levo

Tectonic Hazards

Convergent margins and subduction

  • 3 things to know
  • AS Unit 1 and A2 Unit 4

Overview

Three kinds of convergent plate margin, why magma is generated above a subducting slab and benioff zone.

What you need to know

Answer each one before you reveal it.

Your recallNot started
Key term

What are the three kinds of convergent plate margin?

Key term

Name a mountain range formed at an oceanic to continental margin and the plates responsible.

Key term

To what depth do earthquakes occur within a Benioff zone?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What are the three kinds of convergent plate margin?

    Model answer

    Oceanic plate meeting continental plate, oceanic meeting oceanic, and continental meeting continental.

  2. 2

    What happens where an oceanic plate meets a continental plate?

    Model answer

    The denser oceanic plate is forced down beneath the continental plate into the mantle, producing a deep ocean trench offshore and fold mountains with volcanoes inland.

  3. 3

    Name a mountain range formed at an oceanic to continental margin and the plates responsible.

    Model answer

    The Andes, formed as the Nazca plate is subducted beneath the South American plate.

  4. 4

    Explain why magma is generated above a subducting slab.

    Model answer

    Water held in the wet sediments and minerals of the descending plate is driven off as the slab heats, and it lowers the melting point of the mantle wedge above so that the mantle melts.

  5. 5

    Why is magma at a subduction zone so explosive?

    Model answer

    It rises through and melts silica-rich continental crust, becoming viscous andesitic magma that traps its dissolved gas until the pressure is released violently.

  6. 6

    What is the Benioff zone?

    Model answer

    The Benioff zone is the inclined band of earthquake foci that marks the descending slab at a subduction zone, dipping away from the trench beneath the overriding plate.

Other ways to work this

The same content, four other ways.

What is inside Levo

Six ways to work the same material.

1Closed book
2Open book
3Closed book

The 3-step method, run for you

Answer cold, learn it, then prove it stuck. Levo tracks the jump between your first attempt and your last.

Coastal Landscapes
Glaciated Landscapes
Tectonic Hazards
Changing Places

Cram a whole paper in one sitting

Sort every topic into what you know and what you do not, then drill only the weak ones.

Governments must win votes.
ruralurbanelite

Blank Blitz makes facts automatic

Rapid timed gap-fills on the terms and numbers you need to recall without thinking.

AFew coastal people recognised the signs.
BThe coasts were densely populated.
CMany communities were struck with no notice at all.

Build It gets the exam shape right

Assemble a full-mark answer from its marking points, in the order an examiner wants them.

The Mariana Trench reaches almost 11,000 m below sea level.
TrueFalse

Test It catches misconceptions

Spot the fault in a statement. The traps are the mistakes students actually make.

721941163128510

Brain Breaks between sessions

Short focus games to reset attention, so the next set lands better than the last.

Every question in Tectonic Hazards, on a schedule.

Attempt a question from memory, write the correct version, then attempt it again. Levo records the jump between your first attempt and your last, and brings each question back on the day you are due to forget it.

Or £46 a year, about £3.83 a month. Cancel anytime.