THE SUMMER OF 1873.
1. The time crept away with indescribable monotony. The crew performed
their heavy labours, but of events there were none. The only change in
our position was the constant decay of the buttresses and walls of ice,
until the frozen sea lay like a snowy chaos before us. Pure sharp-edged
ice was nowhere to be seen; the edges were no longer transparent;
evaporation had transformed the surface into a kind of glacier-snow.
June 1, we had the greatest degree of cold of the month, the thermometer
marking 13° F.; but on the last day it rose to 32·2° F.; the mean
temperature being 31·1° F. Every week brought us promises of summer. On
the 1st the black-bulb thermometer reached 98° F.; on the 14th rain fell
for the first time; on the 16th the temperature at 9 o’clock A.M., was
41·5° F., on the 26th 46·4° F., and on the 29th even 50·2° F. On these
days the air seemed to have the pleasant mildness of southern climes, and
when there was no wind we felt an oppressive sultriness. Wreaths of mist
moved along the icy wastes which glowed with sunlight, while the long
dark lines of ice-wall lay in deep shadow. The air was filled with flocks
of birds; day and night we heard the shrill cries of the Robber-gulls,
ever and anon mingled with the barking of the dogs in full pursuit of
them. Flocks of rotges congregated without fear in the narrow basins of
distant “leads;” and the “great gulls,” shunning companionship, sat for
hours on the top of an ice-cliff, or in the middle of a floe.
2. No one who has not actually seen it, can imagine the blaze of light
in the Arctic regions on clear days, or the glow which floats sometimes
over the cold white ice-floes, with their outlines in constant vibration,
while refraction transforms the icebergs into a variety of shapes. The
sun’s power is sometimes so great as to blister the skin in a few hours,
and the glare from snow and ice produces snow-blindness, if the eyes be
not carefully protected. At a little distance the sea appears to be of a
deep black colour, though it still preserves its ultramarine hues in the
narrow “leads;” even the pure blue of the heavens may be called almost
black when compared with the dazzling sheen of the ice. In the middle
of June there was an incessant dripping and oozing in the ice-world,
and streams of thaw-water flowed into the open fissures. By the end of
the month the surface of the ice resembled snow; and even at some depth
it was viscous, instead of brittle and hard as glass, as it is during
the colder season. Streams of thaw-water ran through the softened and
saturated snow. Small lakes were formed on the levels, and swamps of
snow, wearing a traitorous exterior, surrounded their borders. In the
summer of 1873 we observed a vertical decrease of five or six feet in
the thickness of the ice; but this diminution in thickness was from
the surface downwards, while in the sea itself there was little or no
thawing, because the temperature of its surface was still below zero. The
moisture, from which there was no escape, became exceedingly troublesome.
In spite of our stout leather boots we had never the comfort of dry
feet during the whole of the summer, and this we felt the more, as our
labours to free the ship, which we had commenced at the beginning of May,
necessitated our being constantly amid the snow and ice.
3. At the end of May the ship began slowly to settle, and the water rose
between the ice and the hull on the fore-part of the ship. But we soon
discovered that these small changes would not suffice to free us from our
prison-house, but that we must ourselves endeavour to loosen the fetters
which held us fast, if it were only to banish gloomy thoughts of the
future by action of some kind or other. Hence constant digging, sawing,
and blasting on our floe, through May, June, July, and August—labours
in which the whole crew of the ship, with the exception of the sick
and of the cook, took part; labours, alas! which admonished us of the
impotence of man when he contends against the power of Nature. Only on
the port side of the ship were our efforts to dig through the floe at
all successful; on the starboard side the floe had been so enormously
increased by the tables of ice forced upon one another, that we had not
pierced through the ice after sinking a shaft eighteen feet deep; and at
last the water, forcing itself through the pores of the ice, compelled
us to desist from the labour of sinking deeper. The process of sawing
was possible only where we had broken through the ice—that is, on the
port side; yet even there the great thickness of the floe necessitated
the construction of longer instruments, for which the iron casing of
the engine-room had to furnish the material. The difficulty of sawing
increases with the thickness of the ice in an almost incredible manner.
