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Research draft

seafloor spreading

vr.tr.seafloor-spreading · ACT.PRC

Let an agent explain seafloor spreading, relay evidence, mechanisms, rates and associated features from geoscience sources, describe the cold seep alias as related, and distinguish seafloor spreading from continental drift as the earlier idea, subduction, rifting on continents and hotspot volcanism.

Thing Registry Activities and processes

Research draft, second pass

A second pass drafted this model: the structure a model of this thing needs, and what is known about it in the world. The line under this one says how the second half was obtained - researched against sources, or recalled without web access, in which case nothing here was read anywhere and every claim is a lead to verify. Unreviewed either way.

written by Claude from model knowledge without web access - no source was read, every claim is a lead to verify

Researched by: Claude

Purpose and description

Let an agent explain seafloor spreading, relay evidence, mechanisms, rates and associated features from geoscience sources, describe the cold seep alias as related, and distinguish seafloor spreading from continental drift as the earlier idea, subduction, rifting on continents and hotspot volcanism.

The geological process by which new oceanic crust forms at mid-ocean ridges as tectonic plates move apart and magma rises, proposed by Harry Hess in 1962 and confirmed by symmetric magnetic stripes explained by Vine, Matthews and Morley in 1963, a key foundation of plate tectonics, with spreading rates from a few centimetres per year on the Mid-Atlantic Ridge to over ten centimetres per year on the East Pacific Rise and hydrothermal vents along ridges; the registry alias cold seep names seafloor fluid seepage typically at continental margins, a related but different phenomenon.

What it is for: Not applicable; a geological process.

It can be explain evidence and mechanism; relay rates and features; describe related phenomena; distinguish related processes.

Distinguishing features

Ridge-centred

Magnetic striping

Plate tectonics evidence

Hydrothermal activity

What it looks like

Not directly visible; seen in bathymetric maps of ridges and magnetic anomaly stripes.

Physical character

Hess proposal: 1962 year

Vine-Matthews-Morley hypothesis: 1963 year

Mid-Atlantic Ridge spreading rate: about 2-5 cm per year - approximate

East Pacific Rise spreading rate: up to about 15 cm per year - approximate

How it is recognised

Formation of new ocean crust at ridges

Seafloor spreading, mid-ocean ridge spreading, cold seep

Continental drift was Wegener s earlier idea; subduction destroys crust; continental rifting splits continents; hotspots are mantle plumes

Related models

is a kind of - in registry terms, process

tectonics

occurs at -

mid-ocean ridge

is evidence for -

plate tectonics

is contrasted with - misfiled alias

cold seep

In practice

Families and kinds

slow-spreading ridges

fast-spreading ridges

ultraslow ridges

back-arc spreading

hydrothermal vent systems

Standards and regulation

International Seabed Authority rules for deep-sea mining near ridges

Failure modes and hazards

Confusing spreading with continental drift

Misfiled cold seep alias

Partisan framing of deep-sea mining debates

Also called

cold seep

Where this came from

wikidata · CC0 1.0

Drafted structure

Bundle to layer to finding to question, as the second pass will find it: 4 bundles · 8 layers · 8 findings · 16 questions.

Understand What seafloor spreading is.

Science.

Definition

Definition.

Definition

Definition.

  1. What is seafloor spreading, and how does it differ from continental drift, subduction, rifting and hotspots? definition
  2. Is the question about geology, ocean exploration or deep-sea mining? boundary

Cold seeps

Cold seeps.

Cold seeps

Cold seeps.

  1. What are cold seeps, and how do they differ from hydrothermal vents at ridges? definition
  2. Which entry fits cold seep? action
Evidence Evidence.

Science.

Magnetic stripes

Magnetic stripes.

Magnetic stripes

Magnetic stripes.

  1. How did magnetic anomaly stripes confirm spreading? provenance
  2. Which references are standard? provenance

Crust age

Crust age.

Crust age

Crust age.

  1. Why does ocean crust get older away from ridges, as drilling showed? provenance
  2. Which sources are cited? provenance
Features Ridge features.

Application.

Vents

Hydrothermal vents.

Vents

Vents.

  1. How do hydrothermal vents form and support ecosystems? provenance
  2. Which entry fits hydrothermal vent? action

Rates

Spreading rates.

Rates

Rates.

  1. How do spreading rates affect ridge shape? measurement
  2. Which entry fits East Pacific Rise? action
Context History and resources.

Context.

History

History.

History

History.

  1. How did Hess, Tharp and others build the case for spreading? provenance
  2. Which entry fits Marie Tharp? action

Mining

Deep-sea mining.

Mining

Mining.

  1. What debates exist about mining seafloor massive sulphides, with positions attributed? provenance
  2. Is the presentation neutral and attributed? boundary

What the second pass must settle

  • The registry alias cold seep should be moved to its own entry
  • How should geoscience sources be linked?
  • Should hydrothermal vents be linked separately?