Á¦ 58 Æí |
PAPER 58 |
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À¯¶õ½Ã¾ÆÀÇ »ý¸í ŵ¿ |
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58:0.1 |
»çŸ´Ï¾Æ Àüü¿¡¼, »ý¸íü-º¯Çü Ç༺ÀÎ À¯¶õ½Ã¾Æ¿Í ºñ½ÁÇÑ ¼¼°è´Â 61°³ ¹Û¿¡ ¾ø´Ù. °ÅÁֵǴ ¼¼°èµé ´ëºÎºÐÀº ÀÌ¹Ì È®Á¤µÈ ±â¹ý¿¡ ÀÇÇØ¼ °ÅÁÖÇϵµ·Ï µÇ¾î ÀÖÀ¸¸ç; ±×·¯ÇÑ ±¸Ã¼¿¡¼ »ý¸í¿î¹ÝÀÚµéÀº »ý¸í À̽ÄÀ» À§ÇÑ ±×µéÀÇ °èȹ¿¡ ÀÖ¾î¼ ¿©Áö°¡ º°·Î ¾ø´Ù. ±×·¯³ª ¾à 10ºÐÀÇ 1¿¡ ÇØ´çÇÏ´Â ¼¼°è´Â ½ÊÁø¹ý Ç༺À¸·Î ÁöÁ¤µÇ°í, »ý¸í¿î¹ÝÀÚµéÀÇ Æ¯º° µî·Ï¿¡ ¹èÁ¤ µÈ´Ù; ±×·¯ÇÑ Ç༺¿¡¼ ¿ì¸®´Â »ý¸íÀÇ Ç¥ÁØ ¿ìÁÖ À¯ÇüÀ» º¯Çü½ÃŰ°Å³ª, ¶Ç´Â °¡´ÉÇÑ ¹üÀ§ ³»¿¡¼ ¹ßÀü½Ã۰íÀÚ ÇÏ´Â ³ë·ÂÀÇ ÀÏȯÀ¸·Î ¾î¶² »ý¸í ½ÇÇèÀ» ¼öÇàÇϵµ·Ï Çã¶ôÀ» ¹Þ¾Ò´Ù. |
IN ALL Satania there are only sixty-one worlds similar to Urantia, life-modification planets. The majority of inhabited worlds are peopled in accordance with established techniques; on such spheres the Life Carriers are afforded little leeway in their plans for life implantation. But about one world in ten is designated as a decimal planet and assigned to the special registry of the Life Carriers; and on such planets we are permitted to undertake certain life experiments in an effort to modify or possibly improve the standard universe types of living beings. |
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58:1.1 |
600,000,000³â Àü¿¡, »ý¸í¿î¹ÝÀÚµé À§¿øÈ¸°¡ ¿¹·ç¼ÀÀ¸·ÎºÎÅÍ ÆÄ°ßµÇ¾î À¯¶õ½Ã¾Æ¿¡ µµÂøÇÏ¿´À¸¸ç, »çŸ´Ï¾Æ ü°èÀÇ 606¹øÀÇ ¼¼»ó¿¡ »ý¸íü¸¦ ŵ¿½Ã۱â À§ÇÑ Áغñ °úÁ¤À¸·Î, ¹°¸®ÀûÀÎ Á¶°ÇÀ» ¿¬±¸Çϱ⠽ÃÀÛÇÏ¿´´Ù. À̰ÍÀº ¿ì¸®°¡ »çŸ´Ï¾Æ¿¡¼ ³×¹Ùµ· »ý¸í ¿øÇüƲÀ» Àü¼öÇÏ´Â 606¹øÂ° üÇèÀ̾úÀ¸¸ç, Áö¿ª¿ìÁÖÀÇ ±âº»ÀûÀ̰í Ç¥ÁØÀûÀÎ »ý¸í ¼³°è¿¡ º¯È¸¦ ÀÏÀ¸Å°°í º¯ÇüÀ» ½ÃµµÇÏ´Â 60¹øÂ° ±âȸ¿´´Ù |
600,000,000 years ago the commission of Life Carriers sent out from Jerusem arrived on Urantia and began the study of physical conditions preparatory to launching life on world number 606 of the Satania system. This was to be our six hundred and sixth experience with the initiation of the Nebadon life patterns in Satania and our sixtieth opportunity to make changes and institute modifications in the basic and standard life designs of the local universe. |
58:1.2 |
±¸Ã¼°¡ ÁøÈ ¼øÈ¯Áֱ⸦ °³½ÃÇϱ⿡ ¾Ë¸ÂÀº ȯ°æÀÌ ¼º¼÷µÇ±â Àü¿¡´Â »ý¸í¿î¹ÝÀÚ°¡ »ý¸íÀ» Àü¼öÇÒ ¼ö ¾ø´Ù´Â »ç½ÇÀ» ºÐ¸íÈ÷ ÇØ µÑ Çʿ䰡 ÀÖ´Ù. »Ó¸¸ ¾Æ´Ï¶ó ¿ì¸®´Â Ç༺ÀÇ ¹°¸®ÀûÀÎ Áøº¸¿¡ ÀÇÇØ¼ À¯ÁöµÇ°í ¼ö¿ëµÉ ¼ö ÀÖ´Â °Íº¸´Ù ´õ ºü¸¥ »ý¸í ¹ßÀüÀ» ÁغñÇÒ ¼öµµ ¾ø´Ù. |
It should be made clear that Life Carriers cannot initiate life until a sphere is ripe for the inauguration of the evolutionary cycle. Neither can we provide for a more rapid life development than can be supported and accommodated by the physical progress of the planet. |
58:1.3 |
»çŸ´Ï¾ÆÀÇ »ý¸í¿î¹ÝÀÚµéÀº »ý¸íÀÇ ¿°È³ªÆ®·ý ¿øÇüƲÀ» ±¸Ã¼ÀûÀ¸·Î Åõ»ç ÇÏ¿´¾ú´Ù; ±×·¸±â ¶§¹®¿¡ ¹Ù´å¹°ÀÌ ÃæºÐÇÑ ¼Ò±Ý±â¸¦ °®°Ô µÇ±â Àü¿¡´Â ±×°ÍÀ» ½É´Â ´Ü°è°¡ ÁøÇàµÉ ¼ö ¾ø¾ú´Ù. À¯¶õ½Ã¾Æ À¯ÇüÀÇ ¿øÇüÁúÀº Àû´çÇÑ ¼Ò±Ý±âÀÇ ¿ë¾× ¼Ó¿¡¼¸¸ ±â´ÉÇÒ ¼ö ÀÖ´Ù. Á¶»óÀÌ µÇ´Â¦¡½Ä¹°°ú µ¿¹°¦¡¸ðµç »ý¸íÀº ¼Ò±Ý-¿ëÇØ ¼½ÄÁö¿¡¼ ÁøÈµÇ¾ú´Ù. ±×¸®°í ºñ·Ï ¸Å¿ì °íµîÀÇ À¯±âü À°Áöµ¿¹°µµ ¹Ù·Î ÀÌ µ¿ÀÏÇÑ º»ÁúÀû ¼Ò±Ý¿ëÇØ¾×ÀÌ Ç÷·ù·Î¼ ±×µéÀÇ ¸öü¸¦ ÀÚÀ¯·Ó°Ô Àû½Ã¸ç, ±ÛÀÚ±×´ë·Î Àá±â¾î, ¸ðµç °¢°¢ÀÇ ¹Ì¼¼¼¼Æ÷°¡ ÀÌ ¡®¼Ò±Ý±â¿¡ Àá°ÜÀÖÀ½¡¯À¸·Î »ì¾Æ°¡µµ·Ï ±×µé ¸öü¿¡ µÎ·ç ¼øÈ¯ÇÏÁö ¾ÊÀ¸¸é »ý¸íÀ» °è¼Ó À¯ÁöÇÒ ¼ö ¾ø´Ù |
The Satania Life Carriers had projected a sodium chloride pattern of life; therefore no steps could be taken toward planting it until the ocean waters had become sufficiently briny. The Urantia type of protoplasm can function only in a suitable salt solution. All ancestral life -- vegetable and animal -- evolved in a salt-solution habitat. And even the more highly organized land animals could not continue to live did not this same essential salt solution circulate throughout their bodies in the blood stream which freely bathes, literally submerses, every tiny living cell in this "briny deep." |
58:1.4 |
³ÊÈñµéÀÇ ¿ø½Ã Á¶»óµéÀº § ¹Ù´Ù¿¡¼ ÀÚÀ¯·Ó°Ô ¼øÈ¯ÇÏ¿´À¸¸ç; ¿À´Ã³¯¿¡´Â, ¹Ù·Î ÀÌ ¹Ù´Ù¿Í °°Àº ¼Ò±Ý ¿ëÇØ°¡ ³ÊÈñµéÀÇ ¸ö¼Ó¿¡¼ ÀÚÀ¯·Ó°Ô ¼øÈ¯Çϰí, ÃÖÃÊÀÇ »ì¾ÆÀÖ´Â ¼¼Æ÷µéÀÇ Ã¹ ¿øÇüÁú ¹ÝÀÀÀÌ Ç༺¿¡¼ ±â´ÉÇϵµ·Ï ÀÚ±ØÀ» ÁÖ¾ú´ø ¼Ò±Ý¹°°ú ºñ±³µÉ ¼ö ÀÖ´Â ¸ðµç º»ÁúÀûÀÎ ¿ä¼ÒµéÀÇ ÈÇÐÀûÀÎ ¿ë¾×À¸·Î °¢°¢ÀÇ µ¶¸³µÈ ¼¼Æ÷¸¦ Àû¼ÅÁÖ°í ÀÖ´Ù. |
Your primitive ancestors freely circulated about in the salty ocean; today, this same oceanlike salty solution freely circulates about in your bodies, bathing each individual cell with a chemical liquid in all essentials comparable to the salt water which stimulated the first protoplasmic reactions of the first living cells to function on the planet. |
58:1.5 |
±×·¯³ª ÀÌ ½Ã´ë°¡ ½ÃÀ۵ǾúÀ» ¶§, À¯¶õ½Ã¾Æ´Â ¸ðµç ¸é¿¡¼ ÇØ¾ç »ý¸íÀÇ Ãʱâ ÇüŵéÀ» ºÎ¾ç(ݦå×)Çϱ⿡ ¾Ë¸ÂÀº »óÅ·ΠÁøÈµÇ¾î °¡°í ÀÖ¾ú´Ù. Áö±¸¿Í °¡±î¿î °ø°£ÀÇ Áö¿ªµé¿¡¼, ¿ì¸®°¡ °áÁ¤ÇÏ¿´´ø °ÍÀÌ Àü°³µÇ´Â ¹°¸®Àû ȯ°æ¦¡Áö»ó°ú °ø°£ÀǦ¡¿¡ °¡Àå Àß ÀûÀÀÇÒ ¼ö ÀÖµµ·Ï, ¹°¸®ÀûÀÎ ¹ßÀüÀÌ ¼Óµµ´Â ´À¸®Áö¸¸ È®½ÇÇÏ°Ô ±×·¯ÇÑ »ý¸í ÇüŵéÀ» ¼ö¸³ÇÒ ¼ö ÀÖ´Â ¹Ì·¡ÀÇ ½ÃµµµéÀ» À§ÇÑ ¹«´ë¸¦ ÁغñÇϰí ÀÖ´Ù. |
But as this era opens, Urantia is in every way evolving toward a state favorable for the support of the initial forms of marine life. Slowly but surely physical developments on earth and in adjacent space regions are preparing the stage for the later attempts to establish such life forms as we had decided would be best adapted to the unfolding physical environment -- both terrestrial and spatial. |
58:1.6 |
±×¸®°í ³ª¼ »ý¸í¿î¹ÝÀÚµéÀÇ »çŸ´Ï¾Æ À§¿øÈ¸´Â ´ë·ú ¶¥ µ¢¾î¸®°¡ ´õ ³ª´µ¾îÁ®¼, ½ÇÁ¦ÀûÀÎ »ý¸í À̽ÄÀÌ ½ÃÀ۵DZâ Àü¿¡, ´õ ¸¹Àº ³»·ú ¹Ù´Ù¿Í º¸È£µÈ ¸¸(ؽ)µéÀÌ ÀÌ·ç¾îÁú ¶§¸¦ ±â´Ù¸®±â·Î ÇÏ°í ¿¹·ç¼ÀÀ¸·Î µ¹¾Æ°¬´Ù. |
Subsequently the Satania commission of Life Carriers returned to Jerusem, preferring to await the further breakup of the continental land mass, which would afford still more inland seas and sheltered bays, before actually beginning life implantation. |
58:1.7 |
»ý¸íÀÌ ÇØ¾çÀ¸·ÎºÎÅÍ ±â¿øµÈ Ç༺¿¡¼ »ý¸í À̽ÄÀ» À§ÇÑ ÀÌ»óÀûÀÎ Á¶°ÇµéÀº ¼ö¸¹Àº ³»·úÀÇ ¹Ù´Ùµé, ³¡¾øÀÌ ÆîÃÄÁø ¼ö½ÉÀÌ ¾èÀº ÇØ¾È¼±°ú º¸È£µÈ ¸¸(ؽ)µé¿¡ ÀÇÇØ¼ Á¦°øµÇ¾úÀ¸¸ç; Áö±¸»óÀÇ ¹°µéÀÇ ¹Ù·Î ±×¿Í °°Àº ºÐÆ÷°¡ ºü¸¥ ¼Óµµ·Î ÁøÇàµÇ¾ú´Ù. °í´ëÀÇ ÀÌ·¯ÇÑ ³»·ú ÇØ(ú)µéÀÇ ±íÀÌ´Â 500 ³»Áö 600ÇÇÆ®¸¦ °ÅÀÇ ³ÑÁö ¾Ê¾ÒÀ¸¸ç, ÅÂ¾ç ±¤¼±Àº ÇØ¼ö 600ÇÇÆ® À̻󿡱îÁö ¹ÌÄ¥ ¼ö ÀÖ¾ú´Ù. |
