Formation of placer gold deposits in Canadian Shield during late Wisconsin glaciation This paper deals with phenomena of energy generation during the ice sheet degradation. The melted water from ice surface is moving downward along englacial channel similar as water moving in turbine of HPP. Both have same engineering patterns. But for glacial mills the water pressure head and diameter of channels are in many times more than same parameters of HPP. In the same times of mills capacity is greater. Everyone thinks watching the Niagara Waterfall, - it is strength of the Monster. In the same time, its water pressure head is 51 m only. For glacial mills the water pressure head up to 1000 m. Because glacial mill hidden in ice we can not see how much they powerful, how they works and results of their work. Consequences we can observe after ice retreat. Because glacial mill hidden in ice we can not to see how much they powerful, how they works and their results. Consequences will accessible for observations for observations after retreat of ice. Today we can to do it in Greenland and after that the reconstruction of events for Canadian Shield for late Wisconsin glaciation can be create.
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Formation of placer gold deposits in Canadian Shield during late Wisconsin glaciation
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Formation of placer gold deposits in Canadian
Shield during late Wisconsin glaciation
This paper deals with phenomena of energy generation during
the ice sheet degradation. The melted water from ice surface is
moving downward along englacial channel similar as water moving in
turbine of HPP. Both have same engineering patterns. But for glacial
mills the water pressure head and diameter of channels are in many
times more than same parameters of HPP. In the same times of mills
capacity is greater. Everyone thinks watching the Niagara Waterfall, -
it is strength of the Monster. In the same time, its water pressure
head is 51 m only. For glacial mills the water pressure head up to 1000
m. Because glacial mill hidden in ice we can not see how much they
powerful, how they works and results of their work. Consequences we
can observe after ice retreat. Because glacial mill hidden in ice we can
not to see how much they powerful, how they works and their results.
Consequences will accessible for observations for observations after
retreat of ice. Today we can to do it in Greenland and after that the
reconstruction of events for Canadian Shield for late Wisconsin
glaciation can be create.
According to tradition, but for some unknown
reason, after the phrase "the glacier created it",
audience conciliatory nods their heads as a tribute to
his omnipotence. But is it really? Let assume the ice
moving at the fantastic speed of 300 m per day (From
Wikipadia, Russian version of “Serge” definition).
After converted to the Si-system unit the ice speed is
something 0.0035 m/s. It is absolutely nothing. So,
“absolutely nothing” it is opinion. And no more.. For
obtaining of the correct results we must comparisons
the kinetic energies of the ice and water flows.
For calculations we take that the average velocity
of lowland rivers is around 1 m/s. According to the
basic formula of classical mechanics, which
characterizes the energy of motion body - W = mV2/2 ,
the ratio of the running water energy at normal speed
and ice flow speed at abnormal value is 82944. In this
case the kinatic energy of 1 kg ice is equivalent the
energy of 0,012 g water. This ratio for actual ice flow
speed of 100m per year is reduced by several orders of
magnitude. It is suspected that the energy of a single
tubercle bacillus emitted by sneezing is higher than
the energy of one kilogram of ice that "rushing" in
surge flow.
In terms of energy, the ice age divided on two
stages. First one was energy accumulation, second –
energy release. It is clear. The energy accumulated
over thousands of years in practically immovable ice
during its melting converts into kinetic energy of
running water. Because, this occurs on the glacier
surface on altitude as a few hundred meters the water
has a huge reserve of potential energy. Problems are
where and how this energy can be released and what its
consequences? These questions are goals of our study.
Greenland became main object of preliminary study
of processes and phenomena that took place at North
America during the late Wisconsin period, i.e. time of
intensive ice melting. As results we focused on some
regularity.
1. Visual observations of Google space views shown
that parallel of the current glacial limit on the ice
surface there are many supraglacial lakes (fig. 1).
Fig. 1.
2. On the same picture the turbid water of the
streams from under the ice body clearly visible.
3. Via Internet and from Google Earth the few
images of Glacial Mills (Moulin) were obtained. These
are very interesting and maximal important phenomena.
They have practically ideal circle (fig. 2 and 3).
These appearances immediately recall whirlpools in
kitchen sinks, in bathtubs and in toilet bowls. Other
is not given. Moulin is result of vortex activity!
Fig. 2.
Fig.3.
4. Tourist pictures of sand forms next to ice
lobes from under which water flows were found (fig. 4
– 10).Because the Greenland geology practically in 100%
constructed by basement rocks the question, - Where
sands are coming from? Question actual not only for
Greenland it is actual for Canadian and Scandinavian
shields, too. All these geological units are composed
by basement rocks. Sand deposits are extraneous for
them.
Fig. 4.
Fig. 5.
Fig. 6.
Fig. 7.
Fig. 8.
Fig. 9.
Fig. 10.
Let's assume that the term Moulin is not metaphor
only? Expression, the crystalline rocks has turned to
powder by glacier is common for textbooks around the
world. But, how it did is not written. In glaciology
the term of Moulin (mill) used hundred years more but
only as metaphor. Why? In fact, its construction is
true water mill. Because the ice thickness, its power
is ten times the capacity of the Krasnoyarsk HPP, that
was proud of the Soviet and then Russian energy. Water
mill energy realize on contact of ice with solid rocks.
The results of the water mills activity are holes and
water streams that remove debris, sand and powder.
After the retreat of the glacier kettle lakes were left
on ground. Beside this, lot of debris deposited in
subglacial lakes. These facts prove by ariel and space
views from Google Earth (fig. 11-12).
For compare say, the single turbine power of
Krasnoyarsk HPP is 508 MW with at 93 m water pressure
head and 8.5 m rotor diameter. Altitudes of supralakes
are 800-1200 m a. s. l. With regard to bedrock altitude
(up to 500 m) ice thicknesses are 300-700 m. These
values are water pressure head for glacial mills for
this part of Greenland. In the case of the same
diameter of mill’s hole, its capacity is three-seven
times more that Krasnoyarsk HPP single generator. The
energy of mill was using direct here on small area.
Consequences are: 1 – basement rock disintegration: 2 –
removing of debris from holes and they became deeper: 3
– debris separation as on ore-dressing enterprise; 4 –
removing by water the fine grain debris far away. All
together aspects of the vortex system activities are
equal of mining plus ore-dressing and processing
enterprise. Sometimes in reality it looks as sludge
chamber system. Example presented on fig. 13.
Fig. 11.
Fig. 12.
Fig. 13. Fresh deposits readily available for sampling
and prospecting.
Good Luck! Maybe.Small glacial mills limited by red square
There are some instrumental evidences of current
mills activity. At fig. 14 the Greenland ice sheet
hydrologic system and spreading of fine grain debris in
Greenland fjord sediment plumes are show. The
quantitative measures prove that mills are working
constantly. Presence of sludge in water streams is
strong evidence of this.
Elements of the Greenland ice sheet hydrologic system for land-terminating and marine-terminating glacier outlets, from Chu,V.W. (2014). Greenland Ice Sheet hydrology: a review. Progress in PhysicalGeography. 38(1):19-54 pdf
Greenland fjord sediment plumes
Sediment-rich meltwaterentering fjords from bothmarine-terminating outletglaciers and rivers fromland-terminating glacierscan become buoyant on thewater surface, creating aturbid sediment plumevisible in satelliteimagery. The presence ofsediment plumes in outletglacier fjords signalsfreshwater release from theice sheet to the ocean,with plumes showing lowersalinity and highersuspended sedimentconcentration (SSC) thansurrounding marine water.The image on the rightshows a map of sedimentplumes around Greenland,representing a spatial andtemporal climatology of