the oceans should
have almost filled up, and the land should have pretty well been eroded
to level plains.

   Conceivably these figures would have been changed some by presumed
mountain building some hundred million years ago, but the basic concept
of the oceans filling with sediment as the land masses eroded should
hold true.

   Ocean Sediments Analyzed

   Let us now examine the evidence as far as the ocean sediments are
concerned.  In 1949 Maurice Ewing wrote in the National Geographic
Magazine concerning the exploration of the floor of the Atlantic Ocean.
His comments are as follows:

   In more than 3,000 places over vast areas of the Atlantic
   we have now measured with sound echoes the depth of the
   sediment on top of the bed-rock of the ocean floor.
   These measurements clearly indicate thousands of feet of
   sediments on the foothills of the Ridge.  Surprisingly,
   however, we have found that in the great flat basins on
   each side of the Ridge this sediment appears to be less
   than 100 feet thick, a fact so startling that it needs
   further checking.(15)

   Much of the Pacific floor, too, is covered by sediments under  100
meters in depth, (16) with some areas as thin as 20 meters.(17) The
following statement relates to investigation of the East Pacific Rise:

   A deep-towed magnetometer profile made across the East
   Pacific Rise crest shows sediment accumulation increases
   from less than 2 meters at the rise crest axis to about
   20 meters at the western end and 10 meters at the eastern
   end of the profile.(18)

   Evidence from the oceans, it seems, may not be used automatically to
support the view of a very old earth.  In fact, the opposite conclusion
seems to be better supported. Patrick M. Hurley wrote in the Scientific
American:

   The topography of the ocean floors has been rapidly
   revealed in the past two decades by the depth recorder...
   It became a great puzzle how in the total span of earth's
   history only a thin veneer of sediment had been laid
   down.  The deposition rate measured today would extend
   the process of sedimentation back to the Cretaceous
   times, or 100 to 200 million years, compared with a
   continental and oceanic history that goes back at least
   3,000 million years.  How could three-quarters of the
   earth's surface be wiped clean of sediment in the last 5
   per cent of terrestrial time?  Furthermore, why were all
   the oceanic islands and submerged volcanoes so young?(19) 
   Kuenen wrote:

   Two great problems challenge earth sciences in this
   domain.  The huge wedge of terrace sediment underlying
   the shelf off the east coast of the United States has
   been built up in little more than 10^8 years, that is in
   less than 2 or 3 per cent of geological time.  What has
   happened to the terraces that must have been produced
   earlier?  Have they subsided into the mantle and been
   absorbed; have they been pushed under the continents; or
   have they been incorporated into mountain chains?  The
   second problem is the discrepancy between the estimated
   thickness on the deep sea floor, and the values actually
   found.  Various suggestions have been offered?  (1) the
   layers below the unconsolidated sediment are mainly
   consolidated deposits; (2) the rate of sedimentation has
   been much slower than in recent times, especially in
   pre-tertiary times; (3) creep of the sea floor under the
   continental blocks under the influence of convection
   currents in the mantle; (4) the ocean floor is relatively
   young; (5) the sedimentary carpet has been invaded from
   below and metamorphosed so completely as to become basic
   rock.(20)

   Here, then, is a great enigma.  If the oceans are only hundreds of
millions of years old, sediments averaging 600 or more meters (2,000
ft.) should be found all over the ocean floor. Instead, sediments are
found normally to be far less than this, and in many cases the ocean
floor is almost bare of sediment.  No idea, other than that of a very
young ocean, has thus far been set forth that seems as plausible or
direct; and if the age of the earth were billions of years, then the
puzzle of the missing ocean sediments is increased enormously.

   

   Summary

   The following truths summarize this study:

   l.  A great discrepancy exists between the three or four billion
year age date derived from radioactive decay data and the evidence
obtainable from the oceans.  Either the ocean data is completely
untrustworthy, or there is a question regarding the dependability of
the radioactive dating.

   2.  If the accumulation of sodium by the weathering of continental
rocks as a part of NaCl in the oceans is used as a guide for the age of
the oceans, a number of unanswerable problems remain:

   a.  Some chemicals, (Cl, Br, etc.), must have been a part
   of the oceans since the very beginning or must have been
   introduced apart from rock weathering.
   b.  The sediments in the ocean should be much thicker
   than actually found.
   c.  Almost all the other elements which supposedly
   weathered while the sodium was weathering are in far too
   short supply to allow for a weathering period of 260 million
   years, which is required to bring this amount of sodium into
   oceans.  Therefore, using NaCl as a standard results in an
   untenable solution.

