PRINTABLES | SECURING | ADVANCING Knowledge Notes
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PRINTABLES SECURING ADVANCING Knowledge Notes 1 INTRODUCE Y6 Physical processes Earthquakes, mountains and volcanoes SECURING structure of the Earth crust mantle outer core inner core cold, rocky outer layer makes up the surface of the
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01
PRINTABLES | SECURING | ADVANCING
Knowledge Notes 1 INTRODUCE
Y6 Physical processes
Earthquakes, mountains and volcanoes<br>
Knowledge Notes 1 INTRODUCE
Y6 Physical processes
Earthquakes, mountains and volcanoes<br>
02
SECURING structure of the Earth crust mantle outer core inner core cold, rocky outer layer makes up the surface of the Earth, including sea floor and continents mantle inner core crust liquid rock with varying
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron outer core very, very hot and mostly made of solid iron with gold and silver about the same
size as the Moon structure of the Earth crust mantle outer core inner core cold, rocky outer layer makes up the surface of the Earth, including sea floor and continents mantle inner core crust liquid rock with varying
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron outer core very, very hot and mostly made of solid iron with gold and silver about the same
size as the Moon structure of the Earth crust mantle outer core inner core cold, rocky outer layer makes up the surface of the Earth, including sea floor and continents mantle inner core crust liquid rock with varying
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron outer core very, very hot and mostly made of solid iron with gold and silver about the same
size as the Moon 2<br>
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron outer core very, very hot and mostly made of solid iron with gold and silver about the same
size as the Moon structure of the Earth crust mantle outer core inner core cold, rocky outer layer makes up the surface of the Earth, including sea floor and continents mantle inner core crust liquid rock with varying
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron outer core very, very hot and mostly made of solid iron with gold and silver about the same
size as the Moon structure of the Earth crust mantle outer core inner core cold, rocky outer layer makes up the surface of the Earth, including sea floor and continents mantle inner core crust liquid rock with varying
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron outer core very, very hot and mostly made of solid iron with gold and silver about the same
size as the Moon 2<br>
03
structure of the Earth crust mantle outer core inner core cold, rocky outer layer makes up the surface of the Earth, including sea floor and continents mantle inner core crust driven by heat from the core liquid rock with varying
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron rotates faster than the rest of the planet outer core very, very hot and mostly made of solid iron with gold, platinum and silver about the same size as the moon ADVANCING structure of the Earth crust mantle outer core inner core cold, rocky outer layer makes up the surface of the Earth, including sea floor and continents mantle inner core crust driven by heat from the core liquid rock with varying
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron rotates faster than the rest of the planet outer core very, very hot and mostly made of solid iron with gold, platinum and silver about the same size as the moon structure of the Earth crust mantle outer core inner core cold, rocky outer layer makes up the surface of the Earth, including sea floor and continents mantle inner core crust driven by heat from the core liquid rock with varying
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron rotates faster than the rest of the planet outer core very, very hot and mostly made of solid iron with gold, platinum and silver about the same size as the moon 3<br>
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron rotates faster than the rest of the planet outer core very, very hot and mostly made of solid iron with gold, platinum and silver about the same size as the moon ADVANCING structure of the Earth crust mantle outer core inner core cold, rocky outer layer makes up the surface of the Earth, including sea floor and continents mantle inner core crust driven by heat from the core liquid rock with varying
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron rotates faster than the rest of the planet outer core very, very hot and mostly made of solid iron with gold, platinum and silver about the same size as the moon structure of the Earth crust mantle outer core inner core cold, rocky outer layer makes up the surface of the Earth, including sea floor and continents mantle inner core crust driven by heat from the core liquid rock with varying
viscosity
(stickiness / thickness) Very hot and mostly made of
liquid iron rotates faster than the rest of the planet outer core very, very hot and mostly made of solid iron with gold, platinum and silver about the same size as the moon 3<br>
04
affected by the heat from inside of the Earth major tectonic plates (much bigger than the size
of the continents) SECURING affected by the heat from inside of the Earth major tectonic plates (much bigger than the size
of the continents) affected by the heat from inside of the Earth major tectonic plates (much bigger than the size