On a planet where life has a marine origin the ideal conditions for life implantation are provided by a large number of inland seas, by an extensive shore line of shallow waters and sheltered bays; and just such a distribution of the earth's waters was rapidly developing. These ancient inland seas were seldom over five or six hundred feet deep, and sunlight can penetrate ocean water for more than six hundred feet. |
58:1.8 |
¿ø½Ã ½Ä¹° »ý¸íÀÌ ¶¥ À§·Î ¿Ã¶ó°¥ ¼ö ÀÖ´Â ±æÀ» ¹ß°ßÇÑ °ÍÀº ¹Ù·Î ±×·¯ÇÑ ÈÄ´ë(ýÓÛ)ÀÇ ¿ÂÈÇÏ°í ±ÕÀÏÇÑ ±âÈĸ¦ °®´Â ÇØ¾È¼±¿¡¼¿´´Ù. ±×°÷¿¡ ´ë±â ¼Ó¿¡ ÀÖ´Â ³ôÀº ³óµµÀÇ Åº¼Ò´Â »õ·Î¿î ¶¥¿¡ ½Å¼ÓÇÏ°í ¹«¼ºÇÑ ¼ºÀåÀÇ ´Ù¾çÇÑ »ý¸í ±âȸ¸¦ Á¦°øÇÏ¿´´Ù. ÀÌ·¯ÇÑ ´ë±â »óŰ¡ ½Ä¹°ÀÇ ¼ºÀå¿¡ ÀÌ»óÀûÀÌÁö¸¸, ÀÌ»êÈź¼ÒÀÇ ³óµµ°¡ ³Ê¹« ³ô¾Ò±â ¶§¹®¿¡ ¾î¶² µ¿¹°µµ ÁöÇ¥¸é¿¡ »ì ¼ö ¾ø¾úÀ¸¸ç »ç¶÷Àº ´õ¿í ±×·¯ÇÏ¿´´Ù. |
And it was from such seashores of the mild and equable climes of a later age that primitive plant life found its way onto the land. There the high degree of carbon in the atmosphere afforded the new land varieties of life opportunity for speedy and luxuriant growth. Though this atmosphere was then ideal for plant growth, it contained such a high degree of carbon dioxide that no animal, much less man, could have lived on the face of the earth. |
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58:2.1 |
Ç༺ÀÇ ´ë±â´Â žçÀÇ Àüü ºû ¹æÃâ Áß¿¡¼ ¾à 2½Ê¾ï ºÐÀÇ ÀÏÀ» Áö±¸ ¼ÓÀ¸·Î µé¾î¿À°Ô ÇÑ´Ù. ¸¸¾à¿¡ ºÏ ¾Æ¸Þ¸®Ä«¿¡ ºñÄ¡´Â ±¤¼±¿¡ ´ëÇÏ¿© ½Ã°£´ç 1ų·Î¿ÍÆ®¸¶´Ù 2¼¾Æ®ÀÇ ºñÀ²·Î µ·À» ¸Å±ä´Ù¸é, ¿¬°£ »ç¿ë·®¿¡ ´ëÇÑ ºñ¿ëÀº ¾à 80 °æ(ÌÈ) ´Þ·¯ ÀÌ»óÀÌ µÉ °ÍÀÌ´Ù. ÅÂ¾ç ±¤¼±¿¡ ´ëÇÏ¿© ½ÃÄ«°í ½Ã¿¡ ºÎ°úµÉ ºñ¿ëÀº ÇÏ·ç¿¡ 1¾ï ´Þ·¯ ÀÌ»ó¿¡ »ó´çÇÏ´Â ±Ý¾×ÀÌ µÉ °ÍÀÌ´Ù. ±×¸®°í ³ÊÈñµéÀº žçÀ¸·ÎºÎÅÍ ´Ù¸¥ ÇüÅÂÀÇ ¿¡³ÊÁöµéµµ ¹Þ°í ÀÖ´Ù´Â °ÍÀ» ±â¾ïÇØ¾ß¸¸ ÇÒ °ÍÀÌ´Ù¦¡ºû¸¸ÀÌ ³ÊÈñµéÀÇ ´ë±â¿¡ ³¢Ä¡´Â žçÀÇ ±â¿©°¡ ¾Æ´Ï´Ù. Àΰ£ÀÇ ´«À¸·Î ½Äº°ÇÒ ¼ö ÀÖ´Â ¹üÀ§º¸´Ù ³ô°Å³ª ³·Àº ÆÄÀåµéÀ» Æ÷ÇÔÇÏ¿© ±¤´ëÇÑ ÅÂ¾ç ¿¡³ÊÁöµéÀÌ À¯¶õ½Ã¾Æ¿¡ ³»·Á ÂÉÀ̰í ÀÖ´Ù |
The planetary atmosphere filters through to the earth about one two-billionths of the sun's total light emanation. If the light falling upon North America were paid for at the rate of two cents per kilowatt-hour, the annual light bill would be upward of 800 quadrillion dollars. Chicago's bill for sunshine would amount to considerably over 100 million dollars a day. And it should be remembered that you receive from the sun other forms of energy -- light is not the only solar contribution reaching your atmosphere. Vast solar energies pour in upon Urantia embracing wave lengths ranging both above and below the recognition range of human vision. |
58:2.2 |
½ºÆåÆ®·³ÀÇ Àڿܼ± ¸Ç ³¡ ºÎºÐ¿¡ ÀÖ´Â ÅÂ¾ç ¹æ»ç´É ¹°ÁúÀÇ ´ëºÎºÐÀº Áö±¸ÀÇ ´ë±â¸¦ Åë°úÇÏÁö ¸øÇÑ´Ù. ÀÌ·¯ÇÑ ÂªÀº ÆÄÀåµéÀÇ ´ëºÎºÐÀº Áö±¸ Ç¥¸éÀ¸·ÎºÎÅÍ ¾à 10¸¶ÀÏ »ó°ø Àü¿ª¿¡ ÀÖ°í ±×¸®°í ´Ù½Ã ¿ÜºÎ °ø°£À¸·Î 10¸¶ÀÏ È®ÀåµÇ´Â ¿ÀÁ¸Ãþ¿¡ ÀÇÇØ¼ Èí¼öµÇ¸ç, Áö±¸ Ç¥¸é¿¡ ¿µÇâÀ» ³¢Ä¡´Â ¿ÀÁ¸Àº ¿ÀÁ÷ 10ºÐÀÇ 1ÀÎÄ¡ µÎ²²¿¡ ÇØ´çµÇ´Â Ãþ¿¡ ºÒ°úÇÏÁö¸¸; ±×·³¿¡µµ ºÒ±¸Çϰí, ºñ±³Àû ¼Ò·®ÀÌ°í °Ñº¸±â¿¡ º°·Î ´ë´ÜÄ¡ ¾ÊÀº ÀÌ·¯ÇÑ ¿ÀÁ¸ÀÌ Å¾籤¼± ¼Ó¿¡ ÀÖ´Â À§Ç轺·´°í ÆÄ±«ÀûÀÎ Àڿܼ± ¹æ»ç´É ¹°Áú·ÎºÎÅÍ À¯¶õ½Ã¾Æ °ÅÁֹεéÀ» º¸È£ÇÑ´Ù. ±×·¯³ª ÀÌ ¿ÀÁ¸ÃþÀÌ Á¶±Ý¸¸ ´õ µÎÅÍ¿öµµ, ³ÊÈñµéÀÇ °Ç°À» À¯Áö½ÃÄÑ ÁÖ°í °¡Àå ÇʼöÀûÀÎ ºñŸ¹Îµé Áß ÇϳªÀÇ ±Ù¿øÀÌ µÇ¸ç ÇöÀç Áö±¸ Ç¥¸é¿¡ ÂÉÀ̰í ÀÖ´Â ¸Å¿ì Áß¿äÇÑ Àڿܼ±ÀÌ Â÷´ÜµÉ °ÍÀÌ´Ù. |
The earth's atmosphere is all but opaque to much of the solar radiation at the extreme ultraviolet end of the spectrum. Most of these short wave lengths are absorbed by a layer of ozone which exists throughout a level about ten miles above the surface of the earth, and which extends spaceward for another ten miles. The ozone permeating this region, at conditions prevailing on the earth's surface, would make a layer only one tenth of an inch thick; nevertheless, this relatively small and apparently insignificant amount of ozone protects Urantia inhabitants from the excess of these dangerous and destructive ultraviolet radiations present in sunlight. But were this ozone layer just a trifle thicker, you would be deprived of the highly important and health-giving ultraviolet rays which now reach the earth's surface, and which are ancestral to one of the most essential of your vitamins. |
58:2.3 |
±×·¯³ª ³ÊÈñµé Áß¿¡¼ »ó»ó·ÂÀÌ ºó¾àÇÑ ÀϺÎÀÇ ¹°ÁúÁÖÀÇÀÚµéÀº ¾ÆÁ÷µµ ¹°Áú âÁ¶¿Í Àΰ£ ÁøÈ¸¦ ÇϳªÀÇ ¿ì¿¬ÇÑ Çö»óÀ¸·Î º¸·Á´Â °æÇâÀ» ³ªÅ¸³»°í ÀÖ´Ù. À¯¶õ½Ã¾ÆÀÇ ÁßµµÀÚµéÀº ¿ì¿¬ÇÑ Çö»óÀû ¹ýÄ¢°ú ¸ð¼øµÇ´Â °ÍÀ¸·Î °£ÁֵǴ 5¸¸ °¡Áö ÀÌ»óÀÇ ¹°¸®Àû ±×¸®°í ÈÇÐÀû »ç½ÇµéÀ» ¼öÁýÇÏ¿´¾úÀ¸¸ç, ±×µéÀº ±×°ÍµéÀ» Åä´ë·Î ÇÏ¿© ¹°Áú âÁ¶¿¡ Áö´ÉÀûÀÎ ¸ñÀûÀÇ ÇöÁ¸À» ºÐ¸íÇÏ°Ô ½ÇÁõÇÑ´Ù°í ÁÖÀåÇÑ´Ù. ±×¸®°í ÀÌ ¸ðµç °ÍÀº ¹°Áú ¿ìÁÖÀÇ °èȹ°ú âÁ¶ ±×¸®°í À¯Áö¿¡¼ ¸¶À½ÀÌ ÇöÁ¸Çϰí ÀÖÀ½À» Áõ¸íÇÏ´Â µ¥ µµ¿òÀÌ µÇ´Â, ¹°¸®Àû ±×¸®°í ÈÇÐÀû ¿µ¿ª ¹Û¿¡¼ ¹ß°ßµÈ 10¸¸ °¡Áö ÀÌ»óÀÇ °Íµé¿¡ ´ëÇÑ ¸ñ·ÏÀ» °í·ÁÇÏÁö ¾ÊÀº °ÍÀÌ´Ù. |
And yet some of the less imaginative of your mortal mechanists insist on viewing material creation and human evolution as an accident. The Urantia midwayers have assembled over fifty thousand facts of physics and chemistry which they deem to be incompatible with the laws of accidental chance, and which they contend unmistakably demonstrate the presence of intelligent purpose in the material creation. And all of this takes no account of their catalogue of more than one hundred thousand findings outside the domain of physics and chemistry which they maintain prove the presence of mind in the planning, creation, and maintenance of the material cosmos. |
58:2.4 |
žçÀº ³ÊÈñµé¿¡°Ô ½ÇÁ¦ÀûÀ¸·Î Ä¡¸íÀûÀÎ ±¤¼±À» ½ñ¾Æ³»°í ÀÖ°í, À¯¶õ½Ã¾Æ¿¡¼ÀÇ ³ÊÈñµéÀÇ ÄèÀûÇÑ »îÀº, µ¶Æ¯ÇÑ ÀÌ ¿ÀÁ¸ÃþÀÇ ÀÛ¿ë°ú À¯»çÇÑ, °ÑÀ¸·Î º¸±â¿¡ À¯¿¬ÇÏ°Ô º¸ÀÌ´Â 40°¡Áö ÀÌ»óÀÇ º¸È£ ÀÛ¿ëµéÀÇ ¡°¿ì¿¬ÇÑ¡± ¿µÇâ¿¡ ±âÀεǰí ÀÖ´Ù. |
Your sun pours forth a veritable flood of death-dealing rays, and your pleasant life on Urantia is due to the "fortuitous" influence of more than two-score apparently accidental protective operations similar to the action of this unique ozone layer. |
58:2.5 |
¹ã¿¡ ´ë±âÀÇ ¡°´ã¿ä¡± È¿°ú°¡ ¾ø¾ú´Ù¸é, ¹æ¿ ÀÛ¿ëÀ¸·Î ÀÎÇÏ¿© ¿ÀÌ ³Ê¹«µµ ½Å¼ÓÇÏ°Ô ¹ß»êµÇ±â ¶§¹®¿¡, ÀÎÀ§ÀûÀÎ ¿ °ø±ÞÀÌ ¾øÀÌ´Â ¾î¶² »ý¸íüµµ »ì¾Æ³²Áö ¸øÇÒ °ÍÀÌ´Ù. |
Were it not for the "blanketing" effect of the atmosphere at night, heat would be lost by radiation so rapidly that life would be impossible of maintenance except by artificial provision. |
