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The alignment of these particular features is somewhat irregular; modern maps with much more detail show a broad zone of more regular alignments.

Subsequent geological investigations have suggested various refinements and adjustments. Most geological features are initially identified or characterized from a local expression of that feature.

The OWL was first identified as a perceptual effect, a pattern perceived by the human visual system in a broad field of many seemingly random elements.

But is it real? Or just an optical illusion , such as the Kanizsa triangle see image , where we "see" a triangle that does not really exist?

Raisz considered whether the OWL might be just a chance alignment of random elements, and geologists since have not been able to find any common unitary feature, nor identify any connection between the various local elements.

Davis called it a "fictional structural element". Yet it has been found to coincide with many faults and fault zones, and to delineate significant differences of geology.

But for all of its prominence, there is as yet no understanding of what the OWL is or how it came to be. The OWL piques the interest of geologically minded persons in part because its characteristic NW-SE angle of orientation — approximately 50 to 60 degrees west of north a little short of northwest [3] — is shared by many other seeming local features across a broad swath of geography.

Around Seattle these include strikingly parallel alignments at the south end of Lake Washington, the north side of Elliott Bay, the valley of the Ship Canal, the bluff along Interlaken Blvd.

All of these are carved into "recent" less than 18, years old glacial deposits, and it is difficult to conceive of how these could be controlled by anything other than a recent glacial process.

Yet the same orientation shows up in the Brothers, Eugene-Denio, and McLoughlin fault zones in Oregon see map , below , which are geological features tens of millions of years old, and the Walker Lane lineament in Nevada.

Likewise to the east, where both the OWL and the Brothers Fault Zone become less distinct in Idaho where they hit the old North American continental craton and the track of Yellowstone hotspot.

But some 50 miles to the north is the parallel Trans-Idaho Discontinuity, and further north, the Osburn fault Lewis and Clark line running roughly from Missoula to Spokane.

And aeromagnetic [4] and gravitational anomaly [5] surveys suggest extension into the interior of the continent.

A problem in evaluating any hypothesis regarding the OWL is a dearth of evidence. Raisz suggested that the OWL might be a "transcurrent fault" long strike-slip faults at what are now known to be plate boundaries , but lacked both data and competence to assess it.

One of the first speculations that the OWL might be a major geological structure Wise — written when the theory of plate tectonics was still new and not entirely accepted [6] — was called by the author "an outrageous hypothesis".

Modern investigation is still largely balked by the immense span of geography involved and lack of continuous structures, the lack of clearly cross-cutting features, and a confusing expression in both rock millions of years old and glacial sediments only 16, years old.

Geological investigation of a feature begins with determining its structure, composition, age, and relationship with other features.

The OWL does not cooperate. It is expressed as an orientation in many elements of diverse structure and compositions, and even as a boundary between areas of differing structure and composition; there is yet no understanding of what kind of feature or process — the "ur-OWL" — could control this.

Nor are there particular "OWL" rocks which can be examined and radiometrically dated. We are left with determining its age by looking at its relationship with other features, such as which features overlap or cross-cut other presumably older features.

In the following sections we will look at several features which might be expected to have some kind of structural relationship with the OWL, and consider what they might tell us about the OWL.

The most notable geological feature crossing the OWL is the Cascade Range , raised up in the Pliocene two to five million years ago as a result of the Cascadia subduction zone.

Raisz judged the Cascades on the north side of the OWL to be offset about six miles to the west, and similarly for the Blue Mountains, but this is questionable, and similar offsets are not apparent in the older — up to 17 Ma millions of years old — Columbia River basalt flows.

In general, there are no clear indications of structures offset by the OWL, but neither are there any distinct features crossing the OWL and older than 17 Ma that positively demonstrate a lack of offsetting.

For example, that the OWL is not offset suggests that it must be younger than the last strike-slip motion on the SCF, [9] anywhere from around 44 to about 41 million years ago [10] i.

While some geologists have speculated that it does continue directly south, albeit hidden under younger deposits, [12] not a trace has been found.

If the SCF fault does not continue directly southward [13] — and the utter lack of evidence that it does makes a case for evidence of lack — then where else might it be?

But that is inconsistent with the SCF itself and most other strike-slip faults associated with the OWL being right lateral dextral , and incompatible with the geology to the southeast.

Particularly, studies of the region to the southeast in connection with Department of Energy activities at the Hanford Reservation show no indication of any fault or other structure comparable to the SCF.

He has subsequently speculated [17] that the missing part of the SCF may have been dextrally offset to become a southerly trending fault in the Puget Lowland.

