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Intrusive igneous rock, large crystals
Impermeable rock
Batholith – mass of intrusive igneous rock
reaching surface ( exposed when overlying
rock is eroded)
 Granite Mostly found in:
 South West England and
North Scotland and
West and East coasts of Ireland.
Tough, resistant to erosion and weathering
Consists of: grey quartz, black mica, pink
feldspar
Feldspar - Decays to form kaolin (china
clay)
Granite has cracks or joints
Vertical joints formed when granite cooled
and contracted
Horizontal joints formed due to release of
pressure (from overlying rocks)
Joints make granite vulnerable to
mechanical weathering
Impermeable rock – granite moorlands
oftenly wet, marshy with lots of rivers.
Isolated outcrop of granite on a hilltop
Linton suggested:
- Spacing of vertical joints
- Some close, some far apart
- Warm and wet conditions, with deep
chemical weathering
- Closely spaced joints eroded quicker
- Erosion and slumping removed weathered
granite forming tor

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Granite landscapes

  • 1.
  • 2. Intrusive igneous rock, large crystals Impermeable rock Batholith – mass of intrusive igneous rock reaching surface ( exposed when overlying rock is eroded)  Granite Mostly found in:  South West England and North Scotland and West and East coasts of Ireland.
  • 3. Tough, resistant to erosion and weathering Consists of: grey quartz, black mica, pink feldspar Feldspar - Decays to form kaolin (china clay)
  • 4. Granite has cracks or joints Vertical joints formed when granite cooled and contracted Horizontal joints formed due to release of pressure (from overlying rocks) Joints make granite vulnerable to mechanical weathering Impermeable rock – granite moorlands oftenly wet, marshy with lots of rivers.
  • 5. Isolated outcrop of granite on a hilltop Linton suggested: - Spacing of vertical joints - Some close, some far apart - Warm and wet conditions, with deep chemical weathering - Closely spaced joints eroded quicker - Erosion and slumping removed weathered granite forming tor