Thin Lizzy Whiskey in the Jar

The stack will then be attacked right at the base by the wave, and this will weaken this structure thus collapsing to create a stump.Beaches are unique geological features which tend to fluctuate between the retreat and advance of the sediments.

A headland of considerable size often is called a cape. The sea erodes the softer rock faster than the harder rock, forming a bay. Bays are usually formed where weaker rocks like clay and sand are eroded leaving a band of harder rocks. The stable beach is made up of stable hard rocks, which cannot be affected by the waves. Through the deposition of sediment within the bay and the erosion of the headlands, coastlines eventually straighten out. Bays and headlands usually form on a discordant coastline, where the coastline has bands of rocks with varying resistance which run perpendicular to the coastline. The waves are diffracted around the headland and also near the beach when it is in a static equilibrium state.

Less resistant rock (e.g. Headlands are characterized by high, breaking waves, rocky shores, intense erosion, and steep sea cliffs. This increases the shear stress in the cliff-forming material and accelerates mass movement.Wave refraction disperses wave energy through the bay, and along with the sheltering effect of the headlands, this protects bays from storms.

Headlands are formed when the sea attacks a section of coast with alternating bands of hard and soft rock. The harder rock that is left protruding into the sea is the headland.

Bays are made up of soft rocks while headlands are made up of hard rocks. boulder clay) erodes more rapidly than less resistant rock. If a cave is formed on the headland, it might break through to the other side thus creating an arch. Headlands are characterised by breaking waves, rocky shores, intense erosion and steep sea cliffs. A bay is surrounded by land on three sides, whereas a headland is surrounded by water on three sides. The joints on the headland are usually eroded back to create a cave, which can erode further to create arches.Caves are formed by erosion and weathering of the band of hard rocks on the already formed headland. The unshaped beaches are usually reshaped by the continuous deposition and erosion on the beach. Once it is at static equilibrium, the unstable beaches will stabilize and can no longer be affected by erosion.The wave refraction breaks the wave energy through the bays, and the sheltering effect of the headlands protects the bay from storms. Bays form where less resistant rocks, such as In the formation of sea cliffs, wave erosion undercuts the slopes at the shoreline, which retreat landward. Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. This increases the shear stress in the cliff-forming material and accelerates mass movement.Wave refraction disperses wave energy through the bay, and along with the sheltering effect of the headlands, this protects bays from storms. Hard rocks like granites can resist the wave which causes erosion resulting in the creation of a peninsula (a raised land mass) while the softer rocks like clay are easily eroded thus creating bays. A bay is the reverse, an area of water bordering land on three sides. A gulf generally occupies an area larger than a bay and may itself contains one or more bays. The arch will eventually grow bigger until it collapses leaving a stack on one side and the headland on the other. It is a type of promontory. 2. Headlands and bays form on discordant coastlines, where the land consists of bands of rock o…

The caves form when the waves go through the cracks on the cliff face. This effect means that the waves reaching the shore in a bay are weaker than the waves reaching the headland, and the bay is thus a safer place for water activities like surfing or swimming.

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Thin Lizzy Whiskey in the Jar