Blue zones New Zeeland
by Henryk Szubinski
I found some similarity of the Okinawa blue zones Ridges and the apperance of ridges around New Zeeland.I will show this feature on the first image. That the ridgges are more prominent when the whole of an island or continent has ridgges may indicate that they surround the shape by 360 degrees of motion and the excluded are of the land has it's
Area INVERSION = the 360 degrees x the number of ridges and their directions.
A ridge or mountain ridge is a geological feature consisting of a chain of mountains or hills that form a continuous elevated crest for some distance. Ridges are usually termed hills or mountains as well, depending on size. There are several main types of ridges:-
- Dendritic ridge:- In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed, or other chance occurrences. This type of ridge is generally somewhat random in orientation, often changing direction frequently, often with knobs at intervals on the ridge top.
- Stratigraphic ridge:- In places such as the Ridge-and-Valley Appalachians, long, even, straight ridges are formed because they are the uneroded remaining edges of the more resistant dipping strata that were folded laterally. Similar ridges have formed in places such as the Black Hills, where the ridges form concentric circles around the igneous core. Sometimes these ridges are called "hogback ridges".
- Oceanic spreading ridge:- In tectonic spreading zones around the world, such as at the Mid-Atlantic Ridge, the volcanic activity forming new plate boundary forms volcanic ridges at the spreading zone. Isostatic settling and erosion gradually reduce the elevations moving away from the zone.
- Crater ridges:- Large meteorite strikes typically form large impact craters bordered by circular ridges.
- Volcanic crater/caldera ridges:- Large volcanoes often leave behind a central crater/caldera bordered by circular ridges.
- Fault ridges:- Faults often form escarpments. Sometimes the tops of the escarpments form not plateaus, but slope back so that the edges of the escarpments form ridges.
- Dune ridges:- In areas of large-scale dune activity, certain types of dunes result in sand ridges.
- Moraines and eskers:- Glacial activity may leave ridges in the form of moraines and eskers. An arête is a thin ridge of rock that is formed by glacial erosion.
- Volcanic subglacial ridges:- Many subglacial volcanoes create ridge-like formations when lava erupts through a thick glacier or ice sheet.
- Shutter ridges:- A shutter ridge is a ridge which has moved along a fault line, blocking or diverting drainage. Typically, a shutter ridge creates a valley corresponding to the alignment of the fault that produces it.
The sun light reflections are visable but there is some other side of the shore that bulges into it by way of water. Probably the water has become bent into a smooth curvature that is higher than the shoreline height.
very prominent ATLANTIC BLUE HUE.
Sand hill between two land massess and it's blue color because of the low water level increases the temperature of it.
MAGIC
Wizard
Galactic
Aside from the Atlantic blue of the background on a wizards hat, the blue around the stars is usually this color.
More ridging
Wizards hat effect as seen from above.
The above image displays the shape of a sphere around the land tipp that has another round shape in it's middle as similar to the image below.
This may be the cause of the ridges that simulate the warping of the sphere that we have seen with the warping of the whole Earth on the map.
The above image has another level of a smaller spherical bubble inside it that rests on top of the main warping of the ocean as bubble effects
that are leaving Earth's gravity but is pressed back by smaller bubble sections on top of the larger bubble section as though it were moving the
polarization response as action and reactions of buoyancy and gravity and escape velocity of the way that polarizations may happen by the
other direction of gravity shining back to it's position within the Earth bubble of Earth's atmosphere.The basics of the Wizards hat.
This may be the cause of the ridges that simulate the warping of the sphere that we have seen with the warping of the whole Earth on the map.
The above image has another level of a smaller spherical bubble inside it that rests on top of the main warping of the ocean as bubble effects
that are leaving Earth's gravity but is pressed back by smaller bubble sections on top of the larger bubble section as though it were moving the
polarization response as action and reactions of buoyancy and gravity and escape velocity of the way that polarizations may happen by the
other direction of gravity shining back to it's position within the Earth bubble of Earth's atmosphere.The basics of the Wizards hat.
Mapthematics or the map mathematics as defining the ridges of the Earth where the conecting ridges of the Earth and it's warping may indicate the way that blue zones are made as matter .The position of the Bubble shown previously may be positioned so that on each side of the map shown below, the bubble may reappear or moove over the Earth as the tidal pull positions of the motion of the MOON.