QUOTE(recon_soldier @ Dec 4 2006, 02:00 PM) [snapback]1448884[/snapback]
I pretty much agree with you, the way that those images depict a Hollow earth is...well..highly irregular, that would mean that there is a centre of gravity inbetween the two 'sides' ...to be plausible
i may be wrong.
i have no problem with being wrong

http://www.genesispark.org/genpark/trop/trop.htmObservations by north polar explorers indicate that there is indeed a land in the far north with a subtropical climate heated by a sister sun inside Our Hollow Earth. For example, Explorer's reports of abundant animal and bird life in the summer time in the far north indicates a homeland in the north from which they extend in the summer further south and to which they are seen to migrate in the fall.
Explorer Hays observed abundant insect life in the far north. When he was in latitude 78 degrees, 17 minutes in early July he said, "I secured a yellow-winged butterfly, and--who would believe it--a mosquito...ten moths, three spiders, two bees and two flies." (The Open Polar Sea, p. 413)
Notice the element of surprise that many explorers expressed resulting from the discovery of conditions which they weren't expecting.
Explorer Greely, in his book, THREE YEARS OF ARCTIC SERVICE, in Grinnell Land in June of 1881, reports birds of an unknown species, butterflies, bumblebees, so many flies they couldn't sleep at night, and temperatures of 47 and 50 degrees at latitude 81 degrees 49 minutes north. He also found plenty willow to make fire, and much driftwood, (Chapter 26, Vol. I)
A swedish expedition under Otto Torell, found near Trurenberg Bay in the Arctic Sea, trees floating with green buds on them and among them was found the seed of the tropical Entada Bean which measured 2.25 inches across. (Gardner, p. 253)
Explorer Sverdrup at 81 degrees north found so many hares that they named one inlet, Hare Fiord. Also nearly all expedition parties found enough game to keep their exploring parties well fed with meat. These included herds of musk-oxen and reindeer. (Gardner p. 254)
Captain Beechey saw so many birds on the west coast of Spitzbergen that sometimes a single shot killed thirty of them. (Gardner p. 254)
All explorers observed that not all animals migrate south to escape the cold Arctic winds in winter, but many instead go north. Where do they go? Greely, surprised at the tremendous amount of wildlife in a supposed frozen north wrote, "Surely this presence of birds and flowers and beasts was a greeting on nature's part to our new home."
Explorer Kane reported seeing several groups of Brent Geese, which is an American migratory bird, flying NORTHEAST in their wedge-shaped line of flight at 80 degrees 50' north at Cape Jackson, near Grinnelland in late June 1854.
Explorer Greely makes this statement of the northward migration of bears, "Lieutenant Lockwood, in May, 1882, noticed bear tracks (going NORTHEAST) on the north coast of Greenland, near Cape Benet in 83 degrees 3' N.," and commented, "...I cannot understand why the bear ever leaves the rich hunting-field of the 'North Water' for the desolate shores of the northward." (THREE YEARS, p. 366)
Greely also wrote about the Ross Gull, "...the observations of Murdoch at Point Barrow show that this bird, in thousands, passes over that point to the NORTHEAST in October, none of which were seen to return." (THREE YEARS, p. 383)
Explorer Adolf Erick Nordenskiold, leader of a Swedish expedition, recorded in THE ARCTIC VOYAGE OF 1858-1878, that on May 23, they saw north of Amsterdam Island (by Spitzbergen), "great numbers of barnacle geese...flying towards the NORTHWEST, perhaps to some land more northerly than Spitzbergen. (There is no such land on our present-day maps) The existence of such a land," wrote Nordenskiold, "is considered quite certain by the walrus-hunters, who state that at the most northerly point hitherto reached, such flocks of birds are seen steering their course in rapid flight yet farther toward the north." (Gardner, p. 160)
Daines Barrington, in his book, ON THE POSSIBILITY OF APPROACHING THE NORTH POLE, wrote that observers in Spitzbergen have always noticed in spring, just before the hatching season, the wild ducks, geese, and other birds, fly in a northerly direction. There is also a heavy fall migration to the north.
In HEARNES JOURNAL, is told of observations around Hudson's Bay by Hearne of ten species of geese, particularly the snow goose, blue goose, brent goose, horned wavy goose, lay their eggs and raise their young in some country which to Hearne was unknown. Explorers, Indians and Eskimos could never tell where these fowl bred and it was well known that they never migrated to the south.
Epes Sargent in his WONDERS OF THE ARCTIC WORLD tells that Franklin's second expedition saw large numbers of laughing geese migrating to the unknown north--sure indication of land to the north. And this was observed on the north coast of Canada latitude 69 degrees 29" N., longitude 130 degrees 19 minutes W., on July 13. (Sargent, p. 163).
Newton in his ARCTIC MANUAL, wrote as follows concerning the migrations of the Knot, "The knot...in the spring seeks our island (England) in immense flocks, and after remaining on the coast for about a fortnight, can be traced proceeding gradually northwards, until finally, it takes leave of us. It has been noticed in Iceland and Greenland, but not to stay; the summer there would be too rigorous for its liking, and it goes further and further north. Whither? Where does it build its nest and hatch its young? We loose all trace of it for some weeks. What becomes of it?"
