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Following Hitler’s appointment as chancellor the Nazis were finally in a position of power.
However, this power was limited, as the Nazis were just one party in a three party coalition government, under President Hindenburg.
This topic will explore how the Nazis managed to eliminate their opposition and consolidate ultimate power over Germany, whilst maintaining an illusion of democracy.
It will first explore this topic in chronological order, from the Reichstag Fire through to the death of President Hindenburg, and then explore it thematically in the last section. On the 31 January 1933, Hitler, conscious of his lack of a majority in the Reichstag, immediately called for new elections to try and strengthen his position. The Nazis aimed to increase their share of the vote so that they would have a majority in the Reichstag. This would allow them to rule unopposed and unhindered by coalition governments.
Over the next two months, they launched themselves into an intense election campaign.
On 27 February 1933, as the campaign moved into its final, frantic days, the Reichstag, the German Parliament building, was set on fire and burnt down. An atmosphere of panic and terror followed the event.
This continued when a young Dutch communist, Van der Lubbe was arrested for the crime.
The Nazi Party used the atmosphere of panic to their advantage, encouraging anti-communism. Göring declared that the communists had planned a national uprising to overthrow the Weimar Republic. This hysteria helped to turn the public against the communists, one of the Nazis main opponents, and 4000 people were imprisoned.
The day after the fire, Hindenburg signed the Emergency Decree for the Protection of the German People. On the 28 February 1933, President Hindenburg signed the Emergency Decree for the Protection of the German People. This decree suspended the democratic aspects of the Weimar Republic and declared a state of emergency.
This decree gave the Nazis a legal basis for the persecution and oppression of any opponents, who were be framed as traitors to the republic. People could be imprisoned for any or no reason.
The decree also removed basic personal freedoms, such as the freedom of speech, the right to own property, and the right to trial before imprisonment.
Through these aspects the Nazis suppressed any opposition to their power, and were able to start the road from democracy to a dictatorship. The atmosphere of uncertainty following the Reichstag Fire secured many voters for the Nazi party.
The SA also ran a violent campaign of terror against any and all opponents of the Nazi regime. Many were terrified of voting of at all, and many turned to voting for the Nazi Party out of fear for their own safety. The elections were neither free or fair.
On the 5 March 1933, the elections took place, with an extremely high turnout of 89%.
The Nazis secured 43.9% of the vote.
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2. The power of waves is a significant factor in coastal
processes.
There are constructive and destructive waves.
3.
4.
5. The power of waves is one of the most significant forces of
coastal change.
Waves are created by wind blowing over the surface of the
sea.
As the wind blows over the sea, friction is created -
producing a swell in the water.
The energy of the wind causes water particles to rotate inside
the swell and this moves the wave forward.
7. The size and energy of a wave is influenced by:
• how long the wind has been blowing
• the strength of the wind
• how far the wave has travelled (the fetch)
9. Waves can be destructive or constructive.
When a wave breaks, water is washed up the beach - this is
called the swash.
Then the water runs back down the beach - this is called the
backwash.
With a constructive wave, the swash is stronger than the
backwash.
With a destructive wave, the backwash is stronger than the
swash.
10. Destructive waves are created in storm conditions.
• They are created from big, strong waves when the wind is
powerful and has been blowing for a long time.
• They occur when wave energy is high and the wave has
travelled over a long fetch.
• They tend to erode the coast.
• They have a stronger backwash than swash.
• They have a short wave length and are high and steep.
11.
12. • They are created in calm weather and are less powerful than
destructive waves.
• They break on the shore and deposit material, building up
beaches.
• They have a swash that is stronger than the backwash.
• They have a long wavelength, and are low in height.
13.
14. The sea shapes the coastal landscape. Coastal erosion is the
wearing away and breaking up of rock along the coast.
Destructive waves erode the coastline in a number of ways:
Hydraulic action. Air may become trapped in joints and cracks on
a cliff face. When a wave breaks, the trapped air is compressed
which weakens the cliff and causes erosion.
Abrasion. Bits of rock and sand in waves grind down cliff
surfaces like sandpaper.
15. Attrition. Waves smash rocks and pebbles on the shore into
each other, and they break and become smoother.
Solution. Acids contained in sea water will dissolve some
types of rock such as chalk or limestone.
16. There are various sources of the material in the sea. The
material has been:
• eroded from cliffs
• transported by longshore drift along the coastline
• brought inland from offshore by constructive waves
• carried to the coastline by rivers
18. Waves can approach the coast at an angle because of the
direction of the prevailing wind.
The swash of the waves carries material up the beach at an
angle.
The backwash then flows back to the sea in a straight line at
90°. This movement of material is called transportation.
Continual swash and backwash transports material sideways
along the coast.
This movement of material is called longshore drift and
occurs in a zigzag.
20. There are four ways that waves and tidal currents transport
sediment.
These can then contribute to the movement of sediment by
longshore drift.
21.
22. When the sea loses energy, it drops the sand, rock particles
and pebbles it has been carrying.
This is called deposition.
Deposition happens when the swash is stronger than the
backwash and is associated with constructive waves.
24. Deposition is likely to occur when:
• waves enter an area of shallow water
• waves enter a sheltered area, eg. a cove or bay
• there is little wind
• there is a good supply of material