Norway Impact Craters
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Specimen above is a second iteration fractal shattercone in limestone found north of Oslo.
Torbjorn Larsson of Oslo made this picture outside of Oslo. It is an impact sequence with particle storm with resonance structures. Cobalt, manganese magenta, iron, silica ... Anyway the particle storm is in high shock melt state.
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Impact Bricking shown in the Baltic Sea Anomaly. Baltic Sea anomaly - Wikipedia
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The Baltic Sea Anomaly is the center of a large earth accretion impact. These type impacts involve earth recoil and since they are so large and impacts usually occur at an angle they slide under and push up earth crust. As to weather the British Isles are also part of this structure I cannot tell. It would appear the Norway coast is the crater wall so to speak with it being an arc crater from accretion.
Mosaic bricking disk, melt bubble and push up structure shown on this detail of the Baltic Sea Anomaly.
Step wave harmonic. This is the wavelength of the shock wave at this point. Notice it peels along these wave lines. That is because the wave will pause and delineate its edge. This is true for shatter cones a triangle wave and all the other types. As for the circled figures they are plasma form defects like evaporative holes. Impact is a progressive event and these figures appear to be a later part of this structure even a rain down effect.
The Lofoten Archipelago is located between the 67th and 68th parallels north in the Arctic Circle of northern Norway and is known for its extraordinary natural beauty and for being a major cod fishing centre. Lofoten includes the municipalities of Vågan, Vestvågøy, Flakstad, Moskenes, Værøy and Røst. The main islands, from north to south.
Besides having narrow coning wave structure which is the highest energy type of this wave you can see an overlapping of the triangle wave chevrons, a diamond chevron. In the up flow of wave energy you can see it bifurcate a dual coning structure and then settle down into the pure triangle wave with overlap. Above that it is going into a break up of the energy which would lead to the familiar lightning tree fractal but this structure is encased in an overall strong tringle wave. This was a very powerful earth impact.
A big old impact off the coast of Norway.
This slide is from: RESEARCH ARTICLE| OCTOBER 01, 2010
Global pulsations of intraplate magmatism through the Cenozoic
Rolf Mjelde;
Paul Wessel;
R. Dietmar Müller
Lithosphere (2010) 2 (5): 361–376.
The Canvass Crater - Canvass Craters are big old accretion craters that have a crater plain that is now filled with subsequent smaller impacts. They frame the painting. It can be hard to tell which canvass you are working.
Planetary Landscapes
June 11 ·
Tycho Crater's Peak | On June 10, 2011, NASA's Lunar Reconnaissance Orbiter spacecraft angled its orbit 65° to the west, allowing the LRO Camera NACs to capture a dramatic sunrise view of Tycho crater. A very popular target with amateur astronomers, Tycho is located at 43.37°S, 348.68°E, and is about 51 miles (82 km) in diameter. The summit of the central peak is 1.24 miles (2 km) above the crater floor. The distance from Tycho's floor to its rim is about 2.92 miles (4.7 km).Tycho crater's central peak complex, shown here, is about 9.3 miles (15 km) wide, left to right (southeast to northwest in this view). Credit: NASA Goddard/Arizona State University
View full size image here: https://www.nasa.gov/.../565736main_M162350671LE_full.jpg
Notice how remarkably similar this is to earth mountains. These are large "shattercones." Large shattercones = Mountains.
Zsótér Ferenc · Aug. 3, 2023.
River Långan in Sweden.
Crater Signatures - Harmonic banding, sine wave to coning, impact expansion voids, harmonic energy fractal bleeding. Large powerful earth impacts get overlooked for lack of impact forensic physics theory. Let's take a look at the crater on exaggerated topology of your location, see attached.
Harmonic banding. Notice those beautiful front faces go from a sine wave to a coning feature on the center. That is the physics mechanism of shatter cones. The cookie cutter approach to understanding shatter cones by looking for small Shoemaker Wells Creek low power striations will not help when you do not understand the physical mechanism. Higher power coning does not have striations as it is melting the subject rock. Low power striations still retain lower power imprinting. Banding is a result of harmonic attenuation where the minerals resonate at different frequencies thereby separating them. The iron is from the impacting bolide imparted as a pulverized blast material with free larger inclusions as shown in picture (circled.) Notice the central sign wave is flanked on both sides by coning which even tilts towards the center.
Impact expansion and fractal bleeding. - Over power energy expressions. Impact energy often cannot be imprinted in the explosion. This will make voids. Harmonic banding can be too much energy to imprint as banding and these bands will bleed cracks and fractals in a perpendicular form. A tree fractal is a lower form of energy. It is a physics form shift. In this exposure the form is in it's highest power only able to produce trunks.