of the continents) 4<br>
of the continents) SECURING affected by the heat from inside of the Earth major tectonic plates (much bigger than the size
of the continents) affected by the heat from inside of the Earth major tectonic plates (much bigger than the size
of the continents) 4<br>
05
ADVANCING 5<br>
06
causes | volcanoes (and a few earthquakes) pull apart causes | earthquakes (no volcanoes) causes | volcanoes earthquakes causes | volcanoes earthquakes SECURING causes | volcanoes (and a few earthquakes) pull apart causes | earthquakes (no volcanoes) causes | volcanoes earthquakes causes | volcanoes earthquakes causes | volcanoes (and a few earthquakes) pull apart causes | earthquakes (no volcanoes) causes | volcanoes earthquakes causes | volcanoes earthquakes 6<br>
07
causes | volcanoes (and a few earthquakes) pull apart or separate causes | earthquakes (no volcanoes) causes | volcanoes earthquakes causes | volcanoes earthquakes ADVANCING causes | volcanoes (and a few earthquakes) pull apart or separate causes | earthquakes (no volcanoes) causes | volcanoes earthquakes causes | volcanoes earthquakes causes | volcanoes (and a few earthquakes) pull apart or separate causes | earthquakes (no volcanoes) causes | volcanoes earthquakes causes | volcanoes earthquakes 7<br>
08
earthquake tectonic plate | plate boundary
(fault line)
| pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake = M focus
(where the earthquake occurs) | shock waves produced epicentre | point on the Earth’s surface directly above the focus of an earthquake SECURING earthquake tectonic plate | plate boundary
(fault line)
| pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake = M focus
(where the earthquake occurs) | shock waves produced epicentre | point on the Earth’s surface directly above the focus of an earthquake earthquake tectonic plate | plate boundary
(fault line)
| pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake = M focus
(where the earthquake occurs) | shock waves produced epicentre | point on the Earth’s surface directly above the focus of an earthquake 8<br>
(fault line)
| pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake = M focus
(where the earthquake occurs) | shock waves produced epicentre | point on the Earth’s surface directly above the focus of an earthquake SECURING earthquake tectonic plate | plate boundary
(fault line)
| pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake = M focus
(where the earthquake occurs) | shock waves produced epicentre | point on the Earth’s surface directly above the focus of an earthquake earthquake tectonic plate | plate boundary
(fault line)
| pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake = M focus
(where the earthquake occurs) | shock waves produced epicentre | point on the Earth’s surface directly above the focus of an earthquake 8<br>
09
earthquake tectonic plate | plate boundary
(fault line)
|
|
focus
(where the earthquake occurs) | shock waves produced | vibrations travel as seismic waves
epicentre | point on the Earth’s surface directly above the focus of an earthquake pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake (M) ADVANCING earthquake tectonic plate | plate boundary
(fault line)
|
|
focus
(where the earthquake occurs) | shock waves produced | vibrations travel as seismic waves
epicentre | point on the Earth’s surface directly above the focus of an earthquake pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake (M) earthquake tectonic plate | plate boundary
(fault line)
|
|
focus
(where the earthquake occurs) | shock waves produced | vibrations travel as seismic waves
epicentre | point on the Earth’s surface directly above the focus of an earthquake pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake (M) 9<br>
(fault line)
|
|
focus
(where the earthquake occurs) | shock waves produced | vibrations travel as seismic waves
epicentre | point on the Earth’s surface directly above the focus of an earthquake pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake (M) ADVANCING earthquake tectonic plate | plate boundary
(fault line)
|
|
focus
(where the earthquake occurs) | shock waves produced | vibrations travel as seismic waves
epicentre | point on the Earth’s surface directly above the focus of an earthquake pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake (M) earthquake tectonic plate | plate boundary
(fault line)
|
|
focus
(where the earthquake occurs) | shock waves produced | vibrations travel as seismic waves
epicentre | point on the Earth’s surface directly above the focus of an earthquake pull apart scrape collide Moment Magnitude Scale | strength of an
earthquake (M) 9<br>
10
mountains fold mountain | continental plates collide dome mountain | molten rock rises and pushes layers of rock up fault-block mountain |
blocks of rock drop or shift down volcanic mountain |
magma spills onto the Earth’s crust as lava – cools and hardens orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced SECURING 10 mountains fold mountain | continental plates collide dome mountain | molten rock rises and pushes layers of rock up fault-block mountain |
blocks of rock drop or shift down volcanic mountain |
magma spills onto the Earth’s crust as lava – cools and hardens orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced mountains fold mountain | continental plates collide dome mountain | molten rock rises and pushes layers of rock up fault-block mountain |
