Enipeus Vallis

Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4]

Page Revisions

Year Metadata Sections Top Words First Paragraph
2018

98114 characters

6 sections

14 paragraphs

6 images

675 internal links

13 external links

1. General description

2. Regional geology

3. Photo gallery

4. Notes

5. References

6. See also

enipeus 0.629

valley 0.354

tempe 0.225

vallis 0.219

fluvial 0.174

bedforms 0.126

lat 0.118

channels 0.117

stream 0.110

levee 0.108

segment 0.102

267 0.099

vis 0.096

plateau 0.086

alba 0.084

Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4]

2017

56727 characters

6 sections

14 paragraphs

9 images

187 internal links

13 external links

1. General description

2. Regional geology

3. Photo gallery

4. Notes

5. References

6. See also

enipeus 0.629

valley 0.354

tempe 0.225

vallis 0.219

fluvial 0.174

bedforms 0.126

lat 0.118

channels 0.117

stream 0.110

levee 0.108

segment 0.102

267 0.099

vis 0.096

plateau 0.086

alba 0.084

Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4]

2013

51894 characters

5 sections

14 paragraphs

9 images

184 internal links

12 external links

1. General description

2. Regional geology

3. Photo gallery

4. Notes

5. References

enipeus 0.629

valley 0.354

tempe 0.225

vallis 0.219

fluvial 0.174

bedforms 0.126

lat 0.118

channels 0.117

stream 0.110

levee 0.108

segment 0.102

267 0.099

vis 0.096

plateau 0.086

alba 0.084

Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4]

2012

30591 characters

5 sections

14 paragraphs

5 images

45 internal links

12 external links

1. General description

2. Regional geology

3. Photo gallery

4. Notes

5. References

enipeus 0.629

valley 0.354

tempe 0.225

vallis 0.219

fluvial 0.174

bedforms 0.126

lat 0.118

channels 0.117

stream 0.110

levee 0.108

segment 0.102

267 0.099

vis 0.096

plateau 0.086

alba 0.084

Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4]

2011

29594 characters

5 sections

14 paragraphs

5 images

44 internal links

8 external links

1. General description

2. Regional geology

3. Photo gallery

4. Notes

5. Reference

enipeus 0.629

valley 0.354

tempe 0.225

vallis 0.219

fluvial 0.174

bedforms 0.126

lat 0.118

channels 0.117

stream 0.110

levee 0.108

segment 0.102

267 0.099

vis 0.096

plateau 0.086

alba 0.084

Enipeus Vallis is a valley in the northern hemisphere of the planet Mars . It is centered at lat. 37°N, long. 267°E in the Arcadia quadrangle (MC-3) between the large volcano Alba Mons and the Tempe Terra plateau. The valley follows a gently sinuous , north-south path for a distance of about 357 km (222 mi). [2] It is likely an ancient watercourse that formed during the early Hesperian (or late Noachian ) period, [3] around 3.7 billion years ago. [4]

2010

4296 characters

1 sections

2 paragraphs

2 images

5 internal links

1 external links

1. References

enipeus 0.715

377 0.299

357 0.292

vallis 0.234

arcadia 0.234

93 0.165

bar 0.149

centered 0.144

classical 0.135

river 0.130

valley 0.111

17 0.103

long 0.103

scale 0.100

meters 0.093

Enipeus Vallis is a valley in the Arcadia quadrangle on Mars. Its location is centered at 377° north latitude and 93.17° west longitude. It is 357 km long and was named after a classical river. [1]

2009

4334 characters

1 sections

2 paragraphs

2 images

5 internal links

1 external links

1. References

enipeus 0.724

357 0.296

vallis 0.237

arcadia 0.236

degrees 0.225

93 0.167

37 0.159

bar 0.150

centered 0.146

classical 0.137

river 0.131

valley 0.112

long 0.104

scale 0.101

meters 0.094

Enipeus Vallis is a valley in the Arcadia quadrangle on Mars. Its location is centered at 37 degrees north latitude and 93.1 degrees west longitude. It is 357 km long and was named after a classical river. [1]