It is easy enough to cut through a floe, four or five feet thick, but to
break up one, eight or ten feet thick, is a matter of great difficulty.
Our saws too, even when they were lengthened, permitted a play of only
a foot; and their twisting, as they cut deep, proved a great hindrance.
Besides, when we had cut to the depth of a fathom, the saws were always
frozen fast, and when we attempted to free them by blasting they were
very often broken in pieces. But even the sections, made with so much
difficulty, often proved to be quite useless, as they were frozen
together again by broken ice left in the cut. Blasting with gunpowder
proved as ineffectual as in the previous year; in fact, the process was
only applicable to ice-blocks which had been loosened by sawing, and
which could not be broken up by the crow-bar alone.
4. By the middle of June we were at last convinced that the thickness
of the ice rendered it impossible to join together, by sawing, the
two-and-twenty holes which we had dug out round the ship. Henceforward
our labours were confined to the formation of a basin at the fore-part of
the ship. Although we saw the impossibility of liberating the vessel, as
long as she rested on a mountain of ice, we hoped that the basin would
help to break up the floe, and that the _Tegetthoff_ would of itself
return to its normal position. The gliding down of the ship, raised as it
was, to its natural water-line might indeed easily end in a catastrophe,
but we braved this peril when we thought of the vain attempts we had
made to free her. Though the ship sunk so much in the course of the
summer, that its height above the water-line was a little more than two
feet in the fore-part of the ship, and three feet in the after-part,
this circumstance in our favour was outweighed by the disadvantage of
the rapid melting away of the ice at its sides. The ship, freed from its
covering of ice, stood so high above it, that in order to guard against
the danger of its overturning we were obliged, in the second half of
the summer, to shore it up by strong timbers fastened to its masts. It
looked no longer like a ship, but like a building ready to fall in! In
the middle of July Lieutenant Weyprecht ordered Krisch, the engineer, to
construct heavy chisels and borers to ascertain the thickness of the ice.
After long and hard labour, we found that after boring through several
ice-tables, to a depth of twenty-seven feet, we still struck on ice!
Every attempt, therefore, to break through this accumulation had to be
given up, and we contented ourselves with leading the basin we had formed
on the fore-part round the larboard side of the ship. On the 27th of the
month, twenty tons of coal were removed to the ice, in order to lighten
the ship as much as possible, and every day we had to look to the props
which steadied the ship, as the melting of the ice rendered them unsafe.
In the following weeks, the bows continued to sink into the water, while
the after-part as a natural consequence was raised up.
5. Even in the month of July, the weather was generally gloomy and
unsettled. We had several times two or three inches of snow, and the
showers were mingled with mist, rain, and snow, as had been the case in
June. The winds were generally from the west; the mean temperature of the
month was 34·7° F.; on the 8th of July, the black-bulb thermometer marked
108° F., and the temperature in the shade at the same date amounted to
34° F. But neither wind nor temperature made any change in our position.
The sun on which our liberation depended was seldom visible; and the
winds on which we had counted failed to blow. For weeks we watched for
the formation of fissures round the ship. Fissures indeed were formed,
but at such a distance that they were utterly useless to us. On the 16th
of June, one opened towards the south-east; but it was at least two miles
distant, and in the middle of July it was only half a mile nearer to us.
