Learning Geology

A Geology Outreach Website

Pages - Menu

Home
Rocks
Gemstone Guide
Hydrogeology
Live Virtual Field Tours
Contribute to LG
About Us

Monday, November 21, 2016

Divergent Boundary, Fast Spreading Ridge

at November 21, 2016

Email This BlogThis!Share to X Share to Facebook Share to Pinterest

Newer Post Older Post Home

Facebook Page

Blog Archive

► 2022 (2)
- ► May 2022 (1)
- ► January 2022 (1)

► 2021 (5)
- ► November 2021 (1)
- ► June 2021 (1)
- ► May 2021 (1)
- ► April 2021 (1)
- ► January 2021 (1)

► 2020 (5)
- ► November 2020 (1)
- ► July 2020 (1)
- ► June 2020 (1)
- ► May 2020 (1)
- ► February 2020 (1)

► 2019 (3)
- ► April 2019 (2)
- ► January 2019 (1)

► 2017 (41)
- ► December 2017 (3)
- ► November 2017 (2)
- ► October 2017 (1)
- ► September 2017 (1)
- ► August 2017 (2)
- ► July 2017 (1)
- ► June 2017 (2)
- ► April 2017 (4)
- ► March 2017 (2)
- ► February 2017 (5)
- ► January 2017 (18)

▼ 2016 (165)
- ► December 2016 (31)
- ▼ November 2016 (26)
- ► October 2016 (4)
- ► September 2016 (1)
- ► August 2016 (2)
- ► July 2016 (2)
- ► June 2016 (37)
- ► May 2016 (16)
- ► April 2016 (7)
- ► March 2016 (23)
- ► February 2016 (10)
- ► January 2016 (6)

► 2015 (225)
- ► December 2015 (7)
- ► November 2015 (12)
- ► October 2015 (7)
- ► September 2015 (24)
- ► August 2015 (45)
- ► July 2015 (43)
- ► June 2015 (31)
- ► May 2015 (13)
- ► April 2015 (11)
- ► March 2015 (24)
- ► February 2015 (5)
- ► January 2015 (3)

► 2014 (16)
- ► September 2014 (16)

Labels

gem stone geology structure environment petroleum tectonics sedimentary rock environmental stratigraphy volcano igneous rock earthquake erosion hydrogeology sedimentary structure careers in Geology geological structures geophysics metamorphic rock igneous field work fossil sediments discovery mineral basin diagenesis reservoir rocks Mid Oceanic Ridge Ocean floor astronomy climate change Sea floor carbonate cave contribution evaporite facies geologic time geotechnical glacier guest blog metamorphism orogeny Abrasion Types of Margins energy extinction boundary hydrology petrography plate tectonics model sinkhole tsunami unconformity Cajon California James Hutton Live Virtual Field Video anoxic event crystal dating deformation engineering geology geochemical geological time scale geology books natural hazards ore organic matter pakistan plate tectonics rock cycle stress tour Atoll Banded Iron Formation. Grand Canyon Messinian Norway Salinity crisis San Andreas Fault coal gemology geologic education glossary ice join us karst kimberlite mass flow medical geology ophiolites our aim paleocurrent palynology resistivity log shale soil thin section photos

Other Posts

World Map: Political and Physical

World Map Political Map of the world The guide above and below is a political guide of the world fixated on Europe and Africa. It d...
What Are Earth Layers Made Of?

What Are Earth Layers Made Of? A modern view of Earth‘s interior layers. As a result of studies during the past century, geologists...
What if weathering and erosion is no more?

Rocks form in many different environments. Igneous rocks develop where melt rises from depth and cools. Intrusive igneous rocks form whe...
Iron Ore

What is iron ore? The iron ore deposits are found in sedimentary rocks. They are formed by the chemical reaction of iron and oxygen mix...
Ocean basins

Altogether 71% of the area of the globe is occupied by ocean basins that have formed by sea-floor spreading and are floored by basaltic...

Subscribe To

Posts

Posts

Comments

Comments

Website visits

Messenger

Learning Geology. All rights reserved 2021. Picture Window theme. Powered by Blogger.