58:2.6 |
Áö±¸ ´ë±âÀÇ ¾Æ·¡ÂÊ 5³»Áö 6¸¶ÀÏÀº ´ë·ù±ÇÀÌ´Ù; À̰÷Àº ±â»ó Çö»óÀ» ÀÏÀ¸Å°´Â ¹Ù¶÷°ú °ø±â È帧ÀÇ Áö¿ªÀÌ´Ù. ÀÌ Áö¿ª À§ÀÇ ¾Æ·¡°¡ Àü¸®ÃþÀÌ°í ±× À§¿¡´Â ¼ºÃþ±ÇÀÌ´Ù. Áö±¸ Ç¥¸éÀ¸·ÎºÎÅÍ À§·Î ¿Ã¶ó°¡¸é¼, 6³»Áö 8¸¶ÀÏ¿¡ À̸¦ ¶§±îÁö ¿Âµµ°¡ ÀÏÁ¤ÇÏ°Ô ÇϰÇϸç, °¡Àå ³ôÀº °÷ÀÇ ¿Âµµ´Â Ⱦ¾·Î ¾à ¿µÇÏ 70µµ¿¡ À̸¥´Ù. Ⱦ¾ ¿µÇÏ 65³»Áö 70µµ¿¡ À̸£´Â ÀÌ·± ¿Âµµ´Â ±× ´ÙÀ½ 40¸¶ÀÏÀ» ¿Ã¶ó°¡´Â µ¿¾È º¯È°¡ ¾øÀ¸¸ç; ¿Âµµ°¡ ÀÏÁ¤ÇÑ ÀÌ ±¸¿ªÀÌ ¼ºÃþ±ÇÀÌ´Ù. 45³»Áö 50¸¶ÀÏÀÇ °íµµ¿¡¼, ¿Âµµ´Â ´Ù½Ã »ó½ÂÇϱ⠽ÃÀÛÇϰí, ¿Âµµ »ó½ÂÀº ¿À·Î¶ó Çö»óÀÌ ÀÖ´Â ³ôÀ̱îÁö °è¼ÓµÇ¾î Ⱦ¾·Î 1,200µµ±îÁö ¿Ã¶ó°¡¸ç, ÀÌ·¯ÇÑ °ÇÑ ¿·Î ÀÎÇÏ¿© »ê¼Ò°¡ ÀÌ¿ÂÈ µÈ´Ù. ±×·¯³ª ÀÌ·¸°Ô Èñ¹ÚÇÑ ´ë±â¿¡ÀÇ ¿Âµµ´Â Áö±¸ Ç¥¸é¿¡¼ ´À³¥ ¼ö ÀÖ´Â ¿°ú °ÅÀÇ ºñ±³µÉ ¼ö ¾ø´Â °ÍÀÌ´Ù. Àüü ´ë±âÀÇ ¹Ý Á¤µµ°¡ ÁöÇ¥¸éÀ¸·ÎºÎÅÍ 3¸¶ÀÏ ¼Ó¿¡ ÀÖÀ½À» ±â¾ïÇϱ⠹ٶõ´Ù. Áö±¸ ´ë±âÀÇ ³ôÀ̦¡¾à 400¸¶ÀϦ¡´Â °¡Àå ³ôÀº ¿À·Î¶ó À¯±¤(×µÎÃ)¿¡ ÀÇÇØ¼ ½Äº°µÈ´Ù. |
The lower five or six miles of the earth's atmosphere is the troposphere; this is the region of winds and air currents which provide weather phenomena. Above this region is the inner ionosphere and next above is the stratosphere. Ascending from the surface of the earth, the temperature steadily falls for six or eight miles, at which height it registers around 70 degrees below zero F. This temperature range of from 65 to 70 degrees below zero F. is unchanged in the further ascent for forty miles; this realm of constant temperature is the stratosphere. At a height of forty-five or fifty miles, the temperature begins to rise, and this increase continues until, at the level of the auroral displays, a temperature of 1200¡Æ F. is attained, and it is this intense heat that ionizes the oxygen. But temperature in such a rarefied atmosphere is hardly comparable with heat reckoning at the surface of the earth. Bear in mind that one half of all your atmosphere is to be found in the first three miles. The height of the earth's atmosphere is indicated by the highest auroral streamers -- about four hundred miles. |
58:2.7 |
¿À·Î¶ó Çö»óÀº žç ÈæÁ¡, Áö±¸ÀÇ ¿´ë¼º ÆøÇ³¿ì°¡ ÀϾ´Â °Íó·³ Å¾çÀÇ Àûµµ À§¿Í ¾Æ·¡¿¡¼ ¹Ý´ë ¹æÇâÀ¸·Î ¼Ò¿ëµ¹ÀÌÄ¡´Â žçÀÇ ÆøÇ³°ú Á÷Á¢ °ü·ÃµÈ´Ù. ±×·¯ÇÑ ´ë±â±Ç ºÒ¾ÈÀº ÀûµµÀÇ À§¿Í ¾Æ·¡¿¡¼ »ý°åÀ» ¶§ ¹Ý´ë ¹æÇâÀ¸·Î ¼Ò¿ëµ¹ÀÌÄ¡°Ô µÈ´Ù. |
Auroral phenomena are directly related to sunspots, those solar cyclones which whirl in opposite directions above and below the solar equator, even as do the terrestrial tropical hurricanes. Such atmospheric disturbances whirl in opposite directions when occurring above or below the equator. |
58:2.8 |
ºûÀÇ ÆÄÀåÀ» º¯°æ½ÃŰ´Â Å¾ç ÈæÁ¡µéÀÇ ÈûÀº ÀÌ·¯ÇÑ ÅÂ¾ç ¼Ò¿ëµ¹ÀÌ Á߽ɺεéÀÌ ¸·°ÇÑ ÀÚ·Â(í¸Õô)ó·³ ±â´ÉÇÏ´Â °ÍÀ» º¸¿©ÁØ´Ù. ±×·¯ÇÑ ÀÚÀå(í¸íÞ)Àº žç ÈæÁ¡ ºÐȱ¸µé·ÎºÎÅÍ Áö±¸ ¹Ù±ùÂÊ ´ë±â·Î ´ëÀüµÈ ÀÔÀÚµéÀ» »Õ¾î³»¸ç, ±×°÷¿¡¼ ±×°ÍµéÀÇ ÀÌ¿ÂÈ ÀÛ¿ëÀÌ ±×·¯ÇÑ Àå°üÀÇ ¿À·Î¶ó Çö»óÀ» ³ªÅ¸³½´Ù. ±×·¯¹Ç·Î žç ÈæÁ¡ÀÌ ÃÖ°íÁ¡¿¡ ´ÞÇßÀ» ¶§¦¡È¤Àº ±× Á÷ÈÄ¿¡¦¡±× Á¡µéÀÌ º¸´Ù ÀϹÝÀûÀ¸·Î Àûµµ ºÎ±Ù¿¡ À§Ä¡ÇÏ¿´À» ¶§, °¡Àå Å« ¿À·Î¶ó Çö»óÀÌ ³ªÅ¸³´Ù. |
The power of sunspots to alter light frequencies shows that these solar storm centers function as enormous magnets. Such magnetic fields are able to hurl charged particles from the sunspot craters out through space to the earth's outer atmosphere, where their ionizing influence produces such spectacular auroral displays. Therefore do you have the greatest auroral phenomena when sunspots are at their height -- or soon thereafter -- at which time the spots are more generally equatorially situated. |
58:2.9 |
³ªÄ§¹Ýµµ ÀÌ·¯ÇÑ Å¾ç ÀÛ¿ëÀÇ ¿µÇâÀ» ¹Þ±â ¶§¹®¿¡, ÇØ°¡ ¶ã ¶§´Â ¾à°£ µ¿ÂÊÀ¸·Î Ä¡¿ìÄ¡°í ÇØ°¡ Áú ¹«·Æ¿¡´Â ¾à°£ ¼ÂÊÀ¸·Î Ä¡¿ìÄ¡´Â °ÍÀÌ´Ù. ÀÌ·¯ÇÑ Çö»óÀº ¸ÅÀÏ ÀϾ´Â °ÍÀÌÁö¸¸, žç ÈæÁ¡ ÁֱⰡ ³ôÀº °÷¿¡ ÀÖÀ» ¶§¿¡´Â ³ªÄ§¹ÝÀÇ ÀÌ·¯ÇÑ ÆíÂ÷´Â °ÅÀÇ µÎ ¹è¿¡ À̸£°Ô µÈ´Ù. ³¯¸¶´Ù ÀϾ´Â ³ªÄ§¹ÝÀÇ ÀÌ·¯ÇÑ º¯È´Â, ÅÂ¾ç ±¤¼±¿¡ ÀÇÇØ¼ ÀϾ´Â »óÃþºÎ ´ë±âÀÇ Áõ°¡µÈ ÀÌ¿ÂÈ Çö»ó¿¡ ´ëÇÑ ¹ÝÀÀÀÌ´Ù. |
Even the compass needle is responsive to this solar influence since it turns slightly to the east as the sun rises and slightly to the west as the sun nears setting. This happens every day, but during the height of sunspot cycles this variation of the compass is twice as great. These diurnal wanderings of the compass are in response to the increased ionization of the upper atmosphere, which is produced by the sunlight. |
58:2.10 |
³ÊÈñµéÀÌ Çϰí ÀÖ´Â ÀåÆÄ ±×¸®°í ´ÜÆÄ ¹æ¼ÛÀÌ ¸Õ °Å¸®±îÁö µµ´ÞÇÒ ¼ö ÀÖ´Â ÀÌÀ¯´Â ¼ºÃþ±Ç ¹Û¿¡ ÀÖ´Â ¼·Î ´Ù¸¥ Á¤µµ·Î ÃæÀüµÈ µÎ °³ÀÇ Àüµµ(îîÓô) ±¸¿ªÀÌ ÇöÁ¸Çϱ⠶§¹®ÀÌ´Ù. ³ÊÈñµéÀÌ Çϰí ÀÖ´Â ¹æ¼Û »óÅ´ ÀÌ·¯ÇÑ ¿ÜºÎ Àü¸®ÃþµéÀÇ ±¸¿ª¿¡¼ °¡²û °Å¼¼°Ô ÀϾ´Â ½ÉÇÑ ÆøÇ³¿ì¿¡ ÀÇÇØ¼ ¶§·Î ±³¶õµÇ±âµµ ÇÑ´Ù. |
It is the presence of two different levels of electrified conducting regions in the superstratosphere that accounts for the long-distance transmission of your long- and short-wave radiobroadcasts. Your broadcasting is sometimes disturbed by the terrific storms which occasionally rage in the realms of these outer ionospheres. |
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58:3.1 |
¿ìÁÖ ¹°ÁúÈÀÇ Ãʱ⠱Ⱓ µ¿¾È¿¡, °ø°£ ±¸¿ªµéÀº °Å´ëÇÑ ¼ö¼Ò ±¸¸§µé, ¸Õ °ø°£¿¡ µÎ·ç ¸¹Àº ±¸¿ªµéÀ» Áö±Ýµµ Ư¡Áþ´Â ±×·¸°Ô ±¤´ëÇÑ ¸ÕÁö ±º(ÏØ)µé·Î °¡µæ Â÷ ÀÖ¾ú´Ù. °·ÄÇÑ Å¾çµéÀÌ ÆÄ±«ÇÏ°í º¹»ç ¿¡³ÊÁöó·³ ºÐ»ê½ÃŲ À¯±âü ¹°ÁúÀÇ ´ëºÎºÐÀº ±â¿øÀûÀ¸·Î Ãʱ⿡ ³ªÅ¸³ °ø°£ÀÇ ¼ö¼Ò ±¸¸§µé ¼Ó¿¡¼ Çü¼ºµÇ¾ú´Ù. ¾î¶² Ưº°ÇÑ Á¶°Ç ¾Æ·¡¿¡¼, º¸´Ù Å« ¼ö¼Ò µ¢¾î¸®µéÀÇ Çٽɺο¡ ¿øÀÚ ºÐ¿ÀÌ ¹ß»ýÇÏ¿´´Ù. ÀÌ·¯ÇÑ ¿øÀÚ »ý¼º °ú ºÐ¿ÀÇ ¸ðµç Çö»óÀº, ±Øµµ·Î °¡¿µÈ ¼º¿î¿¡¼ ÀϾ ¶§, º¹»ç ¿¡³ÊÁöÀÇ ÂªÀº °ø°£ ±¤¼±µéÀÇ ºÐÃâµÇ´Â ¹Ð¹°ÀÇ Ã¢¹ßÀÌ µÚµû¸¥´Ù. µ¿¹ÝÇÏ´Â ÀÌ·¯ÇÑ ´Ù¾çÇÑ ¹æ»çµéÀº À¯¶õ½Ã¾Æ¿¡¼ ¾Ë·ÁÁ® ¾ÊÀº °ø°£-¿¡³ÊÁöÀÇ ÇüÅÂÀÌ´Ù. |
During the earlier times of universe materialization the space regions are interspersed with vast hydrogen clouds, just such astronomic dust clusters as now characterize many regions throughout remote space. Much of the organized matter which the blazing suns break down and disperse as radiant energy was originally built up in these early appearing hydrogen clouds of space. Under certain unusual conditions atom disruption also occurs at the nucleus of the larger hydrogen masses. And all of these phenomena of atom building and atom dissolution, as in the highly heated nebulae, are attended by the emergence of flood tides of short space rays of radiant energy. Accompanying these diverse radiations is a form of space-energy unknown on Urantia. |