But same problem: later deposits cover any traces. The seeming southeasterly curvature is possibly explained as a geometrical effect of foreshortening: it occurs in a belt of intense folding much resembling a rug which has slid against a wall which, if unfolded, could restore some of the "curves" to a linear position along the southerly extension of the SCF.

There seem to be no indications that the SCF turns to the west. Although such indications would mostly be buried, the general sense of the topography suggests no such turn.

Displacement, to either the west or the east, seems unlikely in that certain effects that would be expected are not found. Could the SCF just end?

This is difficult to comprehend. If there is displacement along this fault, where did it come from? To quote Wyld et al. So perhaps the displacement came from the depths, and, as it was extruded, was eroded and redistributed as sediments.

But this has not been established. Another possibility is that the missing southern segment of the SCF is on a crustal block that rotated away from the OWL.

This suggests that a continuation of the SCF, if any, and the missing Cenozoic, might be somewhere southwest of Mount Saint Helens , but this has not been observed.

It runs east from a complex of faults on the southern end of Vancouver Island to the town of Darrington, where it turns south to converge with the SCF see map, above.

This can explain an early puzzle [25] as to why the Mesozoic rocks just south of the DDMFZ — the Western and Eastern Melange Belts — have no counterpart on the east side of the OWL and offset to the south: they were not faulted by the SCF, but were pushed against it from the southwest.

Then it gets curiouser. This suggests that the OWL was once a strike-slip fault, possibly a continental margin, along which terranes moved from the southeast.

But that upsets some of the "solutions" described above, and there is yet no consensus on this. This segment, and the associated Yakima fold belts , do include many northeast-trending faults crossing the OWL.

However, these are largely dip-slip vertical faults, associated with compressional folding of the overlying basalt. There is some evidence that some of the northwest-trending ridges may have some continuity with the basement structure, but the nature and details of the deeper structure is not known.

The seismic data showed a uniformity of rock type and thickness across the OWL that discounts the possibility of it being a boundary between continental and oceanic crust.

The results were interpreted as suggesting continental rifting during the Eocene, perhaps a failed rift basin , [31] possibly connected with the rotation of the Klamath Mountain block away from the Idaho Batholith see Oregon rotation , below.

West of there the OWL seems to follow a ridge in the basement structure, to the east it follows a gravity gradient, much like the Klamath—Blue Mountain LIneament see below does.

The Wallula Fault Zone is active, but whether that can be attributed to the OWL is unknown: it may be that, like the Yakima Fold Belt, it is a result of regional stresses, and is expressed only in the superficial basalt, quite independently of what ever is happening in the basement rock.

This system is complex and has been variously interpreted. The interaction of the Wallula and Hite Fault systems is not yet understood.

Past the Hite Fault System the OWL enters a region of geological complexity and confusion, where even the trace of the OWL is less clear, even to the point where it has been suggested that both the topographic feature and the Wallula fault are terminated by the Hite fault.

However, there is a sense that the trend of the faulting in that area turns more to the south; it has been suggested the faulting associated with the OWL takes a large step south to the Vale Fault Zone, [39] which connects with the Snake River Fault Zone in Idaho.

The Imnaha Fault striking towards Riggins, Idaho is more nearly in line with the rest of the OWL, and in line with the previously mentioned gravitational anomalies that run into the continent.

What this says about the nature of the OWL is unclear, although Kuehn concluded that, in northeastern Oregon or western Idaho, it is not a tectonically significant structure.

As described above, the trace of the OWL becomes faint and somewhat confused between the Blue Mountains and the margin of the North American craton the thick orange line on the map , just beyond the Oregon—Idaho border; the dashed line on the diagram below.

This is the Wallowa terrane, a piece of crust that drifted in from somewhere else and got jammed between the Columbia Embayment to the west and the North American continent to the east and north.

Grabens form where the crust is being stretched or extended. Several explanations have been offered as to why this is happening here.

Kuehn theorized that right-lateral slip on the Wallula Fault is being transferred to more southerly faults such as the Vale Fault, wherefore he labelled this region the Wallula—Vale Transfer Zone.

Another explanation is that clock-wise rotation of part of Oregon discussed below about a point near the Wallula Gap has pulled the Blue Mountains away from the OWL; [42] this might also explain why the OWL seems to be bending here.

These theories may all have some truth to them, but what they might imply regarding the genesis and structure of the OWL has not been worked out.

Hells Canyon — North America's deepest river gorge — is so deep because the terrain it cuts through is so high. This is generally attributed to thinning of the crust, which allows the hotter, and therefore lighter and more buoyant, mantle material to rise higher.