"Toward the end of summer back it comes to us in larger flocks than before, and both old birds and young birds remain upon our coasts until November, or, in mild seasons even later. Then it wings its flight to the south, and luxuriates in blue skies and balmy airs until the following spring, then it resumes the order of its migration." (Gardner pp. 259-260) Surely these migrations indicate a land further north than Greenland and Spitzbergen with an ideal climate for the breeding grounds of these migratory birds and animals.
Many explorers noticed a rise in temperature the farther north they went. For example, Nansen reported that a northwind in the winter is warmer than a south wind. On Jan. 18, 1894 at 79 degrees N., Nansen wrote, "It is curious that there is almost always a rise of thermometer with these stronger winds...A south wind of less velocity generally lowers the temperature, and a moderate north wind RAISES it." (FARTHEST NORTH, Vol. I, p. 197) Two months later on March 4th, Nansen also wrote, "It is curious that now the northerly winds bring cold and the southerly warmth. Earlier in the winter IT WAS JUST THE OPPOSITE." This obviously indicates the existence of a warmer land toward the north from which the warm wind blows in the winter.
In Roald Amundsen's FIRST CROSSING OF THE POLAR SEA, by dirigible, May 12, 1926, this rise in temperature toward the pole was also recorded. Upon leaving Spitzbergen the temperature was minus 8 degrees centigrade. Then the temperature at the altitude of flight sank steadily from 5 degrees below freezing over King's Bay to 12 degrees below zero on 88 degrees north on the European side of the pole. FROM THIS PLACE IT BEGAN TO RISE SLOWLY. The temperature at the pole was 2 degrees below zero. That is an increase of 10 degrees! (FIRST CROSSING, p. 230)
In the soviet flight of Mikhail Gromov, of the Soviet Air Force, in an article titled, "Across the North Pole to America," he recorded a similar increase of temperature at the pole. Flying above Franz Josef Land at 13,000 feet, the temperature was minus 16 degrees Centigrade. But at the pole at 8,850 feet the temperature was recorded at minus 8 degrees C--an 8 degree increase in temperature. Both Amundsen and Gromov changed direction after calculating with the sextant that they were at the pole.
It must be understood that when explorers say they have reached the pole, that this means that they have reached a point on the curvature of the earth in the Arctic or Antarctic where the angle of the sun over the horizon on their sextant readings indicates that they are farthest north for the north pole or farthest south for the south pole. Since it is difficult for explorers to measure distances in the Arctic or Antarctic directly, distances were measured by determining the latitude with the sextant. Explorers would travel a certain distance north, for example, take a reading with the sextant and based on that reading and the distance to the pole as shown on a map, they then calculated how many miles they had traveled.
Today, however, with the advent of navigational satellites, geographic determination of location is determined with the GPS, the Global Positioning System. With hand-held devices, anyone can receive the satellite signals from the GPS to determine their latitude and longitude. With overflights of the poles and submarines criss-crossing the Arctic, one would rightly wonder why the polar openings haven't been openly discovered and published to the world. Certainly such a discovery must world-shaking, mind shattering, and revolutionary to our sciences. Our physics books would have to be re-written. Certainly the poles have been attained. Which strongly suggests that any polar openings would have to be located to one side or other of the poles. Such discovery, however, is still World Top Secret.
Still, however strangely it might seem, there are indications that the polar openings do exist! Another evidence of the polar openings is found in the surprised comments of explorers upon finding the fog conditions at the poles. The May 1926, Amundsen dirigible expedition noted that from Spitzbergen, "For more than eleven hours we flew in brilliant sunshine. On 87 degrees latitude we met with fog, which, however, soon disappeared. Between 88 degrees and 89 degrees latitude we came into a new belt of fog. The fog lay, however, so low that we could fly over it by rising to 7,000 meters altitude."
From our theory, we obtain a ready answer concerning the origin of these belts of fog--they come as result of the warm moist air currents issuing from the polar opening, which as they meet the lower cold air next to the ice, condense into fog.
Continuing, Malmgren wrote, "At the Pole itself the fog thinned. The weather, as if for the occasion, at this longed-for spot on the earth's surface, can be described in a few words. The sky for the most part was covered with stratocumulus and altocumulus clouds. There was a complete cessation of wind. The temperature at about 300 meters altitude was 2 degrees below zero. From the pole we set our course towards Point Barrow. The journey from the Pole was, at the beginning, favored with good visibility, but between 86 and 85 degrees latitude we met with continuous fog." And notice was made of "...the temperature in the layer of air nearest the ice was from 3-4 degrees lower than that higher up..."
Commenting on this phenomenon, Malmgren, Amundsen's meteorologist on the expedition wrote, "One of the problems that the expedition has brought to life refers to the polar fog. Why is it that over the monotonous plain which is formed by the polar sea there occur regions, close to one another, with and without fog, often without any changes in atmospheric temperature being observable? Are the lowermost air-layers so conservative that they can still, in the polar sea, retain memories from their more southerly existence? Or is the phenomenon due--which, however, appears incredible--to the variations in the heat development between the air and the underlying ice?" (FIRST CROSSING OF THE POLAR SEA, pp. 272, 280, 281) Notice how Malmgren is puzzled by the temperature difference of the different layers of air suggesting currents from a more southerly or warmer climate.
http://www.geocities.com/Area51/Shadowland...3/under012.html 
Note there are also similar fogs and icecaps on Mars!!!!
http://learn.arc.nasa.gov/planets/index.html
http://www.vnn.org/editorials/ET0003/ET25-5743.htmlhttp://www.vnn.org/editorials/ET0002/ET04-5405.html