58:3.2 |
¿ìÁÖ °ø°£ÀÇ ÀÌ ´ÜÆÄ ¹æ»ç¼± ¿¡³ÊÁö ÃæÀüÀº À¯±âü °ø°£ ±Ç¿ªµé ¼Ó¿¡ Á¸ÀçÇÏ´Â ¸ðµç ´Ù¸¥ º¹»ç ¿¡³ÊÁöÀÇ Çüŵ麸´Ù 400¹è³ª ´õ Å©´Ù. ªÀº °ø°£ º¹»ç¼±µéÀÇ Ãâ·ÂÀÌ, Ÿ¿À¸£´Â ¼º¿îÀ¸·ÎºÎÅÍ, ÆØÆØÇÑ Àü±âÀåÀ¸·ÎºÎÅÍ, ¿ÜºÎ °ø°£À¸·ÎºÎÅÍ, ¶Ç´Â ±¤´ëÇÑ ¼ö¼Ò ¸ÕÁö ±¸¸§µé·ÎºÎÅÍ ¿À´øÁö, ¿Âµµ¿Í Áß·Â ±×¸®°í Àü±âÀû ¾Ð·ÂÀÇ ÆÄµ¿°ú ±×°Íµé ¼Ó¿¡ °©ÀÚ±â ÀϾ´Â Àå·ÂÀÇ º¯Èµé¿¡ ÀÇÇØ¼ ¾çÀûÀ¸·Î ±×¸®°í ÁúÀûÀ¸·Î º¯ÈµÈ´Ù. |
This short-ray energy charge of universe space is four hundred times greater than all other forms of radiant energy existing in the organized space domains. The output of short space rays, whether coming from the blazing nebulae, tense electric fields, outer space, or the vast hydrogen dust clouds, is modified qualitatively and quantitatively by fluctuations of, and sudden tension changes in, temperature, gravity, and electronic pressures. |
58:3.3 |
ÀÌ·¯ÇÑ °ø°£ ±¤¼±µéÀÇ ±â¿ø¿¡¼ »ý°Ü³ª´Â °ÍµéÀº ȸÀüÇÏ´Â ¹°ÁúÀÇ ±Ëµµ¿¡ ÀÇÇØ¼ »Ó¸¸ ¾Æ´Ï¶ó ¸¹Àº Á¶È¿ìÁÖ »ç°Çµé¿¡ ÀÇÇØ¼ °áÁ¤µÇ¸ç, º¯ÇüµÈ ¿øÀ¸·ÎºÎÅÍ ±Ø½ÉÇÑ Å¸¿øÇü¿¡ À̸£±â±îÁö ´Ù¾çÇÏ´Ù. µ¿ÀÏÇÑ ¹°¸®Àû Áö´ë ¾È¿¡¼Á¶Â÷, º¸´Ù Å« ¹°ÁúÀÇ ¿îµ¿°ú´Â °£È¤ ¹Ý´ë ¹æÇâÀ¸·Î ÀüÀÚÀÇ È¸ÀüÀÌ ÀϾ±â ¶§¹®¿¡, ¹°¸®ÀûÀÎ Á¶°Çµé ¿ª½Ã Å©°Ô º¯°æµÉ ¼ö ÀÖ´Ù. |
These eventualities in the origin of the space rays are determined by many cosmic occurrences as well as by the orbits of circulating matter, which vary from modified circles to extreme ellipses. Physical conditions may also be greatly altered because the electron spin is sometimes in the opposite direction from that of the grosser matter behavior, even in the same physical zone. |
58:3.4 |
±¤´ëÇÑ ¼ö¼Ò ±¸¸§µéÀº ½ÇÁ¦ÀûÀÎ Á¶È¿ìÁÖ ÈÇÐÀû ½ÇÇèÀåÀ̸ç, ÁøÈÇÏ´Â ¿¡³ÊÁö¿Í º¯ÇüµÇ´Â ¹°Áú¿¡ ´ëÇÑ ¸ðµç Çö»óµéÀ» °ÅµÎ¾îµÐ´Ù. ¶ÇÇÑ °Å´ëÇÑ ¿¡³ÊÁö Ȱµ¿µéÀÌ, ¸Å¿ì ºó¹øÇÏ°Ô °ãÃÄÁüÀ¸·Î½á ±¤¹üÀ§ÇÏ°Ô µÚ¼¯ÀÌ´Â °Å´ëÇÑ ¿î¼ºµéÀÇ º¯µÎ¸®¿¡ ÀÖ´Â °¡½ºµé ¼Ó¿¡¼ ¹ß»ýµÈ´Ù. ±×·¯³ª ÀÌ °Å´ëÇÏ°í ³Î¸® ÆÛÁø °ø°£ÀÇ ¿¡³ÊÁö Ȱµ¿µéÀº À¯±âÀû »ý¸í¦¡»ì¾ÆÀÖ´Â ¹°Ã¼¿Í Á¸ÀçµéÀÇ ¼¼Æ÷¿øÇüÁú¦¡¿¡ ÀÛÀº ¿µÇâµµ ³¢Ä¡Áö ¾Ê´Â´Ù. °ø°£ÀÇ ÀÌ·¯ÇÑ ¿¡³ÊÁö »óŵéÀº »ý¸í Á¶¼ºÀ» À§ÇÑ ±âº»ÀûÀΠȯ°æ°ú ¹ÐÁ¢ÇÑ °ü°è°¡ ÀÖÁö¸¸, º¹»ç ¿¡³ÊÁöÀÇ º¸´Ù ±ä ¹æ»ç¼±µéÀÇ ¾î¶² °ÍµéÀÌ ±×·± °Íó·³ ¼¼Æ÷ ¿øÇüÁúÀÇ ¿øÃÊÀûÀÎ ¿ä¼ÒµéÀÇ µÚÀ̾î ÀϾ´Â º¯Çü¿¡ È¿·ÂÀ» ¹ÌÄ¡Áö ¾Ê´Â´Ù. »ý¸í ¿î¹ÝÀÚµéÀÌ À̽ÄÇÑ »ý¸íÀº ¿ìÁÖ ¿¡³ÊÁöÀÇ ÂªÀº °ø°£ ¹æ»ç ±¤¼±µéÀÇ ÀÌ ¾öû³ È«¼ö¿¡ ¸ðµÎ Ãæ¸¸ÇÑ ÀúÇ×·ÂÀ» °®°í ÀÖ´Ù |
The vast hydrogen clouds are veritable cosmic chemical laboratories, harboring all phases of evolving energy and metamorphosing matter. Great energy actions also occur in the marginal gases of the great binary stars which so frequently overlap and hence extensively commingle. But none of these tremendous and far-flung energy activities of space exerts the least influence upon the phenomena of organized life -- the germ plasm of living things and beings. These energy conditions of space are germane to the essential environment of life establishment, but they are not effective in the subsequent modification of the inheritance factors of the germ plasm as are some of the longer rays of radiant energy. The implanted life of the Life Carriers is fully resistant to all of this amazing flood of the short space rays of universe energy. |
58:3.5 |
¸ðµç ±âº»ÀûÀ¸·Î ÇÊ¿äÇÑ ÀÌ Á¶È¿ìÁÖ Á¶°ÇµéÀº, »ý¸í¿î¹ÝÀÚµéÀÌ À¯¶õ½Ã¾Æ¿¡ »ý¸í Çü¼ºÀ» ½ÇÁ¦ÀûÀ¸·Î ½ÃÀÛÇÒ ¼ö ÀÖ´Â ½Ã±â°¡ µÇ±â Àü¿¡, Àû´çÇÑ »óÅ·ΠÁøÈµÇ¾î¾ß¸¸ ÇÏ¿´´Ù. |
All of these essential cosmic conditions had to evolve to a favorable status before the Life Carriers could actually begin the establishment of life on Urantia. |
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58:4.1 |
¿ì¸®°¡ »ý¸í¿î¹ÝÀÚ¶ó°í ºÒ¸®´Â °Í ¶§¹®¿¡ ³ÊÈñµéÀÌ È¥µ¿À» ÀÏÀ¸ÄѼ´Â ¾È µÉ °ÍÀÌ´Ù. ¿ì¸®°¡ ¿©·¯ Ç༺µé¿¡°Ô »ý¸íÀ» ¿î¹ÝÇØ ÁÙ ¼öµµ ÀÖ°í ¶Ç ±×·¸°Ô Çϱ⵵ ÇÏÁö¸¸, À¯¶õ½Ã¾Æ¿¡´Â ¾î¶² »ý¸íµµ °¡Á®¿ÀÁö ¾Ê¾Ò´Ù. À¯¶õ½Ã¾ÆÀÇ »ý¸íÀº µ¶Æ¯ÇÑ °ÍÀ̸ç Áö±¸·ÎºÎÅÍ ¹ß»ýµÈ °ÍÀÌ´Ù. À̰÷ ±¸Ã¼´Â »ý¸í-º¯ÇüÀÇ ¼¼°èÀ̸ç; À̰÷¿¡ ³ªÅ¸³ ¸ðµç »ý¸íÀº ¹Ù·Î ÀÌ Áö±¸ À§¿¡¼ ¿ì¸®°¡ Çü¼ºÇÏ¿´´Ù; À¯¶õ½Ã¾ÆÀÇ »ý¸í°ú ¶È°°Àº »ý¸íÀÌ ½ÇÀçÇÏ´Â ¼¼°è´Â »çŸ´Ï¾ÆÀÇ Àü Áö¿ª¿¡ ÀüÇô ½ÇÀçÇÏÁö ¾ÊÀ¸¸ç, ³×¹Ùµ· Àü¿ª¿¡¼µµ ã¾Æº¼ ¼ö ¾ø´Ù. |
That we are called Life Carriers should not confuse you. We can and do carry life to the planets, but we brought no life to Urantia. Urantia life is unique, original with the planet. This sphere is a life-modification world; all life appearing hereon was formulated by us right here on the planet; and there is no other world in all Satania, even in all Nebadon, that has a life existence just like that of Urantia. |
58:4.2 |
550,000,000³â Àü¿¡, »ý¸í¿î¹ÝÀÚ ¹«¸®´ÜÀº À¯¶õ½Ã¾Æ·Î µ¹¾Æ¿Ô´Ù. ¿ì¸®´Â ¿µÀûÀÎ Èûµé°ú ÃÊ(õ±)¹°¸®Àû ±â¼¼µé°ú Çù·ÂÇÏ¿©, ÀÌ ¼¼°è¿¡ ´ëÇÑ ±â¿øÀûÀÎ »ý¸í ¿øÇüƲµéÀ» Á¶Á÷Çϰí â½ÃÇÏ¿´À¸¸ç ±¸Ã¼ÀÇ ÄèÀûÇÑ ¹°¼Ó¿¡ ±×°ÍµéÀ» ½É¾ú´Ù. Ç༺¿µÁÖÀÎ Ä®¸®°¡½ºÆ¼¾ÆÀÇ ½Ã´ë¿¡ À̸£±â±îÁö ¸ðµç Ç༺ »ý¸íÀº (°¡¿ÜÇ༺ °³ÀμºµéÀº Á¦¿ÜÇϰí) ¿ì¸®µéÀÇ ±â¿øÀûÀÌ°í µ¿ÀÏÇÏ¸ç µ¿½ÃÀûÀÎ ¼¼ °³ÀÇ ÇØ¾ç-»ý¸í À̽ĵ鿡 ÀÇÇØ ±â¿øµÇ¾ú´Ù. ÀÌ·¯ÇÑ ¼¼ °³ÀÇ »ý¸í À̽ĵéÀº ´ÙÀ½°ú °°ÀÌ ¼±Á¤µÇ¾ú´Ù: Áß¾Ó È¤Àº À¯¶ó½Ã¾Æ-¾ÆÇÁ¸®Ä«, µ¿ºÎ ȤÀº ¿À½ºÆ®¶ö¶ó½Ã¾Æ Áö¿ª, ±×¸®°í ±×¸°¶õµå¿Í ¾Æ¸Þ¸®Ä« ´ë·úÀ» Æ÷ÇÔÇÏ´Â ¼ºÎ Áö¿ªÀÌ´Ù. |
550,000,000 years ago the Life Carrier corps returned to Urantia. In co-operation with spiritual powers and superphysical forces we organized and initiated the original life patterns of this world and planted them in the hospitable waters of the realm. All planetary life (aside from extraplanetary personalities) down to the days of Caligastia, the Planetary Prince, had its origin in our three original, identical, and simultaneous marine-life implantations. These three life implantations have been designated as: the central or Eurasian-African, the eastern or Australasian, and the western, embracing Greenland and the Americas. |
58:4.3 |
500,000,000³â Àü¿¡, ¿ø½Ã ÇØ¾ç ½Ä¹° »ý¸íÀÌ À¯¶õ½Ã¾Æ¿¡ ¼º°øÀûÀ¸·Î ŵ¿µÇ¾ú´Ù. ³²-ºÏ ¾Æ¸Þ¸®Ä«¸¦ À§½ÃÇÏ¿© ±×¸°¶õµå¿Í ºÏ±Ø ´ë·úÀÌ ¼ÂÊÀ¸·Î ¿À·§µ¿¾È ¼¼È÷ Ç¥·ùÇϱ⠽ÃÀÛÇÏ¿´´Ù. ¾ÆÇÁ¸®Ä«´Â µ¿Âʰú ¼ÂÊ¿¡ ¹Ù´Ù °ñÂ¥±â, º»·¡ÀÇ ´ë·ú°ú ¾ÆÇÁ¸®Ä« ´ë·ú »çÀÌ¿¡ ÀÖ´Â ÁöÁßÇØ ºÐÁö¸¦ Á¶¼ºÇÏ¸é¼ ¾à°£ ³²ÂÊÀ¸·Î À̵¿ÇÏ¿´´Ù. ³²±Ø ´ë·ú°ú ¿À½ºÆ®·¹Àϸ®¾Æ ±×¸®°í ÅÂÆò¾çÀÇ ¼¶µé¿¡ ÀÇÇØ¼ ±× ÈçÀûÀ» ¾Ë ¼ö ÀÖ´Â ´ë·úÀÌ ³²µ¿ÂÊÀ¸·Î ¶³¾îÁ® ³ª°¬°í ±× ³¯ ÀÌÈÄ·Î ¸Ö¸® ¶°³»·Á°¬´Ù. |