   3.  If accumulation of the other major constituent of the ocean
salts, chlorine, is used as a guide for age dating, then the following
points would obtain:

   a.  An accumulation period of about 2 to 3 billions of
   years would result.  This is much closer to the radioactive
   age determination.  The ocean can then be considered to have
   been devoid of chemicals in solution at one time in its
   history.

   b.  This would compound the sediment problem. In this
   long period of time the oceans would have filled with
   sediment.

   c.  This also provides no answer for the short supply of
   many of the ocean chemicals.  This, too, gives an untenable
   solution.

   4.  If the accumulation of the very smallest amounts of chemicals is
used for age dating, the following would obtain:

   a.  The apparent age of the ocean would be under 1,000
   years.
   b.  The ocean would have begun with essentially the
   present compliment of salt and several of the other
   chemicals.  This solution is untenable on the basis of other
   histories.

   5.  Another conclusion remains as the only plausible one, both in
the light of Biblical statements, as well as in the light of the
evidence obtained from studies of the oceans.  That conclusion is that
the ocean and the earth are 13,000 years old.  This conclusion may be
supported by the following secular evidences:

   a.  Elements in the ocean water are not found in a
   saturated condition.  From this, one could deduce the flow
   of chemicals into the ocean was a short-time phenomenon.
   b.  Proportions of elements found in the water or on the
   ocean floor are in no relationship whatsoever to the
   proportions found in the continents.  Such variables as
   resistance to erosion, water transportability, solubility,
   and others, over a very short period of weathering accord
   with these extreme differences in chemical proportions.
   Again, the conclusion seems most logical that the oceans are
   very young.
   c.  The fact that many of the chemicals in ocean solution
   are present in amounts that could have accumulated within
   the last 1,000 years or less, if all rocks were equally
   susceptible to erosion, can be used dramatically to support
   a 13,000 year age of the earth.  For this is precisely what
   would be expected in view of the differences in erosion
   resistance, solubility, etc. of the continental rocks.
   Elements in excess of those expected within 13,000 years
   could have accumulated from easily eroded rocks, whereas far
   less than that expected in 13,000 years of history would
   have accumulated from very hard rocks.
   d.  The concept of a very young earth is supported also
   by existence of a thin layer of sediments on the ocean
   floor.  This is especailly true when consideration is given
   to the cataclysmic worldwide flood of Noah's day.  That
   phenomenon alone could have caused erosion of enormous
   quantities of sediments for ocean solution and deposition.
   In fact, impact of a worldwide flood upon the oceans would
   have been so severe that no accurate estimate of time can
   ever be derived from ocean chemicals.
   e.  The fact that certain salts such as NaCl are in such
   abundance in ocean solution could be interpreted to mean
   that they have been present in essentally their present
   quantities from the very beginning.

   The all-important conclusion remains, however, that even without
considering the effect of the flood on the oceans, under no
circumstance may the ocean evidence be used to deduce an age of
millions of years.  Then, when any recognition is given to the Noachian
flood sediments which must be subtracted from the elements in the
oceans, the contention for a very young ocean may be stated even more
emphatically.  The 13,000 year date of the Bible appears to be the
only true alternative to popular concepts of a very old earth.

   TABLE I

   Elements in Sea Water and in the Earths Crust

Element         Sea Water     Potential "supply"       Percentage
                              in 600 gr. of rock       in solution
                             (mg/kg of sea water)
Silicon             4             165,000                  0.002
Aluminum            0.5            53,000                  0.001
Iron                0.002          31,000                  0.0001
Calcium           408              22,000                  1.9 
Sodium         10,769              17,000                 65
Potassium         387              15,000                  2.6
Magnesium       1,297              13,000                 10
Titanium           --               3,800                  ?
Manganese           0.01              560                  0.002
Phosphorus          0.01              470                  0.02
Carbon             28                 300                  9
Sulphur           901                 300                300
Chlorine       19,353                 290              6,700
Strontium          13                 250                  5
Barium              0.05              230                  0.02
Rubidium            0.02              190                  0.1 
Fluorine            1.4               160                  0.9
Chromium            p                 120                  ?
Zirconium          --                 120                  ?
Copper              0.01               60                  0.02
Nickel              0.0001             60                  0.0002
Vanadium            0.0003             60                  0.0005
Tungsten           --                  41                  ?
Lithium             0.1                39                  0.2
Cerium              0.0004             26                  0.002
Cobalt              p                  24                  ?
Tin                 p                  24                  ?
Zinc                0.005              24                  0.02
Yttrium             0.0003             19                  0.002
Lanthanum           0.0003             11                  0.003
Lead                0.004              10                  0.04
Molybdenum          0.0005              9                  0.005
Thorium             0.0005              6                  0.01
Cesium              0.002               4                  0.05
Arsenic             0.02                3                  0.7
Scandium            0.00004             3                  0.001
Bromine            66                   3              2,000
Boron               4.7                 2                240
Uranium             0.015               2                  0.8
Selenium            0.004               0.4                1
Cadmium             p                   0.3                ?
Mercury             0.00003             0.3                0.001
Iodine              0.05                0.2               25
Silver              0.0003              0.06               0.5 
Gold                0.056               0.003              0.3
Radium              0.093               0.066              0.05