Nothing, absolutely nothing, was to be seen from the deck but ice, and
Klotz, coming down one day from the top-sail yard, described our position
with a melancholy laconic brevity: “Nix als Eisch, und nix als Eisch,
und nit a bisserl a Wosser. (_Nothing but ice, ice everywhere, and not a
patch of water._)” Amid such impressions all hope gradually left us. The
drifting of the ice ceased to animate our hopes. Even the approach of a
fissure on the 29th of July to the distance of three-quarters of a mile,
in consequence of heavy gales from the south and west, ended in miserable
disappointment. A movement in the ice which began a little way off on the
6th of August resulted only in the diminishing of our floe. There was no
essential change in the remainder of this month, except that the monthly
mean temperature fell to 32·7° F. We had the greatest extreme of heat on
the 4th of August, 41·9° F.; but on the last day of the month we had 5·7
degrees of cold.
6. For some time we had been surprised by the appearance of a dark
mass of ice, the distance of which prevented us from making a closer
acquaintance with it. Our life on the narrow space of our floe had quite
assumed the character of that of mere insects, who dwell on the leaf of
a tree and care not to know its edges. Excursions of one or two miles
were regarded as displaying an extraordinary amount of the spirit of
enterprise and discovery. On the 14th some of us pushed on for about four
miles to the group of ice just mentioned, and discovered it to be a very
large iceberg. Two moraines lay on its broad back. These were the first
stones and pieces of rock we had seen for a long time, and so great was
our joy at these messengers of land, that we rummaged about among the
heaps of rubbish, with as much zeal as if we had found ourselves among
the treasures of India. Some of the party found what they fancied to be
gold (pyrites), and gravely considered whether they would be able to take
a quantity of it back to Dalmatia. Although the glaciers of Novaya Zemlya
could not shed icebergs of such magnitude as that on which we now stood,
we all held it for certain that it had come from thence. Not one of us
had the least presentiment that it could belong to new lands, to which
at that time we were near. Even the other icebergs which we discovered
in increasing numbers on the following days, did not as yet speak to us
the language of a message to fill us with hope and ardour. Our walk to
the “dirt iceberg” was an event in our monotonous life, and was often
repeated. These expeditions enabled us also to form some conception of
the size of our floe, the diameter of which could not be less than six or
seven miles.
7. August 18—the birthday of his Majesty our Emperor,—the ship was
dressed with flags, the only form left to us of expressing our loyalty.
Our dinner was as sumptuous as the circumstances permitted, though
fasting would have been more appropriate, as the third day after this was
the anniversary of that sad and gloomy day on which we were inclosed in
the ice. In order to visit an iceberg which lay to the north-west of us,
we ventured beyond our floe for the first time, and passed over a fissure
to some drifting ice-floes which lay in the way. A seal lying on the ice
was immediately attacked by our dogs, but succeeded after many efforts
in reaching its hole. From the top of the iceberg, which was about sixty
feet high, we discovered that the few openings in the ice were not
navigable “leads,” but isolated holes utterly unconnected, and therefore
useless for navigation.
8. We had continually drifted, since the beginning of February, first to
the north-west and then to the north, with few modifications; at that
date, we had reached our greatest East Longitude, and winds appeared as
before to be the main cause of this drifting. At the end of that month
there was a succession of calms, and we lay almost motionless in latitude
79°, and longitude 71°. The subjoined table shows our change of place in
the following months.