500,000,000 years ago primitive marine vegetable life was well established on Urantia. Greenland and the arctic land mass, together with North and South America, were beginning their long and slow westward drift. Africa moved slightly south, creating an east and west trough, the Mediterranean basin, between itself and the mother body. Antarctica, Australia, and the land indicated by the islands of the Pacific broke away on the south and east and have drifted far away since that day. |
58:4.4 |
¿ì¸®´Â ºÐ¸®µÇ´Â ´ë·ú ¶¥ µ¢¾î¸®ÀÇ µ¿-¼ ¹æÇâ °ñÂ¥±â¿¡ ÀÖ´Â Áß¾Ó ¹Ù´ÙÀÇ º¸È£µÈ ¿´ë ±âÈÄÀÇ ¸¸(ؽ)µé ¼Ó¿¡ ¿ø½Ã ÇüÅÂÀÇ ÇØ¾ç »ý¸íÀ» ½É¾ú´Ù. ¼¼ °³ÀÇ ÇØ¾ç »ý¸í À̽ÄÀ» ½ÃÇàÇÏ´Â ¿ì¸®µéÀÇ ¸ñÀûÀº ³ªÁß¿¡ ¶¥ÀÌ ºÐ¸®µÇ¾î ³ª°¥ ¶§, °¢°¢ÀÇ ´ë·ú ¶¥ µ¢¾î¸®µéÀÌ ±× ¿ÂÈÇÑ ¹Ù´å¹° ¼Ó¿¡ ÀÌ »ý¸íÀ» Àß °¡Á®°¡´Â °ÍÀ» È®½ÇÈ÷ Çϱâ À§Çؼ¿´´Ù. ¿ì¸®´Â ¶¥ÀÇ »ý¸íÀÌ Åµ¿µÇ´Â Èı⠽ô뿡, Ç¥·ùÇÏ´Â ÀÌ ´ë·ú ¶¥ µ¢¾î¸®µéÀÌ °Å´ëÇÑ ÇØ¾çÀÇ ¹°·Î¼ ºÐ¸®µÈ´Ù´Â °ÍÀ» ¹Ì¸® ³»´Ùº¸¾Ò´Ù. |
We had planted the primitive form of marine life in the sheltered tropic bays of the central seas of the east-west cleavage of the breaking-up continental land mass. Our purpose in making three marine-life implantations was to insure that each great land mass would carry this life with it, in its warm-water seas, as the land subsequently separated. We foresaw that in the later era of the emergence of land life large oceans of water would separate these drifting continental land masses. |
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58:5.1 |
´ë·úÀÇ ¶¥ÀÇ Ç¥·ù´Â °è¼ÓµÇ¾ú´Ù. Áö±¸ÀÇ Çٽɺδ ÀÔ¹æ ÀÎÄ¡´ç °ÅÀÇ 25,000Åæ¿¡ ´ÞÇÏ´Â ¾Ð·ÂÀÌ °¡ÇØÁ®¼ Á߷¿¡ ÀÇÇÑ ¾öû³ ¾Ð·Â ¶§¹®¿¡, ¼èó·³ ³óµµ°¡ £¾îÁö°í ´Ü´ÜÇØÁ³À¸¸ç, ³»ºÎ ±í¼÷ÇÑ °÷Àº ±× ¶§¿Í ¸¶Âù°¡Áö·Î Áö±Ýµµ ±²ÀåÈ÷ °¡¿µÇ¾îÀÖ´Ù. ÁöÇ¥¸éÀ¸·ÎºÎÅÍ ¾Æ·¡·Î ³»·Á°¡¸é¼ ¿Âµµ´Â Á¡Â÷ Áõ°¡Çϸç Á᫐ ºÎºÐÀº žçÀÇ Ç¥¸é ¿Âµµº¸´Ù ¾à°£ ´õ ³ô´Ù. |
The continental land drift continued. The earth's core had become as dense and rigid as steel, being subjected to a pressure of almost 25,000 tons to the square inch, and owing to the enormous gravity pressure, it was and still is very hot in the deep interior. The temperature increases from the surface downward until at the center it is slightly above the surface temperature of the sun. |
58:5.2 |
Áö±¸ µ¢¾î¸®ÀÇ ¹Ù±ùÇ¥¸é 1,000¸¶ÀÏÀº ÁÖ·Î ´Ù¾çÇÑ Á¾·ùÀÇ ¹ÙÀ§·Î ±¸¼ºµÇ¾î ÀÖ´Ù. ±× ¹ØÀ¸·Î´Â º¸´Ù Á¶¹ÐÇÏ°í ¹«°Å¿î ±Ý¼Ó ¼ººÐÀ¸·Î ÀÌ·ç¾îÁ® ÀÖ´Ù. Ãʱ⠱׸®°í ´ë±â±ÇÀÌ »ý±â±â ÀüÀÇ ½Ã´ë Àüü µ¿¾È¿¡´Â ¼¼°è´Â ¶ß°Ì°Ô °¡¿µÇ°í ³ì¾Æ ÀÖ¾î¼ °ÅÀÇ ¾×ü »óÅ¿¡ ÀÖ¾úÀ¸¹Ç·Î ¹«°Å¿î ±Ý¼Ó ¼ººÐµéÀÌ ¾ÈÂÊÀ¸·Î °¡¶ó¾É¾Ò´Ù. ¿À´Ã³¯ Ç¥¸é ±Ùó¿¡¼ ¹ß°ßµÇ´Â °ÍµéÀº °í´ëÀÇ È»ê Ȱµ¿¿¡ ÀÇÇØ¼ ºÐÃâµÈ °Íµé, ³ªÁß¿¡ ´ë±Ô¸ðÀÇ ¿ë¾ÏÀ¸·Î Èê·¯³ª¿Â °Íµé, ±×¸®°í ±×º¸´Ù ´õ Èı⿡ ¿î¼®µé¿¡ ÀÇÇØ ½×ÀÎ °ÍÀÌ´Ù. |
The outer one thousand miles of the earth's mass consists principally of different kinds of rock. Underneath are the denser and heavier metallic elements. Throughout the early and preatmospheric ages the world was so nearly fluid in its molten and highly heated state that the heavier metals sank deep into the interior. Those found near the surface today represent the exudate of ancient volcanoes, later and extensive lava flows, and the more recent meteoric deposits. |
58:5.3 |
ÁöÇ¥ÃþÀº ¾à 40¸¶ÀÏÀÇ µÎ²²·Î µÇ¾î ÀÖ´Ù. ¿ÜºÎ¸¦ µÑ·¯½Î°í ÀÖ´Â ÀÌ ²®Áú ºÎºÐÀº ´Ù¾çÇÑ µÎ²²ÀÇ ³ì¾Æ ÀÖ´Â Çö¹«¾Ï ¹Ù´Ù ¹Ù·Î À§¿¡ ¶° ÀÖ°í ±×°Í¿¡ ÀÇÇØ¼ ÁöÅʵǰí ÀÖÀ¸¸ç, ¹Ù´Ù´Â ³ì¾ÆÀÖ´Â ¿ë¾ÏÀ¸·Î µÈ À¯µ¿ÇÏ´Â ÃþÀ¸·Î½á, ³ôÀº ¾Ð·Â ¾Æ·¡¿¡¼ À¯ÁöµÇ°í ÀÖÁö¸¸ º¯ÈÇÏ´Â Áö±¸ ¾Ð·ÂÀ» ±ÕµîÇÏ°Ô À¯ÁöÇÏ¿© Áö±¸ Ç¥¸éÀ» ¾ÈÁ¤ÈÇϱâ À§ÇØ Ç×»ó À̵¿ÇÏ´Â °æÇâÀ» °¡Áö°í ÀÖ´Ù. |
The outer crust was about forty miles thick. This outer shell was supported by, and rested directly upon, a molten sea of basalt of varying thickness, a mobile layer of molten lava held under high pressure but always tending to flow hither and yon in equalization of shifting planetary pressures, thereby tending to stabilize the earth's crust. |
58:5.4 |
¿À´Ã³¯¿¡µµ ´ë·úµéÀº ³ì¾ÆÀÖ´Â Çö¹«¾ÏÀ¸·Î ÀÌ·ç¾îÁø ºÎµå·´°í Ç«½ÅÇ«½ÅÇÑ ÀÌ ¹Ù´Ù À§¿¡ ¿©ÀüÈ÷ ¶° ÀÖ´Ù. ÀÌ·¯ÇÑ º¸È£ ȯ°æÀÌ ¾Æ´Ï¾ú´Ù¸é, º¸´Ù ½É°¢ÇÑ ÁöÁøµéÀÌ ¼¼»óÀ» Èçµé¾î¼ ±×¾ß¸»·Î »ê»êÁ¶°¢ ³»¾úÀ» °ÍÀÌ´Ù. ÁöÁøµéÀº È»ê Æø¹ß¿¡ ÀÇÇØ¼°¡ ¾Æ´Ï¶ó µüµüÇÑ ÁöÇ¥ÃþÀÌ ¹Ì²ô·¯Áö°í À§Ä¡°¡ º¯°æµÇ±â ¶§¹®¿¡ ¹ß»ýµÈ´Ù. |
Even today the continents continue to float upon this noncrystallized cushiony sea of molten basalt. Were it not for this protective condition, the more severe earthquakes would literally shake the world to pieces. Earthquakes are caused by sliding and shifting of the solid outer crust and not by volcanoes. |
58:5.5 |
Áö±¸ Áö°¢ÀÇ ¿ë¾ÏÃþÀÌ ³Ã°¢µÇ¸é Ȱ¾ÏÀÌ µÈ´Ù. À¯¶õ½Ã¾ÆÀÇ Æò±Õ ºñÁßÀº ¹° ºñÁßÀÇ 5.5¹èº¸´Ù ¾à°£ ´õ ¹«°Å¿ì¸ç; Ȱ¾ÏÀÇ ºñÁßÀº ¹° ºñÁßÀÇ 3¹èº¸´Ù Á¶±Ý °¡º±´Ù. Áö±¸ Çٽɺδ ¹° ºñÁßÀÇ 12¹è¿¡ ÇØ´çµÈ´Ù. |
The lava layers of the earth's crust, when cooled, form granite. The average density of Urantia is a little more than five and one-half times that of water; the density of granite is less than three times that of water. The earth's core is twelve times as dense as water. |
58:5.6 |
¹Ù´Ù ¹Ø¹Ù´ÚÀº ¶¥ µ¢¾î¸®µéº¸´Ù ´õ ¹Ðµµ°¡ ³ôÀ¸¸ç, ÀÌ°Í ¶§¹®¿¡ ¹° À§·Î ¼Ú¾Æ³ª ÀÖ´Â ´ë·úµéÀÌ À¯ÁöµÇ´Â °ÍÀÌ´Ù. ¹Ù´Ù ¹Ø¹Ù´ÚÀÌ ÇØ¼ö¸é À§·Î µ¹ÃâÇÏ°Ô µÇ¸é, ±×°ÍµéÀÌ ÁÖ·Î Çö¹«¾Ï, ¶¥ À§¿¡ Àִ Ȱ¾Ïº¸´Ù ÈξÀ ´õ ¹«°Å¿î ¿ë¾ÏÀÇ ÇüÅ·ΠµÇ¾î ÀÖÀ½ÀÌ ¹ß°ßµÈ´Ù. ´Ù½Ã ¸»Çؼ, ´ë·úÀÌ ÇØÀúº¸´Ù °¡º±Áö ¾Ê´Ù¸é, Á߷¿¡ ÀÇÇØ¼ ¹Ù´å¹°ÀÌ ¶¥ À§·Î ¿Ã¶ó¿À°Ô µÇ°ÚÁö¸¸, ±×·¯ÇÑ Çö»óÀº °üÂûµÇÁö ¾Ê´Â´Ù. |
The sea bottoms are more dense than the land masses, and this is what keeps the continents above water. When the sea bottoms are extruded above the sea level, they are found to consist largely of basalt, a form of lava considerably heavier than the granite of the land masses. Again, if the continents were not lighter than the ocean beds, gravity would draw the edges of the oceans up onto the land, but such phenomena are not observable. |
58:5.7 |
¶ÇÇÑ ÇØ¾çÀÇ ¹«°Ô´Â ÇØÀú¿¡ Á¡Á¡ ´õ ¼¾ ¾Ð·ÂÀ» °¡ÇÏ´Â ¿äÀÎÀ̱⵵ÇÏ´Ù. º¸´Ù ³·Àº °÷¿¡ ÀÖÁö¸¸ ºñ±³Àû ´õ ¹«°Å¿î ÇØÀúÀÇ ÁöÃþµéÀº, ±× À§¿¡ ÀÖ´Â ¹°ÀÇ ¹«°Ô¸¦ ´õÇØÁø º¸´Ù ³ôÀº °÷¿¡ ÀÖÁö¸¸ º¸´Ù °¡º¿î ´ë·úµéÀÇ ¹«°Ô¿Í ºñ½ÁÇÏ´Ù. ±×·¯³ª ¸ðµç ´ë·úµéÀº ÇØ¾ç ÂÊÀ¸·Î ¼¼È÷ ¿òÁ÷ÀÌ·Á´Â °æÇâÀÌ ÀÖ´Ù. ÇØÀú °èÃþ¿¡¼ ´ë·úÀÌ ÁÖ´Â ¾Ð·ÂÀº Æò¹æ ¼¾Æ¼¹ÌÅÍ ´ç ¾à 550 ų·Î±×·¥¿¡ ´ÞÇÑ´Ù. ´Ù½Ã ¸»Çؼ, À̰ÍÀº ÇØÀú·ÎºÎÅÍ 4,600¹ÌÅÍ·Î ¼Ú¾Æ ÀÖ´Â ´ë·úÀÌ °¡ÇÏ´Â ¾Ð·ÂÀÌ µÉ °ÍÀÌ´Ù. ÇØÀúÀÇ ¼ö¾ÐÀº Æò¹æ ¼¾Æ¼¹ÌÅÍ ´ç ¾à 137 ų·Î±×·¥¿¡ ºÒ°úÇÏ´Ù. ÀÌ·¯ÇÑ ¾Ð·Â Â÷ÀÌ´Â ´ë·úÀÌ ÇØÀú ÂÊÀ¸·Î ¹Ì²ô·¯Áöµµ·Ï ÇÏ´Â ¿øÀÎÀ» Á¦°øÇÑ´Ù. |
