Valley network

Valley networks are branching networks of valleys on Mars that superficially resemble terrestrial river drainage basins . [1] They are found mainly incised into the terrain of the martian southern highlands , and are typically - though not always - of Noachian age (approximately four billion years old). The individual valleys are typically less than 5 kilometers wide, though they may extend for up to hundreds or even thousands of kilometers across the martian surface.

Page Revisions

Year Metadata Sections Top Words First Paragraph
2018

124573 characters

10 sections

20 paragraphs

8 images

745 internal links

4 external links

1. Form

2. Distribution and Age

3. Formation and implications for martian climate history

4. References

5. External links

networks 0.414

valleys 0.260

valley 0.259

noachian 0.212

co2 0.149

greenhouse 0.127

recharge 0.110

hesperian 0.106

precipitation 0.105

aquifers 0.096

ramirez 0.094

groundwater 0.092

channel 0.090

formation 0.087

scales 0.087

Valley networks are branching networks of valleys on Mars that superficially resemble terrestrial river drainage basins . [1] They are found mainly incised into the terrain of the martian southern highlands , and are typically - though not always - of Noachian age (approximately four billion years old). The individual valleys are typically less than 5 kilometers wide, though they may extend for up to hundreds or even thousands of kilometers across the martian surface.

2017

146975 characters

10 sections

20 paragraphs

11 images

846 internal links

4 external links

1. Form

2. Distribution and Age

3. Formation and implications for martian climate history

4. References

5. External links

networks 0.414

valleys 0.260

valley 0.259

noachian 0.212

co2 0.149

greenhouse 0.127

recharge 0.110

hesperian 0.106

precipitation 0.105

aquifers 0.096

ramirez 0.094

groundwater 0.092

channel 0.090

formation 0.087

scales 0.087

Valley networks are branching networks of valleys on Mars that superficially resemble terrestrial river drainage basins . [1] They are found mainly incised into the terrain of the martian southern highlands , and are typically - though not always - of Noachian age (approximately four billion years old). The individual valleys are typically less than 5 kilometers wide, though they may extend for up to hundreds or even thousands of kilometers across the martian surface.

2016

83424 characters

10 sections

19 paragraphs

11 images

291 internal links

4 external links

1. Form

2. Distribution and Age

3. Formation and implications for martian climate history

4. References

5. External links

networks 0.428

valleys 0.269

valley 0.255

noachian 0.219

recharge 0.114

hesperian 0.110

precipitation 0.109

aquifers 0.100

groundwater 0.096

channel 0.093

scales 0.090

paleoclimate 0.088

highlands 0.087

mechanisms 0.084

typically 0.083

Valley networks are branching networks of valleys on Mars that superficially resemble terrestrial river drainage basins . [1] They are found mainly incised into the terrain of the martian southern highlands , and are typically - though not always - of Noachian age (approximately four billion years old). The individual valleys are typically less than 5 kilometers wide, though they may extend for up to hundreds or even thousands of kilometers across the martian surface.

2015

82946 characters

10 sections

19 paragraphs

11 images

291 internal links

4 external links

1. Form

2. Distribution and Age

3. Formation and implications for martian climate history

4. References

5. External links

networks 0.428

valleys 0.269

valley 0.255

noachian 0.219

recharge 0.114

hesperian 0.110

precipitation 0.109

aquifers 0.100

groundwater 0.096

channel 0.093

scales 0.090

paleoclimate 0.088

highlands 0.087

mechanisms 0.084

typically 0.083

Valley networks are branching networks of valleys on Mars that superficially resemble terrestrial river drainage basins . [1] They are found mainly incised into the terrain of the martian southern highlands , and are typically - though not always - of Noachian age (approximately four billion years old). The individual valleys are typically less than 5 kilometers wide, though they may extend for up to hundreds or even thousands of kilometers across the martian surface.

2014

59931 characters

10 sections

19 paragraphs

8 images

185 internal links

4 external links

1. Form

2. Distribution and Age

3. Formation and implications for martian climate history

4. References

5. External links

networks 0.428

valleys 0.269

valley 0.255

noachian 0.219

recharge 0.114

hesperian 0.110

precipitation 0.109

aquifers 0.100

groundwater 0.096

channel 0.093

scales 0.090

paleoclimate 0.088

highlands 0.087

mechanisms 0.084

typically 0.083

Valley networks are branching networks of valleys on Mars that superficially resemble terrestrial river drainage basins . [1] They are found mainly incised into the terrain of the martian southern highlands , and are typically - though not always - of Noachian age (approximately four billion years old). The individual valleys are typically less than 5 kilometers wide, though they may extend for up to hundreds or even thousands of kilometers across the martian surface.

2013

59921 characters

10 sections

19 paragraphs

8 images

185 internal links

4 external links

1. Form

2. Distribution and Age

3. Formation and implications for martian climate history

4. References

5. External links

networks 0.428

valleys 0.269

valley 0.255

noachian 0.219

recharge 0.114

hesperian 0.110

precipitation 0.109

aquifers 0.100

groundwater 0.096

channel 0.093

scales 0.090

paleoclimate 0.088

highlands 0.087

mechanisms 0.084

typically 0.083

Valley networks are branching networks of valleys on Mars that superficially resemble terrestrial river drainage basins . [1] They are found mainly incised into the terrain of the martian southern highlands , and are typically - though not always - of Noachian age (approximately four billion years old). The individual valleys are typically less than 5 kilometers wide, though they may extend for up to hundreds or even thousands of kilometers across the martian surface.

2012

59859 characters

10 sections

19 paragraphs

8 images

184 internal links

4 external links

1. Form

2. Distribution and Age

3. Formation and implications for martian climate history

4. References

5. External links

networks 0.428

valleys 0.269

valley 0.255

noachian 0.219

recharge 0.114

hesperian 0.110

precipitation 0.109

aquifers 0.100

groundwater 0.096

channel 0.093

scales 0.090

paleoclimate 0.088

highlands 0.087

mechanisms 0.084

typically 0.083

Valley networks are branching networks of valleys on Mars that superficially resemble terrestrial river drainage basins . [1] They are found mainly incised into the terrain of the martian southern highlands , and are typically - though not always - of Noachian age (approximately four billion years old). The individual valleys are typically less than 5 kilometers wide, though they may extend for up to hundreds or even thousands of kilometers across the martian surface.

2011

57857 characters

9 sections

19 paragraphs

7 images

183 internal links

0 external links

1. Form

2. Distribution and Age

3. Formation and implications for martian climate history

4. References

networks 0.428

valleys 0.269

valley 0.255

noachian 0.219

recharge 0.114

hesperian 0.110

precipitation 0.109

aquifers 0.100

groundwater 0.096

channel 0.093

scales 0.090

paleoclimate 0.088

highlands 0.087

mechanisms 0.084

typically 0.083

Valley networks are branching networks of valleys on Mars that superficially resemble terrestrial river drainage basins [1] . They are found mainly incised into the terrain of the martian southern highlands , and are typically - though not always - of Noachian age (approximately four billion years old). The individual valleys are typically less than 5 kilometers wide, though they may extend for up to hundreds or even thousands of kilometers across the martian surface.