Discussion Overview
The discussion centers around the claim that Earth was flat between 1800 and 800 million years ago, particularly in relation to geological evidence from the Grenvillean orogeny and other mountain-forming processes. Participants explore the implications of this claim, examining geological records and the presence or absence of certain minerals associated with mountain formation.
Discussion Character
- Debate/contested
- Technical explanation
- Exploratory
Main Points Raised
- Some participants question the claim of a flat Earth during the specified period, citing evidence of mountain formation from orogenies such as Grenvillean, Sveconorwegian, and Kibaran.
- Others seek clarification on what is meant by "flat," suggesting that the term may be an oversimplification or hyperbole.
- A participant references a source indicating fewer mountains during this time, which raises questions about the geological activity and the context of the term "flat."
- Some contributions discuss the "Boring Billion" and its implications for biological versus geological evolution, suggesting that tectonic activity may have been suppressed.
- Participants note the absence of certain geological formations and deposits during this period, which they argue could support the flat Earth claim, while also acknowledging the existence of orogenic rocks.
- There is mention of various orogeny periods and their timelines, with some participants expressing curiosity about the climate and geological conditions during these times.
Areas of Agreement / Disagreement
Participants do not reach a consensus on the claim of a flat Earth during the specified period. Multiple competing views remain regarding the interpretation of geological evidence and the definitions of "flat" and "mountains."
Contextual Notes
Participants highlight limitations in the geological record, including the absence of certain minerals and formations, and the potential for misinterpretation of terms like "flat" and "Boring Billion." The discussion reflects uncertainty about the geological conditions and tectonic activity during the time in question.