Lakes on Mars

In summer 1965, the first close-up images from Mars showed a cratered desert with no signs of water. [1] [2] [3] However, over the decades, as more parts of the planet were imaged with better cameras on more sophisticated satellites, Mars showed evidence of past river valleys, lakes, and present ice in glaciers and in the ground. [4] It was discovered that the climate of Mars displays huge changes over geologic time because its axis is not stabilized by a large moon, as Earth's is. [5] [6] [7] Also, some researchers maintain that surface liquid water could have existed for periods of time due to geothermal effects or asteroid impacts. [8] [9] [10] [11] [12] This article describes some of the places that could have held large lakes.

Page Revisions

Year Metadata Sections Top Words First Paragraph
2018

354629 characters

21 sections

73 paragraphs

51 images

326 internal links

211 external links

1. Overview

2. Images of possible deltas

3. Mars ocean

4. Valles Marineris canyon system

5. Hellas Basin

6. Gale Crater

7. Holden Crater

8. Western Elysium Planitia Paleolake

9. Argyre basin

10. Lakes in Valles Marineris

11. Ritchey Crater

12. Jezero Crater

13. Eridania Lake

14. Columbus crater

15. Navua Valles

16. Southern polar cap subglacial lake

17. See also

18. References

19. External links

lake 0.399

water 0.217

basin 0.207

chasma 0.183

holden 0.174

lakes 0.167

deposits 0.148

terby 0.134

hellas 0.133

crater 0.127

clays 0.121

gale 0.120

ocean 0.118

candor 0.116

eridania 0.111

In summer 1965, the first close-up images from Mars showed a cratered desert with no signs of water. [1] [2] [3] However, over the decades, as more parts of the planet were imaged with better cameras on more sophisticated satellites, Mars showed evidence of past river valleys, lakes, and present ice in glaciers and in the ground. [4] It was discovered that the climate of Mars displays huge changes over geologic time because its axis is not stabilized by a large moon, as Earth's is. [5] [6] [7] Also, some researchers maintain that surface liquid water could have existed for periods of time due to geothermal effects or asteroid impacts. [8] [9] [10] [11] [12] This article describes some of the places that could have held large lakes.

2017

338292 characters

19 sections

72 paragraphs

52 images

326 internal links

186 external links

1. Images of possible deltas

2. Mars Ocean

3. History of observational evidence for Martian oceans

4. Valles Marineris canyon system

5. Hellas Basin

6. Gale Crater

7. Holden Crater

8. Western Elysium Planitia Paleolake

9. Argyre basin

10. Lakes in Valles Marineris

11. Ritchey Crater

12. Jezero (crater)

13. Eridania Lake

14. Columbus crater

15. Navua Valles

16. See also

17. References

18. External links

lake 0.390

water 0.218

basin 0.192

chasma 0.187

holden 0.178

deposits 0.152

lakes 0.149

gale 0.140

terby 0.137

clays 0.133

crater 0.132

candor 0.118

hellas 0.112

ocean 0.109

eridania 0.103

In summer 1965, the first close-up pictures from Mars showed a cratered desert with no signs of water. [1] [2] [3] However, over the decades, as more parts of the planet were imaged with better cameras on more sophisticated satellites, Mars showed evidence of past river valleys, lakes, and ice in glaciers and in the ground. [4] It was discovered that the climate of Mars displays huge changes over geologic time because its axis is not stabilized by a large moon, as Earth's is. [5] [6] [7] Also, some researchers maintain that water could exist for periods of time due to geothermal effects or asteroid impacts. [8] [9] [10] [11] [12]

2016

316238 characters

18 sections

63 paragraphs

47 images

310 internal links

166 external links

1. Images of possible deltas

2. Mars Ocean

3. History of observational evidence for Martian oceans

4. Valles Marineris canyon system

5. Hellas Basin

6. Gale Crater

7. Holden Crater

8. Western Elysium Planitia Paleolake

9. Argyre basin

10. Lakes in Valles Marineris

11. Ritchey Crater

12. Jezero (crater)

13. Eridania Lake

14. Columbus crater

15. See also

16. References

17. External links

lake 0.392

water 0.213

chasma 0.201

holden 0.191

basin 0.185

gale 0.151

terby 0.147

clays 0.143

crater 0.138

lakes 0.137

deposits 0.127

candor 0.127

ocean 0.117

hellas 0.112

marineris 0.103

In summer 1965, the first close-up pictures from Mars showed a cratered desert with no signs of water. [1] [2] [3] However, over the decades, as more parts of the planet were imaged with better cameras on more sophisticated satellites, Mars showed evidence of past river valleys, lakes, and ice in glaciers and in the ground. [4] It was discovered that the climate of Mars displays huge changes over geologic time because its axis is not stabilized by a large moon, as Earth's is. [5] [6] [7] Also, some researchers maintain that water could exist for periods of time due to geothermal effects or asteroid impacts. [8] [9] [10] [11] [12]

2015

262012 characters

18 sections

60 paragraphs

47 images

307 internal links

89 external links

1. Images of possible deltas

2. Mars Ocean

3. History of observational evidence for Martian oceans

4. Valles Marineris canyon system

5. Hellas Basin

6. Gale Crater

7. Holden Crater

8. Geologic history of Holden Crater

9. Western Elysium Planitia Paleolake

10. Argyre basin

11. Lakes in Valles Marineris

12. Ritchey Crater

13. Jezero (crater)

14. Eridania Lake

15. Columbus crater

16. See also

17. References

18. External links

lake 0.388

water 0.220

chasma 0.203

holden 0.192

basin 0.187

gale 0.152

terby 0.148

lakes 0.146

clays 0.144

crater 0.139

candor 0.128

deposits 0.123

ocean 0.118

hellas 0.113

marineris 0.104

In the summer of 1965, the first close-up pictures from Mars revealed a cratered desert with no signs of water. [1] [2] [3] However, over the decades, as more parts of the planet were imaged with better cameras on more sophisticated satellites, Mars showed evidence of past river valleys, lakes, and ice in glaciers and in the ground. [4] It was discovered that the climate of Mars displays huge changes over geologic time because its axis is not stabilized by a large moon like our Earth. [5] [6] [7] Also, some researchers maintain that water could exist for periods of time due to geothermal effects or asteroid impacts. [8] [9] [10] [11] [12]