+------------------+-----------+------------+
| Time. | Latitude. | Longitude. |
| | ° ′ | ° ′ |
+------------------+-----------+------------+
| March 3 1873 | 79 13 | 69 32 |
| ” 9 ” | 79 19 | 68 28 |
| ” 14 ” | 79 20 | 68 28 |
| ” 20 ” | 79 33 | 68 52 |
| ” 25 ” | 79 23 | 67 17 |
| ” 27 ” | 79 15 | 67 29 |
| ” 29 ” | 79 14 | 67 35 |
| April 2 ” | 79 5 | 66 49 |
| ” 3 ” | 79 5 | 66 42 |
| ” 7 ” | 79 4 | — |
| ” 10 ” | 79 12 | 68 1 |
| ” 12 ” | 79 19 | 67 43 |
| ” 13 ” | 79 20 | 67 40 |
| ” 15 ” | 79 14 | 67 0 |
| ” 19 ” | 79 18 | 65 51 |
| ” 20 ” | 79 19 | 65 37 |
| ” 27 ” | 79 13·5 | 64 37·0 |
| ” 28 ” | 79 12·2 | 64 41·8 |
| May 1 ” | 79 15·8 | 64 58·8 |
| ” 2 ” | 79 17·1 | 65 3·9 |
| ” 6 ” | 79 16·0 | 65 0·5 |
| ” 10 ” | 79 20·4 | 65 41·9 |
| ” 11 ” | 79 20·2 | 65 32·4 |
| ” 13 ” | 79 19·7 | 65 15·8 |
| ” 14 ” | 79 19·8 | 64 45·6 |
| ” 16 ” | 79 15·5 | 63 39·0 |
| ” 17 ” | 79 13·1 | 63 21·7 |
| ” 22 ” | 79 9·2 | 62 3·5 |
| ” 29 ” | 79 2·4 | 62 55·5 |
| ” 30 ” | 79 2·5 | 62 54·2 |
| ” 31 ” | 79 2·5 | 62 53·9 |
| June 1 ” | 79 2·4 | 62 43·2 |
| ” 3 ” | 79 0·4 | 62 29·7 |
| ” 5 ” | 79 1·3 | 62 24·8 |
| ” 6 ” | 79 1·1 | 62 20·2 |
| ” 9 ” | 79 5·4 | 61 31·4 |
| ” 10 ” | 79 5·3 | 61 23·6 |
| ” 11 ” | 79 4·3 | 61 21·3 |
| ” 18 ” | 79 6·6 | 61 5·2 |
| ” 20 ” | 79 8·6 | 61 2·8 |
| ” 22 ” | 79 9·2 | 60 54·9 |
| ” 24 ” | 79 8·4 | 60 31·8 |
| ” 25 ” | 79 11·2 | 60 14·6 |
| ” 26 ” | 79 13·3 | 59 55·3 |
| ” 27 ” | 79 13·7 | 59 46·0 |
| ” 28 ” | 79 15·5 | 59 35·4 |
| July 3 ” | 79 15·2 | 59 14·8 |
| ” 4 ” | 79 14·8 | 59 13·3 |
| ” 8 ” | 79 15·2 | 59 5·8 |
| ” 10 ” | 79 13·2 | 59 9·0 |
| ” 15 ” | 79 9·8 | 59 52·6 |
| ” 18 ” | 79 7·3 | 59 50·4 |
| ” 19 ” | 79 7·6 | 59 35·1 |
| ” 20 ” | 79 8·7 | 59 33·6 |
| ” 21 ” | 79 9·2 | 59 33·1 |
| ” 22 ” | 79 9·0 | 59 34·1 |
| ” 23 ” | 79 6·6 | 59 34·2 |
| ” 24 ” | 79 7·1 | 59 29·5 |
| ” 25 ” | 79 6·6 | 59 27·3 |
| ” 31 ” | 78 58·5 | 60 25·5 |
| August 1 ” | 78 56·9 | 60 40·6 |
| ” 4 ” | 79 0·4 | 61 6·2 |
| ” 13 ” | 79 25·4 | 61 6·6 |
| ” 14 ” | 79 24·5 | 61 16·3 |
| ” 16 ” | 79 27·8 | 61 7·6 |
| ” 19 ” | 79 29·1 | 61 31·0 |
| ” 21 ” | 79 31·3 | 61 44·8 |
| ” 30 ” | 79 43·0 | 60 23·7 |
| ” 31 ” | 79 42·5 | 60 5·6 |
| Sept. 2 ” | 79 40·2 | 60 32·9 |
| ” 5 ” | 79 41·3 | 60 12·5 |
| ” 8 ” | 79 34·2 | 59 47·3 |
| ” 9 ” | 79 33·6 | 59 45·9 |
| ” 10 ” | 79 32·2 | 59 53·1 |
| ” 16 ” | 79 45·6 | 61 30·5 |
| ” 23 ” | 79 49·6 | 61 58·1 |
| ” 30 ” | 79 58·3 | 60 41·1 |
| Oct. 16 ” | 79 54·6 | 60 34·7 |
| ” 19 ” | 79 53·9 | 60 40·6 |
| ” 23 ” | 79 44·5 | 60 7·9 |
| ” 26 ” | 79 44·3 | 59 17·1 |
| ” 27 ” | 79 44·0 | 59 14·1 |
| ” 28 ” | 79 43·8 | 59 6·6 |
| ” 29 ” | 79 44·8 | 59 9·8 |
| ” 30 ” | 79 49·0 | 58 59·9 |
| ” 31 ” | 79 50·6 | 58 53·7 |
| Ship in Land ice | 79 51·1 | 58 56·0 |
+------------------+-----------+------------+
9. The meteorological observations of the expedition, and the course
of the _Tegetthoff_ have been ably analysed by Vice-Admiral Baron von
Wüllersdorf-Urbair in the _Mittheilungen_ of the Imperial Academy of
Sciences of Vienna, and while I refer the curious reader to these reports
for a fuller discussion of these questions, I subjoin the most important
paragraphs of the Admiral’s report which concern the course of the
_Tegetthoff_:—