blocks of rock drop or shift down volcanic mountain |
magma spills onto the Earth’s crust as lava – cools and hardens orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced<br>
blocks of rock drop or shift down volcanic mountain |
magma spills onto the Earth’s crust as lava – cools and hardens orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced SECURING 10 mountains fold mountain | continental plates collide dome mountain | molten rock rises and pushes layers of rock up fault-block mountain |
blocks of rock drop or shift down volcanic mountain |
magma spills onto the Earth’s crust as lava – cools and hardens orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced mountains fold mountain | continental plates collide dome mountain | molten rock rises and pushes layers of rock up fault-block mountain |
blocks of rock drop or shift down volcanic mountain |
magma spills onto the Earth’s crust as lava – cools and hardens orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced<br>
11
mountains fold mountain | formed when
continental plates collide dome mountain | formed when
molten rock rises and pushes layers of rock up fault-block mountain | formed when
blocks of rock drop or shift down compared to other blocks volcanic mountain | formed when
magma spills onto the Earth’s crust as lava – cools and hardens to form new layers orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced
(e.g. rocks uplifting) ADVANCING 11 mountains fold mountain | formed when
continental plates collide dome mountain | formed when
molten rock rises and pushes layers of rock up fault-block mountain | formed when
blocks of rock drop or shift down compared to other blocks volcanic mountain | formed when
magma spills onto the Earth’s crust as lava – cools and hardens to form new layers orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced
(e.g. rocks uplifting) mountains fold mountain | formed when
continental plates collide dome mountain | formed when
molten rock rises and pushes layers of rock up fault-block mountain | formed when
blocks of rock drop or shift down compared to other blocks volcanic mountain | formed when
magma spills onto the Earth’s crust as lava – cools and hardens to form new layers orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced
(e.g. rocks uplifting)<br>
continental plates collide dome mountain | formed when
molten rock rises and pushes layers of rock up fault-block mountain | formed when
blocks of rock drop or shift down compared to other blocks volcanic mountain | formed when
magma spills onto the Earth’s crust as lava – cools and hardens to form new layers orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced
(e.g. rocks uplifting) ADVANCING 11 mountains fold mountain | formed when
continental plates collide dome mountain | formed when
molten rock rises and pushes layers of rock up fault-block mountain | formed when
blocks of rock drop or shift down compared to other blocks volcanic mountain | formed when
magma spills onto the Earth’s crust as lava – cools and hardens to form new layers orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced
(e.g. rocks uplifting) mountains fold mountain | formed when
continental plates collide dome mountain | formed when
molten rock rises and pushes layers of rock up fault-block mountain | formed when
blocks of rock drop or shift down compared to other blocks volcanic mountain | formed when
magma spills onto the Earth’s crust as lava – cools and hardens to form new layers orogeny is a word that describes how mountains are formed through folding or fault-block processes
orogeny
| |
mountain born / produced
(e.g. rocks uplifting)<br>
12
magma rises through cracks thin, runny lava
lava runs a long way from the crater – gentle slopes giant
thick, sticky lava
steep sides magma stored in magma chamber
huge explosions
steep sides SECURING magma rises through cracks thin, runny lava
lava runs a long way from the crater – gentle slopes giant
thick, sticky lava
steep sides magma stored in magma chamber
huge explosions
steep sides 12<br>
lava runs a long way from the crater – gentle slopes giant
thick, sticky lava
steep sides magma stored in magma chamber
huge explosions
steep sides SECURING magma rises through cracks thin, runny lava
lava runs a long way from the crater – gentle slopes giant
thick, sticky lava
steep sides magma stored in magma chamber
huge explosions
steep sides 12<br>
13
magma rises through fractures or cracks thin, runny lava (low viscosity)
lava runs a long way from the source – gentle slopes majestic giants
thick, sticky viscous lava
steep sides
symmetrical cone magma stored in magma chamber
huge explosions
steep sides ADVANCING magma rises through fractures or cracks thin, runny lava (low viscosity)
lava runs a long way from the source – gentle slopes majestic giants
thick, sticky viscous lava
steep sides
symmetrical cone magma stored in magma chamber
huge explosions
steep sides 13<br>
lava runs a long way from the source – gentle slopes majestic giants
thick, sticky viscous lava
steep sides
symmetrical cone magma stored in magma chamber
huge explosions
steep sides ADVANCING magma rises through fractures or cracks thin, runny lava (low viscosity)
lava runs a long way from the source – gentle slopes majestic giants
thick, sticky viscous lava
steep sides
symmetrical cone magma stored in magma chamber
huge explosions
steep sides 13<br>