   TABLE II

   Residency Periods for Chemicals in Ocean Solution (in years)

Lithium       2.0 x 10^7           Silver             2.1 x 10^6
Beryllium     150                  Gadolinium         5.0 x 10^5
Sodium        2.6 x 10^8           Tin                1.0 x 10^5
Magnesium     4.5 x 10^7           Antimony           3.5 x 10^5
Aluminum      100                  Cesium             4.0 x 10^4
Silicon       8.0 x 10^3           Barium             8.4 x 10^4
Potassium     1.1 x 10^7           Lanthanum          440
Calcium       8.0 x 10^6           Cerium              80
Scandium      5.6 x 10^3           Praeseodymium      320
Titanium      160                  Neodymium          270
Vanadium      1.0 x 10^4           Samarium           180
Chromium      350                  Europium           300
Manganese    1400                  Gladolinium        260
Iron          140                  Dysprosium         460
Cobalt        1.8 x 10^4           Holmium            530
Nickel        1.8 x 10^4           Erbium             690
Copper        5.0 x 10^4           Thulium           1800
Zinc          1.8 x 10^5           Ytterbium          530
Gallium       1.4 x 10^3           Lutetium           450
Germanium     7.0 x 10^3           Tungsten            10^3
Rubidium      2.7 x 10^5           Gold               5.6 x 10^5
Strontium     1.9 x 10^7           Mercury            4.2 x 10^4
Yttrium       7.5 x 10^3           Lead               2.0 x 10^3
Niobium       300                  Bismuth            4.5 x 10^4
Molybdenum    5.0 x 10^5           Uranium            5.0 x 10^5
                                   Thorium            350

   REFERENCES

(1)  Camping, Harold. 1970.  The Biblical calendar of history, 
Journal of the American Scientific Affiliation, September, p. 98. 
(2)  Sverdrup, H. U., Martin W. Johnson, and Richard H. Fleming, 
1942. The Oceans, Prentice Hall, Inc., New York, p. 219. 
(3)  Kuenen, H. 1965. Geological conditions of sedimentation (in) 
Chemical Oceanography, Riley, J.P. and G. Skirrow. Editors. 
Academic Press, London and New York, Vol. 2, p.1. 
(4)  Ibid., p.4.
(5)  Sverdrup, H. U., Op. cit., p.220,
(6)  Armstrong, F.A.J. 1965. Silicon (in) Chemical Oceanography, 
Riley, J.P. and G. Skirrow. Editors. Academic Press, London and 
New York, Vol.2, p. 410. 
(7)  Kuenen, H., Op. cit., p. 5.
(8)  Kuenen, H., Op. cit., Vol. 1, p. 164.
(9)  Kuenen, H., Op. cit., p. 20.
(10) Wilson, Teyo J. 1967.  Theories of building of continents 
(in) the Earth's Mantle. T. F. Gaskell, Editor. Academic Press, 
London and New York, p. 447.
(11) Sverdrup, H. U., Op. cit., p. 172.
(12) Ibid., p. 219.
(13) Ibid., p. 219.
(14) Ibid., p. 219.
(15) Ewing, Maurice.  1949. New discoveries on the mid-Atlantic 
ridge, National Geographic Magazine, November, p. 612, 613.
(16) Ewing, John et al.  1968. North Pacific sediment layers 
measured by seismic profiling, The crust and upper mantle of the 
Pacific area, William Byrd Press, Richmond, VA, p. 150, 165.
(17) Ibid., p. 148.
(18) Larson, Roger L. and Fred N. Spiers. 1969. East Pacific rise 
crest, a near bottom geophysical profile. Science, January 3, p. 
68. 
(19) Hurley, Patrick.  1968.  The confirmation of continental 
drift, Scientific American, April.
(20) Kuenen, Op. cit., Vol 2, p. 20.