The weight of the oceans is also a factor in the increase of pressure on the sea beds. The lower but comparatively heavier ocean beds, plus the weight of the overlying water, approximate the weight of the higher but much lighter continents. But all continents tend to creep into the oceans. The continental pressure at ocean-bottom levels is about 20,000 pounds to the square inch. That is, this would be the pressure of a continental mass standing 15,000 feet above the ocean floor. The ocean-floor water pressure is only about 5,000 pounds to the square inch. These differential pressures tend to cause the continents to slide toward the ocean beds. |
58:5.8 |
»ý¸íÀÌ Á¸ÀçÇϱâ ÀÌÀü ½Ã´ë µ¿¾È¿¡ ÇØÀúÀÇ Ä§°Àº, Çϳª»ÓÀ̾ú´ø ´ë·úÀÇ ¶¥ µ¢¾î¸®¸¦ ¹Ð¾î ¿Ã·Á¼, Ãø¸éÀÇ ¾Ð·ÂÀÌ µ¿Âʰú ¼ÂÊ ±×¸®°í ³²ÂÊ °¡ÀåÀÚ¸®°¡ ºñÅ»±æ·Î ¹Ì²ô·´°Ô ³»·Á°¡, µÑ·¯½Î°í ÀÖ´Â ÅÂÆò¾ç ¹Ù´ÙÀÇ ¹°¼Ó¿¡ µé¾î°¡, ¹Ø¿¡ ±ò·ÁÀÖ´Â ¹ÝÂë ²öÀû°Å¸®´Â ¿ë¾Ï À§·Î ±×·¸°Ô ¹Ì²ô·¯Áö´Â ¿øÀÎÀÌ µÇ´Â ³ôÀÌ·Î ¹Ð¾î ¿Ã·È´Ù. À̰ÍÀÌ ´ë·úÀÇ ¾Ð·ÂÀ» ³Ê¹«³ª ÃæºÐÈ÷ º¸»óÇÏ¿´±â ¶§¹®¿¡ À̶§ÀÇ °í´ë ¾Æ½Ã¾Æ ´ë·ú µ¿ÂÊ¿¬¾È¿¡´Â Æø ³ÐÀº ±Õ¿ÀÌ ¹ß»ýµÇÁö´Â ¾Ê¾Ò´Ù, ±×·¯³ª ±× µ¿ÂÊ ÇØ¾ÈÀº ±× ÈÄ·Î °è¼Ó, ÀÎÁ¢ÇÑ ÇØ¾ç ½ÉÇØÀÇ ³¶¶°·¯Áö À§¿¡ ¸Éµ¹°í ÀÖ°í, ¹°¼Ó¿¡ ÀÖ´Â ¹«´ý ¼ÓÀ¸·Î ¹Ì²ô·¯Á® µé¾î°¡´Â À§ÇùÀ» ¹Þ°í ÀÖ´Ù. |
Depression of the ocean bottom during the prelife ages had upthrust a solitary continental land mass to such a height that its lateral pressure tended to cause the eastern, western, and southern fringes to slide downhill, over the underlying semiviscous lava beds, into the waters of the surrounding Pacific Ocean. This so fully compensated the continental pressure that a wide break did not occur on the eastern shore of this ancient Asiatic continent, but ever since has that eastern coast line hovered over the precipice of its adjoining oceanic depths, threatening to slide into a watery grave. |
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58:6.1 |
450,000,000³â Àü¿¡, ½Ä¹°·ÎºÎÅÍ µ¿¹° »ý¸íÀ¸·ÎÀÇ º¯ÃµÀÌ ÀϾ´Ù. ÀÌ·¯ÇÑ º¯È¯Àº ¾Æ´ÁÇÑ ¿´ë¼º ±âÈÄÀÇ ¸¸(ؽ)°ú, ºÐ¸®µÈ ´ë·úµéÀÇ ±¤´ëÇÑ ÇØº¯ÀÇ ÀÛÀº ´ËÀÇ ¾èÀº ¹°¼Ó¿¡¼ ÀÌ·ç¾îÁ³´Ù. ±×¸®°í ÀÌ·¯ÇÑ ¹ßÀüÀº ¸ðµÎ ±â¿øÀûÀÎ »ý¸í ¿øÇüƲµé ¼Ó¿¡ ¼±ÃµÀûÀ¸·Î ÀÖ´Â °ÍÀε¥, Á¡Â÷ÀûÀ¸·Î ³ª¿À°Ô µÇ¾ú´Ù. ÃʱâÀÇ ¿ø½Ã½Ä¹° ÇüÅÂÀÇ »ý¸í°ú ÈıâÀÇ Àß Á¶Á÷µÈ µ¿¹° À¯±âü »çÀÌ¿¡´Â ¸¹Àº º¯Ãµ ´Ü°è°¡ ÀÖ¾ú´Ù. ¿À´Ã³¯¿¡µµ °úµµ±â Á¡¾×ÁúÀÌ ÀÜÁ¸Çϰí ÀÖÀ¸¸ç, ±×°ÍµéÀº ½Ä¹°À̳ª µ¿¹°·Î ºÐ·ùÇϱ⵵ ¾î·Æ´Ù. |
450,000,000 years ago the transition from vegetable to animal life occurred. This metamorphosis took place in the shallow waters of the sheltered tropic bays and lagoons of the extensive shore lines of the separating continents. And this development, all of which was inherent in the original life patterns, came about gradually. There were many transitional stages between the early primitive vegetable forms of life and the later well-defined animal organisms. Even today the transition slime molds persist, and they can hardly be classified either as plants or as animals. |
58:6.2 |
½Ä¹°»ý¸í¿¡¼ºÎÅÍ µ¿¹°»ý¸í¿¡ À̸£±â±îÁöÀÇ ÁøÈ¸¦ ÃßÀûÇÒ ¼ö ÀÖ´õ¶óµµ, ±×¸®°í °¡Àå ´Ü¼øÇÑ ÇüÅ·κÎÅÍ °¡Àå º¹ÀâÇÏ°í ¹ßÀüµÈ À¯±âü±îÁö Á¡ÁøÀûÀ¸·Î ÀÌ·ç¾îÁø ½Ä¹°µé°ú µ¿¹°µé¿¡ ´ëÇÑ Á¡ÁøÀûÀÎ ¿¬¼Ó¼ºÀ» ¹ß°ßÇÏ´õ¶óµµ, ³ÊÈñµéÀº µ¿¹°°èÀÇ ¾öû³ ºÐÇÒµéÀÇ »çÀÌ¿¡ ´ëÇÑ ¿¬°á °í¸®µéÀ» ¹ß°ßÇÒ ¼ö ¾øÀ» »Ó¸¸ ¾Æ´Ï¶ó Àΰ£-ÀÌÀü µ¿¹° À¯ÇüÀÇ °¡Àå ¹ßÀüµÈ °Í°ú Àΰ£ Á¾Á·ÀÇ ¿ø½ÃÀλçÀÌÀÇ ¿¬°á °í¸®µµ ¹ß°ßÇÒ ¼ö ¾øÀ» °ÍÀÌ´Ù. ¼ÒÀ§ ¡°ÀÒ¾î¹ö¸° ¿¬°á °í¸®µé¡±À̶ó°í ºÒ¸®´Â À̰͵éÀº ¾ðÁ¦±îÁö³ª ÀÒ¾î¹ö¸° »óÅ·Π³²¾ÆÀÖÀ» °ÍÀε¥, ±×°ÍÀº À̰͵éÀÌ ÀüÇô Á¸ÀçÇÏÁö ¾Ê¾Ò´Ù´Â ´Ü¼øÇÑ ÀÌÀ¯ ¶§¹®ÀÌ´Ù. |
Although the evolution of vegetable life can be traced into animal life, and though there have been found graduated series of plants and animals which progressively lead up from the most simple to the most complex and advanced organisms, you will not be able to find such connecting links between the great divisions of the animal kingdom nor between the highest of the prehuman animal types and the dawn men of the human races. These so-called "missing links" will forever remain missing, for the simple reason that they never existed. |
58:6.3 |
½Ã´ë°¡ ¹Ù²î¸é¼ º»ÁúÀûÀ¸·Î »õ·Î¿î µ¿¹° »ý¸íü Á¾(ðú)µéÀÌ ¹ß»ýÇÏ¿´´Ù. ±×°ÍµéÀº ¹Ì¼¼ÇÑ º¯ÈµéÀÌ Á¡Â÷ÀûÀ¸·Î ´©ÀûµÈ °á°ú·Î ÁøÈµÈ °ÍµéÀÌ ¾Æ´Ï´Ù; ±×µéÀº Ãæ¸¸ÇÑ-¼ºÀåÀÇ ¸ð½ÀÀ¸·Î ±×¸®°í »õ·Î¿î °èÃþÀÇ »ý¸íÀ¸·Î ³ªÅ¸³µÀ¸¸ç, °©Àڱ⠳ªÅ¸³µ´Ù. |
From era to era radically new species of animal life arise. They do not evolve as the result of the gradual accumulation of small variations; they appear as full-fledged and new orders of life, and they appear suddenly. |
58:6.4 |
»õ·Î¿î Á¾Á·µé°ú ´Ù¾çÇÑ °èÃþÀÇ »ý¸í À¯±âüµéÀÇ °©ÀÛ½º·¯¿î ÃâÇöÀº ÀüÀûÀ¸·Î »ý¹°ÇÐÀû, ¼øÀüÈ÷ ÀÚ¿¬ÀûÀÎ °ÍÀÌ´Ù. ÀÌ·¯ÇÑ À¯ÀüÀÚ µ¹¿¬º¯ÀÌ¿¡¼ ÃÊÀÚ¿¬ÀûÀÎ °£¼·Àº ÀüÇô °ü·ÃµÇÁö ¾Ê´Â´Ù. |
The sudden appearance of new species and diversified orders of living organisms is wholly biologic, strictly natural. There is nothing supernatural connected with these genetic mutations. |
58:6.5 |
ÇØ¾çÀÇ Àû´çÇÑ Á¤µµÀÇ ¼Ò±Ý±â ¼Ó¿¡¼ µ¿¹° »ý¸íÀÌ ÁøÈÇÏ¿´À¸¸ç, ÇØ¾ç »ý¸íÀÇ µ¿¹° ¸öü ¼ÓÀ¸·Î ¼Ò±Ý±âÀÇ ¹°ÀÌ ¼øÈ¯µÇµµ·Ï ÇÏ´Â °ÍÀº ºñ±³Àû °£´ÜÇÏ´Ù. ±×·¯³ª ÇØ¾çÀÌ ÁÙ¾îµé°í ¼Ò±Ý ³óµµ°¡ Á¡Â÷ÀûÀ¸·Î ³ô¾ÆÁöÀÚ, ¹Ù·Î ÀÌ µ¿¹°µéÀº, ¼Ò±Ý±â¸¦ º¸Á¸ÇÏ´Â µ¶Ã¢ÀûÀÎ ±â¹ý¿¡ ÀÇÇØ¼ ÀÚ½ÅÀÇ Ã¼¾× ¼Ó¿¡ Àû´çÇÑ Á¤µµÀÇ ¿°È³ªÆ®·ýÀ» À¯ÁöÇÏ´Â ´É·ÂÀ» ½ÀµæÇÏ¿© ¹Î¹° ¼Ó¿¡¼ »ýÁ¸µÇ´Â ¹æ¹ýÀ» üµæÇÑ ±× À¯±âüµé°ú ¶È°°ÀÌ, ÀÚ½ÅÀÇ Ã¼¾× ¼Ó¿¡ ÀÖ´Â ¼Ò±Ý±â¸¦ ÁÙÀÌ´Â ´É·ÂÀ» ÁøÈµÇ¾ú´Ù. |
At the proper degree of saltiness in the oceans animal life evolved, and it was comparatively simple to allow the briny waters to circulate through the animal bodies of marine life. But when the oceans were contracted and the percentage of salt was greatly increased, these same animals evolved the ability to reduce the saltiness of their body fluids just as those organisms which learned to live in fresh water acquired the ability to maintain the proper degree of sodium chloride in their body fluids by ingenious techniques of salt conservation. |
58:6.6 |