“Under ordinary circumstances a ship drifts on with the floe; is
imprisoned, and necessarily obeys the force of the wind and the
sea-currents. Its course, consequently, corresponds to the combined
effect of these forces. But, inasmuch as the _Tegetthoff_ was not in the
free sea, but was driven along for the greater part of the time in close
pack-ice, the ship not only obeyed the general movement of the ice, which
was dependent on the direction of the winds and currents of the sea,
but was also influenced by its vicinity to coasts and by the greater or
lesser accumulation of ice.
“In so far as the _Tegetthoff_ with her hull and masts presented a
greater surface to the wind, the floe, on which it was imprisoned, would
necessarily receive an excess of movement in the direction of the wind.
If this excess formed an angle with the direction of the movement of the
ice, the ship’s floe would deviate to the side of the least resistance,
and drift according to the resultant between wind and resistance. Thus
it might be that the ship’s course deviated from the wind, even in a
direction opposed to it. But these anomalies certainly were not great,
and could not well be estimated, because the deviations which thus arose
depended on the direction of the wind, on the density and mass of the
ice, on causes, in fact, which could not be exhibited under numerical
relations.
“If we compare the statements, as given in the _Meteorological
Journal_,[21] concerning the ice-drift and ice-pressures, it is seen that
the maximum of both occurred in those parts of the sea in which the ship
was within the action of the ice coming from the Sea of Kara, and that
the greatest deviations in the ship’s course necessarily happened there.
“With respect to another abnormal deviation in the ship’s course, it
cannot be doubted that this depended on the vicinity of Franz-Josef Land,
towards which the masses of ice drifted under the action of continuous
south-west winds; and were again driven back, thus forming a circle
in their movement. It would seem natural to assume the existence of a
sea-current in order to explain this peculiarity; but the configuration
of that land and its coasts, or the greater or lesser amount of
immovable ice, or, lastly, the prevailing winds in those regions,
may have influenced the direction of the movement of the ice, and
consequently of the ship’s course.
“If we consider the prevalence of winds, as furnished by Weyprecht’s
observations for more than two years, we find south-west winds prevailing
in the southern part of the seas that were navigated, and north-east
winds in the northern part of those seas.
“If the sea to the east of Franz-Josef Land should not be broken by
larger groups of islands, or by masses of land, but be a vast range of
ocean, the winds would be free from the influence of land, and blow in
a north-easterly direction, and exhibit, so to speak, the phenomenon of
a Polar north-east trade wind. If it should be the case that north-east
winds prevail to the north of the 78th or 79th degree of north latitude,
and, at the same time, south-west winds to the south of that same degree,
the notion of a sea-current must be dismissed, and a revolving movement
in the ice assumed, in the opposite direction to the hands of a clock.
