Back Green Mars
Chapters (68)
  1. Title Page
  2. Dedication
  3. Contents
  4. Map
  5. Part 1: Areoformation
  6. Prologue
  7. 1
  8. 2
  9. 3
  10. 4
  11. 5
  12. Part 2: The Ambassador
  13. Prologue
  14. 1
  15. 2
  16. Part 3: Long Runout
  17. Prologue
  18. 2
  19. 3
  20. Part 4: The Scientist as Hero
  21. Prologue
  22. 1
  23. 2
  24. 3
  25. 4
  26. 5
  27. 6
  28. 7
  29. Part 5: Homeless
  30. Prologue
  31. 1
  32. 2
  33. Part 6: Tariqat
  34. Prologue
  35. 1
  36. 2
  37. 3
  38. 4
  39. 5
  40. 6
  41. Part 7: What Is to Be Done?
  42. Prologue
  43. 1
  44. 2
  45. 3
  46. Part 8: Social Engineering
  47. Prologue
  48. 1
  49. Part 9: The Spur of the Moment
  50. Prologue
  51. 1
  52. 2
  53. 3
  54. 4
  55. 5
  56. 6
  57. 7
  58. 8
  59. Part 10: Phase Change
  60. Prologue
  61. 1
  62. 2
  63. 3
  64. 4
  65. Epilogue
  66. Temperature Comparisons
  67. Bantam Books by Kim Stanley Robinson
  68. Copyright

After that, the circumHellas train trips and the various overflights felt different to Maya, as she perceived the interlaced network of glaciers and ice chaoses in the basin to be the new sea itself, rising and filling and sloshing around. And in fact the liquid sea under the surface ice near Low Point was growing much faster in the springs and summers than it was shrinking in the autumns and winters. And strong winds kicked up waves in the polynyas, which in the summers broke the ice between them, creating regions of brash ice, a floating pack of ice chunks which growled so loudly as they rode the steep little swells that conversation in dirigibles overhead was difficult.

And in the year M-49, the flow rates from all the tapped aquifers reached their maximums, combining to pump 2,500 cubic meters a day into the sea, an amount that would fill the basin to the –1-kilometer contour in about six M-years. To Maya this did not seem long at all, especially as they could see the progress, right there on Odessa’s horizon. In winters the black storms that poured over the mountains would blanket the whole basin floor with startling white snow; in the springs the snow would melt, but the new edge of the ice sea would be closer than it had been the previous autumn.

It was much the same in the northern hemisphere, as news reports and her infrequent trips to Burroughs made clear. The great northern dunes of Vastitas Borealis were being rapidly inundated, as the truly enormous aquifers under Vastitas and the north polar region were being pumped onto the surface by drilling platforms that rose on the ice as the ice accumulated under them. In the northern summers, great rivers were pouring off the melting northern polar cap, cutting channels through the laminate sands and running down to join the ice. And a few months after Minus One had been islanded, news reports showed video of an uncovered stretch of ground in Vastitas, disappearing under a dark flood from west and east and north. This apparently created the last link between the lobes of ice; so now there was a world-wrapping sea in the north. Of course it was patchy still, and covered only about half of the land between the sixtieth and seventieth latitudes, but as satellite photos showed, there were already great bays of ice extending south into the deep depressions of Chryse and Isidis.