¹ÙÀ§ ¼Ó¿¡ µé¾î ÀÖ´Â ÇØ¾ç »ý¸í ȼ®µé¿¡ ´ëÇÑ ¿¬±¸°á°ú·Î, ÀÌµé ¿ø½Ã À¯±âüµéÀÇ Ãʱâ Á¶Àý ÅõÀïÀ» ¹ß°ßÇÒ ¼ö ÀÖ´Ù. ½Ä¹°µé°ú µ¿¹°µéÀº ÀÌ·¯ÇÑ Á¶Àý ½Ãµµ¸¦ ²÷ÀÓ¾øÀÌ Çϰí ÀÖ´Ù. ȯ°æÀÌ º¯ÈÇÒ ¶§¸¶´Ù, ±×¸®°í ¾ðÁ¦µçÁö, »ì¾ÆÀÖ´Â À¯±âüµéÀº ²÷ÀÓ¾ø´Â º¯È¿¡ ÀÚ±â ÀÚ½ÅÀ» ÀûÀÀ½Ã۱â À§ÇÏ¿© ¾Ö¾´´Ù. |
Study of the rock-embraced fossils of marine life reveals the early adjustment struggles of these primitive organisms. Plants and animals never cease to make these adjustment experiments. Ever the environment is changing, and always are living organisms striving to accommodate themselves to these never-ending fluctuations. |
58:6.7 |
»ý¸íÀÇ ¸ðµç »õ·Î¿î °èÃþµéÀÇ ÇØºÎÇÐÀû ±¸Á¶¿Í »ý¸®ÀûÀÎ ÀåÄ¡´Â ¹°¸® ¹ýÄ¢ÀÇ ÀÛ¿ë¿¡ ÀÀ´äÇÑ´Ù, ±×·¯³ª À̾îÁö´Â ¸¶À½ ÀÚÁúÀº Ÿ°í³ ³úÀÇ ¼ö¿ë ´É·Â¿¡ µû¸¥ º¸Á¶ ¸¶À½-¿µµéÀÇ Áõ¿©ÀÌ´Ù. ¸¶À½Àº ¹°¸®Àû ÁøÈ°¡ ¾Æ´Ï¶ó, ¼øÀüÈ÷ ¹°¸®ÀûÀ̰í ÁøÈÀûÀÎ ¼ºÀåµé¿¡ ÀÇÇØ¼ Á¦°øµÇ´Â ³úÀÇ ¼ö¿ë ´É·Â¿¡ ÀüÀûÀ¸·Î ÀÇÁ¸ÇÑ´Ù. |
The physiologic equipment and the anatomic structure of all new orders of life are in response to the action of physical law, but the subsequent endowment of mind is a bestowal of the adjutant mind-spirits in accordance with innate brain capacity. Mind, while not a physical evolution, is wholly dependent on the brain capacity afforded by purely physical and evolutionary developments. |
58:6.8 |
°ÅÀÇ ³¡¾øÀÌ ¼øÈ¯µÇ´Â ȹµæ°ú ¼Õ½Ç, Á¶Àý°ú Àç(î¢)Á¶ÀýÀ» ÅëÇÏ¿©, »ì¾ÆÀÖ´Â ¸ðµç À¯±âüµéÀº ½Ã´ëÀÇ È帧 ¼Ó¿¡¼ Å𺸠¶Ç´Â ÀüÁøÀÇ °úÁ¤À» µÇÇ®ÀÌÇÑ´Ù. Á¶È¿ìÁÖ ÇÕÀÏÀ» ´Þ¼ºÇÏ´Â Á¸ÀçµéÀº Á¸¼ÓµÇÁö¸¸, ÀÌ·¯ÇÑ ¸ñÇ¥¿¡ µµ´ÞÇÏÁö ¸øÇÑ Á¸ÀçµéÀº µµÅµȴÙ. |
Through almost endless cycles of gains and losses, adjustments and readjustments, all living organisms swing back and forth from age to age. Those that attain cosmic unity persist, while those that fall short of this goal cease to exist. |
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58:7.1 |
»ý¸í ŵ¿±â¿Í ¿ø»ý´ë ±â°£ µ¿¾È Áö±¸ÀÇ Áö°¢À» ±¸¼ºÇÏ¿´´ø ¹ÙÀ§ µ¢¾î¸®µéÀÇ ±¤´ëÇÑ ¹«¸®´Â Áö±ÝÀº Áö±¸ Ç¥¸é¿¡¼ °ÅÀÇ ¹ß°ßµÇÁö ¾Ê´Â´Ù. ±×¸®°í ±×°ÍÀÌ ÈÄ´ë¿¡ ½×ÀÎ ¸ðµç ÅðÀû¹°ÀÇ ¾Æ·¡·ÎºÎÅÍ ¼Ú¾Æ¿À¸¦ ¶§, ±×°÷¿¡¼´Â ¿ÀÁ÷ ½Ä¹°°ú ÃʱâÀÇ ¿ø½Ã µ¿¹° »ý¸íÀÇ È¼®À¯¹°µé¸¸ÀÌ ¹ß°ßµÉ °ÍÀÌ´Ù. ´õ ¿À·¡µÈ ¹°¿¡ ÀÇÇØ¼ ÅðÀûµÈ ÀÌ ¹ÙÀ§µé Áß¿¡¼ ¾î¶² °ÍµéÀº ±× ÈÄ¿¡ ÀÌ·ç¾îÁø ÁöÃþµé°ú µÚ¼¯¿´°í, ¾î¶² °æ¿ì¿¡´Â ±×°ÍµéÀÌ Ãʱâ ÇüÅÂÀÇ ½Ä¹° »ý¸íµé Áß ÀϺκÐÀÇ È¼® À¯¹°µéÀ» Æ÷ÇÔÇϰí ÀÖÀ¸¸ç, ¹Ý¸é¿¡ °¡Àå ³ôÀº Ãþ¿¡¼´Â Ãʱâ ÇØ¾ç µ¿¹° À¯±âüÀÇ º¸´Ù ¿ø½Ã Çüŵé ÀϺΰ¡ °£È¤ ¹ß°ßµÉ ¼öµµ ÀÖ´Ù. ÃʱâÀÇ µ¿¹°°ú ½Ä¹°ÀÇ ÇØ¾ç »ý¹°Ã¼·Î ÀÌ·ç¾îÁø ȼ®ÀÌ µé¾îÀÖ´Â °¡Àå ¿À·¡µÈ ÀÌ ¼ºÃþ¾Ï ÁöÃþµéÀº ¸¹Àº °÷¿¡¼ ºÐȵÇÁö ¾ÊÀº °í´ëÀÇ ¹ÙÀ§ À§¿¡¼ Á÷Á¢ ¹ß°ßµÉ ¼ö ÀÖ´Ù. |
The vast group of rock systems which constituted the outer crust of the world during the life-dawn or Proterozoic era does not now appear at many points on the earth's surface. And when it does emerge from below all the accumulations of subsequent ages, there will be found only the fossil remains of vegetable and early primitive animal life. Some of these older water-deposited rocks are commingled with subsequent layers, and sometimes they yield fossil remains of some of the earlier forms of vegetable life, while on the topmost layers occasionally may be found some of the more primitive forms of the early marine-animal organisms. In many places these oldest stratified rock layers, bearing the fossils of the early marine life, both animal and vegetable, may be found directly on top of the older undifferentiated stone. |
58:7.2 |
ÀÌ ½Ã±âÀÇ È¼®µé ¼Ó¿¡´Â ÇØÃÊ, »êÈ£ ¸ð¾çÀÇ ½Ä¹°µé, ¿ø½Ã ¿ø»ýµ¿¹° Á¾·ùµé, ±×¸®°í ½ºÆÝÁöó·³ »ý±ä º¯Ãµ±âÀÇ À¯±âüµéÀÌ Æ÷ÇԵǾî ÀÖ´Ù. ±×·¯³ª ÃʱâÀÇ ¹ÙÀ§ Ãþ ¼Ó¿¡ ±×·¯ÇÑ È¼®µéÀÌ µé¾îÀÖÁö ¾Ê´Ù´Â »ç½ÇÀÌ, »ì¾ÆÀÖ´Â »ý¸íüµéÀÌ ±×°ÍµéÀÇ ÅðÀû±â¿¡ ¾î´À °÷¿¡µµ Á¸ÀçÇÏÁö ¾Ê¾ÒÀ½À» ¹Ýµå½Ã Áõ¸íÇÏ´Â °ÍÀº ¾Æ´Ï´Ù. »ý¸íÀº ÀÌ·¯ÇÑ Ãʱ⠽ô뿡 µÎ·ç ¸Å¿ì Èñ¼ÒÇÏ¿´°í, Áö±¸ Ç¥¸éÀ¸·Î ´ÜÁö ¼¼È÷ ³ª¾Æ°¬À» »ÓÀÌ´Ù. |
Fossils of this era yield algae, corallike plants, primitive Protozoa, and spongelike transition organisms. But the absence of such fossils in the early rock layers does not necessarily prove that living things were not elsewhere in existence at the time of their deposition. Life was sparse throughout these early times and only slowly made its way over the face of the earth. |
58:7.3 |
ÀÌ °í´ëÀÇ ¹ÙÀ§µéÀÌ ÇöÀç Áö±¸ Ç¥¸é¿¡ Àְųª Ç¥¸é¿¡¼ ¾ÆÁÖ °¡±î¿î °÷¿¡ À§Ä¡Çϰí ÀÖÀ¸¸ç ÇöÀç ´ë·ú ÀüüÀÇ ¾à 8ºÐÀÇ 1¿¡ °ÉÃÄÀÖ´Ù. °¡Àå ¿À·¡µÈ ¼ºÃþ¾Ï ÁöÃþÀÎ, º¯Ãµ±â¿¡ ÀÌ·ç¾îÁø ÀÌ µ¹ÀÇ Æò±Õ µÎ²²´Â ¾à 1.5¸¶ÀÏ¿¡ À̸¥´Ù. ¾î¶² ÁöÁ¡¿¡¼´Â °í´ëÀÇ ÀÌ ¹ÙÀ§ µ¢¾î¸®µéÀÌ 4¸¶ÀÏ¿¡ À̸£´Â µÎ²²¸¦ °®±âµµ ÇÏÁö¸¸, ÀÌ ½Ã±â¿¡ ÇØ´çµÇ´Â °ÍÀ¸·Î »ý°¢µÇ´Â ´ëºÎºÐÀÇ ÁöÃþµéÀº ÈÄ´ë¿¡ ÀÌ·ç¾îÁø °ÍÀÌ´Ù. |
The rocks of this olden age are now at the earth's surface, or very near the surface, over about one eighth of the present land area. The average thickness of this transition stone, the oldest stratified rock layers, is about one and one-half miles. At some points these ancient rock systems are as much as four miles thick, but many of the layers which have been ascribed to this era belong to later periods. |
58:7.4 |
ºÏ ¾Æ¸Þ¸®Ä«¿¡¼´Â ¿ø½Ã ȼ®ÀÌ µé¾î ÀÖ´Â °í´ëÀÇ ÀÌ ¹ÙÀ§ ÁöÃþÀÌ µ¿ºÎ¿Í Áß¾Ó Áö¿ª ±×¸®°í ij³ª´ÙÀÇ ºÏºÎ Áö¿ªÀÇ ÁöÇ¥¸é¿¡ µ¹Ã⠵Ǿî ÀÖ´Ù. ¶ÇÇÑ ±×°÷¿¡´Â Ææ½Çº£ÀÌ´Ï¾Æ¿Í °í´ëÀÇ ¾Öµð·Ð´ì »êµé·ÎºÎÅÍ ½ÃÀÛÇÏ¿© ¹Ì½Ã°£°ú À§½ºÄܽб׏®°í ¹Ì³×¼ÒŸ¸¦ °ÅÃÄ ¼ÂÊÀ¸·Î »¸¾î ³ª°£ ÀÌ ¹ÙÀ§ ÃþÀ¸·Î ÀÌ·ç¾îÁø µ¿-¼ ¹æÇâÀÇ °£ÇæÀûÀÎ »ê¸ÆÀÌ ÀÖ´Ù. ´ºÈ͵巣µå·ÎºÎÅÍ ¾Ù¶ó¹è¸¶·Î, ±×¸®°í ¾Ë·¡½ºÄ«·ÎºÎÅÍ ¸ß½ÃÄÚ·Î À̾îÁö´Â ´Ù¸¥ »ê¸Æµéµµ ÀÖ´Ù. |
In North America this ancient and primitive fossil-bearing stone layer comes to the surface over the eastern, central, and northern regions of Canada. There is also an intermittent east-west ridge of this rock which extends from Pennsylvania and the ancient Adirondack Mountains on west through Michigan, Wisconsin, and Minnesota. Other ridges run from Newfoundland to Alabama and from Alaska to Mexico. |
58:7.5 |
ÀÌ ½Ã´ëÀÇ ¹ÙÀ§µéÀÌ ¼¼°è °÷°÷¿¡ ³ëÃâµÇ¾î ÀÖÁö¸¸, ÄÝ·Î¶óµµ °ÀÌ È帣´Â ±×·£µå ij³Í°ú ½´ÇǸ®¾î È£¼ö ±ÙóÀÇ Áö¿ª¿¡ ÀÖ´Â ¹ÙÀ§µéó·³ ½±°Ô È®ÀεǴ °÷ÀÌ ¾øÀ¸¸ç, ±×°÷¿¡¼ ÀÌ ¿ø½Ã ȼ®ÀÌ µé¾î ÀÖ°í ¿©·¯ ÃþÀ¸·Î µÇ¾î ÀÖ´Â ÀÌ ¹ÙÀ§µéÀº, ¸Õ ¿¾³¯¿¡ ÀϾ´ø À¶±â¿Í ÁöÇ¥¸é º¯µ¿À» Áõ¸íÇÑ´Ù. |
The rocks of this era are exposed here and there all over the world, but none are so easy of interpretation as those about Lake Superior and in the Grand Canyon of the Colorado River, where these primitive fossil-bearing rocks, existing in several layers, testify to the upheavals and surface fluctuations of those faraway times. |