The observations of Weyprecht on these winds establish their circulatory
character. The curve of deviation in the course of the _Tegetthoff_ seems
to be in harmony with this assumption. But these suppositions cannot be
accepted, until observations be made on the winds to the south of 79° N.
L. at the same season of the year with those which were so successfully
made by Weyprecht to the north of this degree.
“The following arguments, however, would seem to favour the supposition
of the existence of a sea-current. The curve at the commencement of its
deviation corresponds pretty nearly with the direction which the Gulf
Stream would take after passing round Norway, and in its further course
with that current, which comes out of the Sea of Kara between Novaya
Zemlya and Cape Taimyr, and which undoubtedly exists, though its course
has to be more accurately determined.
“However small may be the value we assign to the winds in explanation of
the deviation in the _Tegetthoff’s_ course, it is at any rate impossible
to ascribe those phenomena to the influence of the coast formation. We
must, therefore, assume either, that the different directions of the wind
produce a constant circulation of the ice in the sea to the north of
79°; or that currents known to exist in this and contiguous seas cannot
be excluded from the small part of the ocean lying between Novaya Zemlya
and Franz-Josef Land.”
From these and other grounds the Vice-Admiral Baron von Wüllersdorf draws
the following conclusions:—
“It is probable that there exists a sea-current in the seas between
Novaya Zemlya and Franz-Josef Land; that at any rate, its existence
cannot positively be denied, although the prevailing winds may produce
similar phenomena.
“That there is a great probability that the Ocean stretches far to the
north and east beyond the eastern end of Novaya Zemlya.”
[Illustration: SOUNDING IN THE FROZEN OCEAN.]
10. During the summer Orel took soundings of the depth of the sea,
which he was prevented from continuing in the winter by the frost.
These show its shallowness on the north of Novaya Zemlya, especially
towards Franz-Josef Land. A bank, over which we drifted in the summer of
1873, and which we explored with a drag-net, was the principal source
of the collection of marine fauna, which we shall speak of in a later
chapter. These soundings also enabled Orel to prove the small increase
of the temperature of the sea at any considerable depth. He used in his
experiments the maximum and minimum thermometer of Casella. The specimens
we collected showed, that the bottom of the sea consists of layers of
mud and shells. The soundings are exhibited in the following table:—
