Back Blue Mars
Chapters (93)
  1. Title Page
  2. Dedication
  3. Contents
  4. Map
  5. The Martain Calendar
  6. Part 1: Peacock Mountain
  7. Prologue
  8. 1
  9. 2
  10. Part 2: Areophany
  11. Prologue
  12. 1
  13. 2
  14. 3
  15. 4
  16. Part 3: A New Constitution
  17. Prologue
  18. 1
  19. 2
  20. 3
  21. 4
  22. 5
  23. 6
  24. 7
  25. Part 4: Green Earth
  26. Prologue
  27. 1
  28. 2
  29. 3
  30. Part 5: Home at Last
  31. Prologue
  32. 1
  33. 2
  34. 3
  35. Part 6: Ann in the Outback
  36. Prologue
  37. 1
  38. 2
  39. 3
  40. Part 7: Making Things Work
  41. Prologue
  42. 1
  43. 2
  44. 3
  45. 4
  46. 5
  47. 6
  48. Part 8: The Green and the White
  49. Prologue
  50. 1
  51. 2
  52. 3
  53. 4
  54. Part 9: Natural History
  55. Prologue
  56. 1
  57. 2
  58. Part 10: Werteswandel
  59. Prologue
  60. 1
  61. 2
  62. 3
  63. Part 11: Viriditas
  64. Prologue
  65. 1
  66. 2
  67. 3
  68. 4
  69. 5
  70. 6
  71. Part 12: It Goes So Fast
  72. Prologue
  73. 1
  74. 2
  75. 3
  76. 4
  77. 5
  78. Part 13: Experimental Procedures
  79. Prologue
  80. 1
  81. 2
  82. 3
  83. 4
  84. 5
  85. 6
  86. 7
  87. Part 14: Phoenix Lake
  88. Prologue
  89. 1
  90. Acknowledgments
  91. About the Author
  92. Bantam Books by Kim Stanley Robinson
  93. Copyright

There were, however, a few exceptions to this situation. The Noachian Age had been followed by a brief “warm wet period” in the late Hesperian, a period perhaps as short as a hundred million years, when a thick warm CO2 atmosphere had allowed liquid water to run on the surface, carving some river channels down the gentle tilts of the plateau, between crater aprons diverting them this way and that. And these watercourses had of course remained after the atmosphere had frozen out, empty arroyos gradually widened by the wind. These fossil riverbeds, like Nirgal Vallis, Warrego Valles, Protva Valles, Patana Valles, or Oltis Vallis, were narrow sinuous canyons, true riverine canyons rather than grabens or fossae. Some of them even had immature tributary systems. So efforts to design a macro-watershed system for the south naturally used these canyons as primary watercourses, with water pumped to the head of every tributary. Then there were also a number of old lava channels that could easily become rivers, as the lava, like the water, had tended to follow the path of least resistance downhill. And there were a number of tilted graben fractures and fissures, as at the foot of the Eridania Scopulus, that could likewise be turned to use.

In the conference, big globes of Mars were marked up daily to display different water regimes. There were also rooms full of 3-D topo maps, with groups standing around different watershed systems, arguing their advantages and disadvantages, or simply contemplating them, or fiddling with the controls to change them, restlessly, from one pattern to another. Nadia wandered the rooms looking at these hydrographies, learning much about the southern hemisphere that she had never known. There was a six-kilometer-high mountain near Richardson Crater, in the far south. The south polar cap itself was quite high. Dorsa Brevia, on the other hand, crossed a depression that looked like a ray cut out from the Hellas impact, a valley so deep that it ought to become a lake, an idea that the Dorsa Brevians naturally did not like. And certainly the area could be drained if they cared to do it. There were scores of variant plans, and every single system was strange looking to Nadia. Never had she seen so clearly how different a gravity-driven fractal was from impact randomness. In the inchoate meteoric landscape, almost anything was possible, because nothing was obvious— nothing except for the fact that in any possible system, some canals and tunnels would have to be built. Her new finger itched with the desire to get out there and run a bulldozer or a tunnel borer.