58:7.6 |
²®ÁúÀÇ °¡Àå ¿À·¡µÈ ȼ®ÀÌ µé¾î ÀÖ´Â ÁöÃþÀÎ ÀÌ ¾Ï¼®ÃþÀº ÁÖ¸§ÀÌ Áö°í °ãÃÄÁ³À¸¸ç ÁöÁøÀ¸·Î ÀÎÇÑ À¶±â¿Í ÃʱâÀÇ È»ê Ȱµ¿ÀÇ °á°ú·Î ±â±«ÇÑ ¸ð½ÀÀ¸·Î µÚƲ¾îÁ³´Ù. ÀÌ ½Ã±âÀÇ ¿ë¾Ï ºÐÃâÀº ¸¹Àº ö°ú µ¿ ±×¸®°í ³³À» Áö±¸ Ç¥¸é °¡±îÀÌ °¡Á®¿Ô´Ù. |
This stone layer, the oldest fossil-bearing stratum in the crust of the earth, has been crumpled, folded, and grotesquely twisted as a result of the upheavals of earthquakes and the early volcanoes. The lava flows of this age brought much iron, copper, and lead up near the planetary surface. |
58:7.7 |
À§½ºÄܽſ¡ ÀÖ´Â ¼¼ÀÎÆ® Å©·ÎÀͽº °è°îº¸´Ù ´õ »ý»ýÇÏ°Ô ±×·¯ÇÑ È°µ¿µéÀÌ º¸ÀÌ´Â Àå¼Ò´Â ÀÌ Áö±¸ À§¿¡ °ÅÀÇ ¾ø´Ù. ÀÌ Áö¿ª¿¡¼´Â 127ȸ¿¡ ´ÞÇÏ´Â ¿¬¼ÓÀûÀÎ ¶¥ À§·ÎÀÇ ¿ë¾Ï ºÐÃâ°ú À̾îÁö´Â ħ¼ö Çö»ó ±×¸®°í ±× °á°ú·Î ÀÏ¾î³ ¹ÙÀ§ÀÇ ÅðÀûÀÌ ÀϾ¾ú´Ù. ´ëºÎºÐÀÇ »óÃþºÎ ¾Ï¹ÝÀÇ Ä§Àü°ú °£ÇæÀûÀÎ ¿ë¾Ï ºÐÃâÀÌ ¿À´Ã³¯¿¡´Â ÀϾÁö ¾Ê°í ÀÖ´Ù ÇÏ´õ¶óµµ, ±×¸®°í ÀÌ ±¸Á¶µéÀÇ ¹Ø¹Ù´ÚÀÌ Áö±¸ ¼Ó ±íÀº °÷¿¡ ¹¯ÇôÀÖ´Ù ÇÒÁö¶óµµ, ¾à 65-70°³ÀÇ Áö³ª°£ ½Ã´ëµéÀÇ ÃþÈ(öµûù)µÈ ±â·ÏµéÀÌ ÇöÀç ¹ÛÀ¸·Î µå·¯³ª ÀÖ´Ù. |
There are few places on the earth where such activities are more graphically shown than in the St. Croix valley of Wisconsin. In this region there occurred one hundred and twenty-seven successive lava flows on land with succeeding water submergence and consequent rock deposition. Although much of the upper rock sedimentation and intermittent lava flow is absent today, and though the bottom of this system is buried deep in the earth, nevertheless, about sixty-five or seventy of these stratified records of past ages are now exposed to view. |
58:7.8 |
´ëºÎºÐÀÇ ¶¥ÀÌ ÇØ¼ö¸é°ú °ÅÀÇ µ¿ÀÏÇÏ¿´´ø ÀÌ·¯ÇÑ Ãʱ⠽ô뿡, ¿©·¯ Â÷·ÊÀÇ ¿¬¼ÓÀûÀΠħ°°ú À¶±â°¡ ¹ß»ýµÇ¾ú´Ù. Áö±¸ÀÇ Áö°¢Àº ºñ±³Àû ¾ÈÁ¤µÈ Èı⠽ô뿡 ¸· Á¢¾îµé°í ÀÖ¾ú´Ù. Ãʱ⠴ë·úÀÇ Ç¥·ùÀÇ ±ÁÀÌÄ¡´Â Çö»óµé, »ó½Â°ú Çϰ ÀÛ¿ëµé·Î ÀÎÇÏ¿© °Å´ëÇÑ ¶¥ µ¢¾î¸®µéÀÌ ÁÖ±âÀûÀ¸·Î ¹°¿¡ Àá°å´Ù. |
In these early ages when much land was near sea level, there occurred many successive submergences and emergences. The earth's crust was just entering upon its later period of comparative stabilization. The undulations, rises and dips, of the earlier continental drift contributed to the frequency of the periodic submergence of the great land masses. |
58:7.9 |
¿ø½Ã ÇØ¾ç »ý¸íÀÇ ÀÌ ±â°£ µ¿¾È, ±¤´ëÇÑ Áö¿ªÀÇ ´ë·ú ÇØ¾È¼±ÀÌ ÀÛ°Ô´Â ¸î ÇÇÆ®¿¡¼ Å©°Ô´Â ¹Ý¸¶ÀÏ¿¡ À̸£±â±îÁö ¹Ù´Ù ¹ØÀ¸·Î °¡¶ó¾É¾Ò´Ù. ´õ ¿À·¡µÈ »ç¾Ï°ú ¿ª¾ÏÀÇ ´ëºÎºÐÀº ÀÌ·¯ÇÑ °í´ëÀÇ ÇØ¾È¼±ÀÌ Ä§Àü ÅðÀûÀ» º¸¿©ÁØ´Ù. ÀÌ·¯ÇÑ Ãʱ⠼ºÃþ(à÷öµ)¿¡ µé¾î ÀÖ´Â ÅðÀû¾ÏµéÀº »ý¸íÀÇ ±â¿ø ÈξÀ Àü, Áö±¸ Àü¿ª¿¡ ÆÛÁø ÇØ¾çÀÇ ½Ã±â¿¡ Çü¼ºµÈ ÁöÃþµé ¹Ù·Î À§¿¡ ³õ¿© ÀÖ´Ù. |
During these times of primitive marine life, extensive areas of the continental shores sank beneath the seas from a few feet to half a mile. Much of the older sandstone and conglomerates represents the sedimentary accumulations of these ancient shores. The sedimentary rocks belonging to this early stratification rest directly upon those layers which date back far beyond the origin of life, back to the early appearance of the world-wide ocean. |
58:7.10 |
ÀÌµé º¯Ãµ±â ¾Ï¹Ý ÅðÀûÀÇ »óÃþÀÇ ÀϺο¡´Â ¼Ò·®ÀÇ ÀÌÆÇ¾ÏÀ̳ª ¾îµÎ¿î »ö±òÀÇ Á¡ÆÇ¾ÏÀÌ µé¾î ÀÖÀ¸¸ç, À̰ÍÀº À¯±âÁú ź¼ÒÀÇ ½ÇÀ縦 ÀǹÌÇϸç, °è¼ÓµÈ ¼®Åº±â µ¿¾È¿¡ Áö±¸ À§¿¡ ³Î¸® ÆÛÁø ½Ä¹° »ý¸í ÇüŵéÀÇ Á¶»óÀÌ Á¸ÀçÇÏ¿´À½À» Áõ¸íÇÑ´Ù. ÀÌ·¯ÇÑ ¾Ï¼®Ãþ ¼Ó¿¡ ÀÖ´Â ±¸¸® ¼ººÐÀÇ ´ëºÎºÐÀº ¹°ÀÇ Ä§ÀüÀ¸·Î ¸¸µé¾îÁø °ÍÀÌ´Ù. ¾î¶² °ÍÀº ´õ ¿À·¡µÈ ¹ÙÀ§µé Æ´ ¼Ó¿¡¼ ¹ß°ßµÇ¸ç, °í´ëÀÇ º¸È£µÈ ÇØ¾È¼±¿¡ ÀÖ´ø ¿Ï¸¸ÇÑ ´ËÁö´ëÀÇ ¹°·ÎºÎÅÍ ÀÀÃàµÈ °ÍÀÌ´Ù. ºÏ ¾Æ¸Þ¸®Ä«¿Í À¯·´ÀÇ Ã¶±¤µéÀº, ÃþÀ» ÀÌ·çÁö ¾ÊÀº ´õ ¿À·¡µÈ ¾Ï¼®µé ¼Ó¿¡ ±×¸®°í »ý¸í Çü¼ºÀÇ º¯È¯±â¿¡ ÃþÀ» ÀÌ·é ÈÄ´ëÀÇ ¹ÙÀ§ ¼Ó¿¡ ºÎºÐÀûÀ¸·Î Æ÷ÇԵǾî ÀÖ´Â, ÅðÀûÃþ°ú ºÐÃâµÈ ÁöÃþ ¼Ó¿¡ À§Ä¡ÇÑ´Ù. |
Some of the upper layers of these transition rock deposits contain small amounts of shale or slate of dark colors, indicating the presence of organic carbon and testifying to the existence of the ancestors of those forms of plant life which overran the earth during the succeeding Carboniferous or coal age. Much of the copper in these rock layers results from water deposition. Some is found in the cracks of the older rocks and is the concentrate of the sluggish swamp water of some ancient sheltered shore line. The iron mines of North America and Europe are located in deposits and extrusions lying partly in the older unstratified rocks and partly in these later stratified rocks of the transition periods of life formation. |
58:7.11 |
ÀÌ ±â°£¿¡, Áö±¸ ÀüüÀÇ ¹°¼Ó¿¡´Â »ý¸íÀÌ ÆÛÁ® ÀÖ¾úÀ¸¸ç; ÇØ¾ç »ý¸íÀÌ À¯¶õ½Ã¾Æ¿¡ ¼º°øÀûÀ¸·Î Á¶¼ºµÇ¾ú´Ù. ±íÀ̰¡ ¾èÀº ±¤´ëÇÑ ³»·úÀÇ ¹Ù´Ùµé ¹Ø¹Ù´ÚÀº dzºÎÇÏ°í ¿ïâÇÏ°Ô Àڶ󳪴 ½Ä¹°µé·Î Á¡Â÷ °¡µæ Â÷°Ô µÇ¾úÀ¸¸ç, ¹Ý¸é¿¡ ÇØ¾È¼±ÀÇ ¹°¿¡´Â ´Ü¼øÇÑ ÇüÅÂÀÇ µ¿¹° »ý¸íµéÀÌ ¹«¸®¸¦ Áþ°í ÀÖ¾ú´Ù. |
This era witnesses the spread of life throughout the waters of the world; marine life has become well established on Urantia. The bottoms of the shallow and extensive inland seas are being gradually overrun by a profuse and luxuriant growth of vegetation, while the shore-line waters are swarming with the simple forms of animal life. |
58:7.12 |
¸ðµç ÀÌ À̾߱â´Â Áö±¸ Àüü¿¡ ±â·ÏµÈ ±¤´ëÇÑ ¡°¾Ï¼® ¿ª»çÃ¥¡±ÀÇ È¼®¿¡¼ »ý»ýÇÏ°Ô º¸À̰í ÀÖ´Ù. ±×¸®°í ³ÊÈñ°¡ ±×°ÍµéÀ» ÇØµ¶ÇÒ ¼ö ÀÖ´Â ±â¼úÀ» ½ÀµæÇϱ⸸ ÇÑ´Ù¸é, °Å´ëÇÑ ÀÌ »ý¹°ÁöÁúÇÐÀû ±â·Ïµé ¼Ó¿¡¼ ¹Ýµå½Ã Áø½ÇÀ» ¹ß°ßÇÏ°Ô µÉ °ÍÀÌ´Ù. ÀÌ·¯ÇÑ °í´ëÀÇ ÇØÀú ÁöÃþµé ´ëºÎºÐÀº ÇöÀç À°Áö À§·Î ³ôÀÌ ¼Ú¾Æ¿Ã¶ó ÀÖÀ¸¸ç, ¿©·¯ ½Ã´ë¿¡ °ÉÃÄ ÅðÀûµÈ ÁöÃþµéÀº ±× Ãʱ⿡ »ý¸íµéÀÌ ¾î¶»°Ô ÅõÀïÇÏ¸ç »ì¾Æ³²¾Ò´ÂÁö¸¦ º¸¿©ÁØ´Ù. ³ÊÈñµé Áß¿¡ ¾î¶² ½ÃÀÎÀÌ ¡°¿ì¸®°¡ ¹â°í ÀÖ´Â ÀÌ Èëµµ ÇÑ ¶§´Â »ì¾Æ ÀÖ¾ú´Ù.¡±¶ó°í Ç¥ÇöÇÑ °ÍÀº Á¤¸»·Î ¸Â´Â ¸»ÀÌ´Ù. |
All of this story is graphically told within the fossil pages of the vast "stone book" of world record. And the pages of this gigantic biogeologic record unfailingly tell the truth if you but acquire skill in their interpretation. Many of these ancient sea beds are now elevated high upon land, and their deposits of age upon age tell the story of the life struggles of those early days. It is literally true, as your poet has said, "The dust we tread upon was once alive." |
58:7.13 |
[ÇöÀç Áö±¸¿¡ °ÅÇϰí ÀÖ´Â À¯¶õ½Ã¾Æ »ý¸í¿î¹ÝÀÚ ¹«¸®´ÜÀÇ ÀÏ¿ø¿¡ ÀÇÇØ Á¦½ÃµÇ¾úÀ½] |
Presented by a member of the Urantia Life Carrier Corps now resident on the planet. |