Southpacificocean Free Stock Images

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Brunch of white of tiare flowers at green outdoors background

Brunch of white of tiare flowers at green outdoors background

Brunch of white of tiare flowers at green outdoors background

Brunch of white of tiare flowers at green outdoors background

An old Indian cave located on a remoteTurks and Caicos Island. Beautiful Caribbean sea glowing and warm sunlight bathing some remote palm trees on a deserted island. An old Indian cave located on a remoteTurks and Caicos Island. Beautiful Caribbean sea glowing and warm sunlight bathing some remote palm trees on a deserted island.

Brunch of blossoming yellow tiare flowers

Brunch of blossoming yellow tiare flowers

Brunch of yellow tiare flowers at green outdoors background

Brunch of yellow tiare flowers at green outdoors background

Close up of yellow tiare flowers at green outdoors background

Close up of yellow tiare flowers at green outdoors background

Banks Peninsular.NZ

Banks Peninsula is situated in about the middle of the east coast of the South Island on the margin of the Canterbury Plains. It is approximately 450 sq. miles in area and its highest point is Herbert Peak, 3,014 ft. It comprises two extinct volcanoes which were active less than half a million years ago. Their craters have subsequently been enlarged to many times their original size by stream erosion; they were then invaded by the sea during the postglacial world-wide rise in sea level beginning about 15,000 years ago. They now form the harbours of Lyttelton and Akaroa. Originally Banks Peninsula was an island, but it became tied to the Canterbury Plains at some late stage in geological history when the growing alluvial plain reached its base. Banks Peninsula is situated in about the middle of the east coast of the South Island on the margin of the Canterbury Plains. It is approximately 450 sq. miles in area and its highest point is Herbert Peak, 3,014 ft. It comprises two extinct volcanoes which were active less than half a million years ago. Their craters have subsequently been enlarged to many times their original size by stream erosion; they were then invaded by the sea during the postglacial world-wide rise in sea level beginning about 15,000 years ago. They now form the harbours of Lyttelton and Akaroa. Originally Banks Peninsula was an island, but it became tied to the Canterbury Plains at some late stage in geological history when the growing alluvial plain reached its base.

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