High heat mosaic with directionality splatterform. It is the largest splatterform I have ever seen and would be from a large earth impact. the boulder and splatterform arrived as a unit. The boulder sags because it was plastic at the time of landing. Melt coning, not the harmonic type we call shatter cones. This melt coning is a landing direction as you can see it is counter to gravity. Aug. 5, 2023.
Geology
Charlie Plisinsky · 10h ·
Any ideas what is it? Smallest and closest picture I could take, round like a tree.
Diameter ca 2,5m
Northern Norway Bodø, near Mjelle beach
May I use this picture? High velocity viscous merger, thin plane insertion from impact. The rubble was in a high heat state and mosaic cracking. The impact progression blows these jets of melted matter streams out at hypersonic speeds. Aug. 6, 2023.
This was a very large impact. The physics of crack conformity. Notice how the banding is falling into the cracks or melting into them. A smaller crack a smaller conformity. As any slow sedimentary process you have to explain the crack that the insert layer went into which is not evident as there are many cracks which do not have the insert band. Then you have to explain how the sedimentary banding was overturned yet all still in a line as these are broken boulders. The odd of that are nil. Less than winning the billion dollars in the lottery. Without a viable mechanism you have no theory. Impact explains this with one uniform mechanism. This has never been observed in thousands of years of volcanic activity. How would tectonics do this?
Philip Mansfield · ·
Does anyone know how these rock formations were formed and what they are called?
Photo taken at Tueneset, Álesund in Norway
High heat mosaic bricking, fractals shown left side and crossing planar features. Gurskøya, Møre Romsdal, Norway. Bricking is not normal for mosaic surfaces as they are a fractal like the one in front. The bricking mosaic is following the bricking imprint laid down by the cross planar shock. The fractal left is thought to be a petroglyph, but is a long fractal energy signature. Remember this is a crater that has Iceland as a central uplift so this energy is at a scale much larger than the smaller craters. Sept. 4, 2023.
Philip Mansfield photography. Sept. 4, 2023.
The earth has over a million surface craters of a mile diameter or greater. You can see this with lidar and snow. Dec. 7, 2023.
LiDAR and Aerial Archaeology ·
Meteorite crate with smaller craters from 700-200 Bc.
Kaali, Saaremaa, Estonia.
Old-Greeks said that this was sun god Helios son Phaeton death(falling).
Vikings have said that this was Thor arrival.
Geological map (scale 1:5 million) of Finland (Korsman et al., 1997). The big craters of Finland. Feb. 4, 2024.
Field photographs of typical shatter cones at the Keurusselkaïmpact structure. a) Large well developed full cone in metavolcanic rock from Jylha¨nniemiJylha¨nniemi site (KE; coordinates N62°9¢9.3¢¢, E24°39¢4¢¢). The cone is approximately 18 cm wide. b) More or less flat in situ shatter cone in granodioritic rock from Harmaaniemi site (KV; coordinates N62°7¢58¢¢, E24°40¢25.7¢¢). Note that the cone is almost vertical, dipping upward. Arrows indicate the approximate apex direction. Fig 2 - uploaded by Gordon R. Osinski Keurusselkä is a lake in Central Finland between the towns of Keuruu to the north and Mänttä to the south. It covers an area of 117.3 km2 (45.3 sq mi). Its average depth is 6.4 m (21 ft) with a maximum depth of 40 m (130 ft). The surface lies at 105.4 m (346 ft) above sea level. The lake is 27 km (17 mi) long and is a part of the Kokemäenjoki water system.[1][2][3] Keurusselkä gained international publicity in 2004 when a pair of amateur geologists discovered an ancient impact crater on the western shore of the lake.[4]
Landsat 7 image of the Keurusselkä region. Area where shatter cones have been found is marked with a red ellipse and the suggested impact structure of Ukonselkä is marked with a white circle.
Tri Crater. Geologist go to all the trouble to expense this detail mapping and ignore the crater(s), instead hung up on where shatter cones were found. I found much higher energy shatter cones in the Howell Structure but only at one place. A crater defines itself better in these anomaly maps.
(a) Bouguer gravity and (b) airborne magnetic map of the Keurusselkä area (for details, see Pesonen et al., 2004 and references therein). Small dots in (a) are places with gravity measurements. (D ~ 2.5 km) is shown in upper right corner. (Aeromagnetic map, courtesy Hanna Leväniemi, Geologial Survey of Finland.)
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Jan 2005
A new meteorite impact structure "Keurusselkä" was discovered in Central Finland in 2003 by S. Hietala and J. Moilanen (Hietala and Moilanen, 2004a, 2004b). The discovery was based on shatter cone findings in a circular area of some 10 km in diameter between the village of Kolho and the western shore of the lake Keurusselkä.