+----------------+-------+
| Time. |Metres.|
+----------------+-------+
| July 20 1872 | 400 |
| ” 28 ” | 115 |
| ” 31 ” | 250 |
| Aug. 3 ” | 130 |
| ” 4 ” | 80 |
| ” 22 ” | 36 |
| ” 30 ” | 170 |
| Sept. 16 ” | 100 |
| ” 25 ” | 90 |
| ” 29 ” | 85 |
| ” 30 ” | 190 |
| Oct. 2 ” | 170 |
| ” 9 ” | 450 |
| Nov. 14 ” | 345 |
| Jan. 28 1873 | 510 |
| Mar. 27 ” | 450 |
| April 28 ” | 350 |
| May 17 ” | 230 |
| ” 18 ” | 187 |
| ” 19 ” | 172 |
| ” 20 ” | 163 |
| ” 21 ” | 138 |
| ” 22 ” | 186 |
| ” 23 ” | 162 |
| ” 25 ” | 177 |
| ” 25 ” | 182 |
| ” 26 ” | 186 |
| ” 27 ” | 249 |
| ” 28 ” | 251 |
| ” 29 ” | 254 |
| ” 30 ” | 253 |
| ” 31 ” | 256 |
| June 1 ” | 238 |
| ” 2 ” | 210 |
| ” 3 ” | 183 |
| ” 4 ” | 207 |
| ” 5 ” | 200 |
| ” 6 ” | 198 |
| ” 7 ” | 190 |
| ” 8 ” | 215 |
| ” 9 ” | 231 |
| ” 10 ” | 203 |
| ” 11 ” | 240 |
| ” 12 ” | 218 |
| ” 13 ” | 211 |
| ” 14 ” | 235 |
| ” 15 ” | 161 |
| ” 16 ” | 184 |
| ” 17 ” | 222 |
| ” 18 ” | 200 |
| ” 19 ” | 186 |
| ” 20 ” | 220 |
| ” 21 ” | 195 |
| ” 22 ” | 200 |
| ” 23 ” | 169 |
| ” 24 ” | 178 |
| ” 25 ” | 195 |
| ” 26 ” | 220 |
| ” 27 ” | 227 |
| ” 28 ” | 233 |
| ” 29 ” | 240 |
| ” 30 ” | 240 |
| July 1 ” | 240 |
| ” 3 ” | 245 |
| ” 4 ” | 250 |
| ” 5 ” | 235 |
| ” 6 ” | 235 |
| ” 7 ” | 274 |
| ” 8 ” | 266 |
| ” 9 ” | 250 |
| ” 10 ” | 250 |
| ” 11 ” | 236 |
| ” 12 ” | 265 |
| ” 13 ” | 247 |
| ” 14 ” | 215 |
| ” 15 ” | 195 |
| ” 16 ” | 184 |
| ” 17 ” | 200 |
| ” 18 ” | 240 |
| ” 19 ” | 232 |
| ” 20 ” | 231 |
| ” 21 ” | 231 |
| ” 22 ” | 226 |
| ” 23 ” | 198 |
| ” 24 ” | 205 |
| ” 25 ” | 216 |
| ” 26 ” | 218 |
| ” 27 ” | 218 |
| ” 28 ” | 236 |
| ” 29 ” | 260 |
| ” 30 ” | 236 |
| ” 31 ” | 234 |
| Aug. 1 ” | 225 |
| ” 2 ” | 219 |
| ” 3 ” | 173 |
| ” 4 ” | 188 |
| ” 5 ” | 210 |
| ” 6 ” | 107 |
| ” 7 ” | 216 |
| ” 8 ” | 184 |
| ” 9 ” | 244 |
| ” 10 ” | 225 |
| ” 11 ” | 209 |
| ” 12 ” | 214 |
| ” 13 ” | 189 |
| ” 14 ” | 177 |
| ” 15 ” | 170 |
| ” 16 ” | 170 |
| ” 17 ” | 174 |
| ” 18 ” | 148 |
| ” 19 ” | 152 |
| ” 20 ” | 138 |
| ” 21 ” | 130 |
| ” 22 ” | 131 |
| ” 23 ” | 128 |
| ” 24 ” | 145 |
| ” 25 ” | 140 |
| ” 26 ” | 185 |
| ” 27 ” | 219 |
| ” 28 ” | 180 |
| ” 29 ” | 132 |
| ” 30 ” | 211 |
| ” 31 ” | 197 |
| Sept. 1 ” | 260 |
| ” 2 ” | 142 |
| ” 3 ” | 212 |
| ” 4 ” | 215 |
| ” 5 ” | 178 |
| ” 6 ” | 188 |
| ” 7 ” | 204 |
| ” 8 ” | 250 |
| ” 9 ” | 240 |
| ” 10 ” | 218 |
| ” 11 ” | 168 |
| ” 12 ” | 127 |
| ” 13 ” | 132 |
| ” 14 ” | 137 |
| ” 15 ” | 111 |
| ” 16 ” | 134 |
| ” 17 ” | 178 |
| ” 18 ” | 175 |
| ” 19 ” | 275 |
| ” 20 ” | 300 |
| ” 21 ” | 220 |
| ” 22 ” | 188 |
| ” 24 ” | 237 |
| ” 25 ” | 325 |
| Oct. 28 ” | 165 |
| ” 31 ” | 210 |
+----------------+-------+