OCR A-Level Geography H481
Coastal Landscapes
Glaciated Landscapes
Dryland Landscapes
Earth’s Life Support Systems
Changing Spaces; Making Places
Trade in the Contemporary World
Global Migration
Human Rights
Power and Borders
Climate Change
Disease Dilemmas
Exploring Oceans
Future of Food
Hazardous Earth
Geographical Skills
Exploring Oceans
Mining the deep sea bed for metals
- 2 things to know
- Component 03
Overview
Recall questions on ferrous and non-ferrous minerals, polymetallic nodules in the Clarion-Clipperton Zone, seafloor massive sulfides and cobalt-rich crusts, rising demand for battery metals and cobalt from the Democratic Republic of the Congo, the International Seabed Authority and the common heritage of mankind, ecological impacts, slow recovery, and calls for a pause.
What you need to know
Answer each one before you reveal it.
Distinguish between ferrous and non-ferrous minerals.
Questions from this subtopic
Each one with the model answer underneath.
- 1
Distinguish between ferrous and non-ferrous minerals.
Model answer
Ferrous minerals contain iron, such as the iron ore used in steelmaking, while non-ferrous minerals such as copper, nickel, cobalt, zinc and gold contain no iron.
- 2
What are polymetallic nodules?
Model answer
They are potato-sized lumps of metal oxide that lie loose on the surface of abyssal plains, rich in manganese, nickel, copper and cobalt.
- 3
At roughly what depth do polymetallic nodules occur?
Model answer
They occur on the deep ocean floor at around 4,000 to 6,000 m.
- 4
Which region of the Pacific holds the largest known field of polymetallic nodules?
Model answer
The Clarion-Clipperton Zone, a vast area of abyssal plain between Hawaii and Mexico, holds the richest known deposits.
- 5
Why can polymetallic nodules be regarded as effectively non-renewable?
Model answer
They grow by only a few millimetres every million years, so any that are removed will not be replaced on any human timescale.
- 6
What are seafloor massive sulfides, and where do they form?
Model answer
They are metal-rich deposits of copper, zinc, gold and silver precipitated from hot mineral-laden fluids at hydrothermal vents on ocean ridges.
Other ways to work this
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