This is believed by many to be involved with the Yellowstone hotspot and Columbia River Basalts ; the nature of such involvement, if any, is hotly debated.

Likewise, clarification of the nature and history of the Wallowa terrane, and particularly of the nature and causes of the apparent bending and multiple alignments of the OWL in this region, would be a major step in understanding the OWL.

The bedrock of Washington and Oregon, like most of the continent, is nearly all pre-Cenozoic rock, older than 66 million years. The exception is southwestern Washington and Oregon, which has virtually no pre-Cenozoic strata.

This is the Columbia Embayment, a large indentation into the North American continent characterized by oceanic crust covered by thick sedimentary deposits.

In the geological past, the coast of North America was in Idaho and Nevada, as will be described later. The Columbia Embayment is of interest here because its northern margin is approximately delineated by the OWL.

The variations are mainly in the region of the CLEW , where sediments are buried under the basalts of the Columbia Basin , and in Puget Sound, where the Cenozoic geology extends as far north as Vancouver Island.

The southern edge of the Columbia Embayment is along a line from the Klamath Mountains on the Oregon coast to a point in the Blue Mountains just east of the Wallula Gap.

Unlike the OWL, this line has little topographical expression, [47] and aside from the Hite Fault System is not associated with any major fault systems.

Rotation of the earth's crust around the U. One interpretation of this is that western Oregon and southwestern Washington have swung as a rigid block about a pivot point at the northern end, near the Olympic Peninsula.

The interesting thing is: backing out this rotation restores the Coast Range to an earlier position nearly juxtaposed against the OWL.

Hammond argues that the Coast Range believed to be seamounts that had previously accreted to the continent were rifted away from the continent starting about 50 Ma ago mid- Eocene.

This interpretation implies a " back arc " of magmatism, probably fed by a subduction zone, and possibly implicated with the intrusion of various plutons in the North Cascades around 50 Ma.

The cause and nature of the rifting does not seem to have been worked out yet. Certain complications in the subduction of the Kula and Farallon plates may have been involved.

During this rotation of the Coast Range the block of continental crust that is now the Blue Mountains on the eastern side of the KBML was also rifted away from the Idaho batholith, and also rotated about 50 degrees, but about a point near the Wallula Gap or perhaps further east.

While the rigid-block rotation model has much appeal, many geologists prefer another interpretation that minimizes whole—block rotation, and instead of rifting invokes "dextral shear" resulting from the relative motion of the Pacific plate past the North American plate, or possibly from the extension of the Basin and Range province as the primary driving force.

The large values of paleomagnetic rotation are explained by a "ball bearing" model: [55] the entire Oregon block western Oregon including the Cascades and southwestern Washington are deemed to be composed of many smaller blocks on the scale of tens of kilometers , each of which rotates independently on its own axis.

Evidence of such small blocks at least in southwestern Washington has been claimed. How this affects the postulated rifting does not seem to have been addressed.

Modern measurements show that central Oregon is still rotating, with the calculated rotation poles bracketing the Wallula Gap, [59] which is approximately the intersection of the OWL and KBML.

It is intriguing to consider whether the KBML has participated in this rotation, but this is unclear; that it is unbent where it crosses the OWL suggests it is not.

The OWL seems to be the northern edge of the rotating block, [60] and the paucity of paleomagnetic data to the southeast of the KBML suggests it might be the southern edge.

But the details of all this remain murky. Such a fault was once proposed [61] on the basis of certain marine seismic data, but the proposal was stiffly rejected, and now seems to have been abandoned.

Combined terrestrial and bathymetric topography shows a distinct lineament along the west side of Puget Sound from Vashon Island just north of Tacoma north to the west side of Holmes Harbor and Saratoga Passage on Whidbey Island see image.

But at Port Madison at the red bar in the image it is split by a distinct offset of several miles. Curiously, the southern section lies in the approximate zone of the OWL.

Note OWL—associated lineaments running parallel to the red line. This suggests dextral offset along a strike-slip fault. But if that is the case then there should be a major fault in the vicinity of Port Madison and crossing to Seattle perhaps at the Ship Canal, aligned with the red line — but for this there is even less evidence than there was for the Puget Sound fault.

That it seems to be expressed in Ice Age 16 Ka deposits implies a very recent but entirely unknown event; but perhaps these recent deposits are only draped over a much older topography.

A recent offset might explain the apparent offsetting of north—south glacial drumlins bisected by the Ship Canal, but is not evident in more eastern segments.

Alternately — and this would seem very pertinent in regard of the OWL — perhaps some mechanism other than strike-slip faulting creates these lineaments.

This is not a strike-slip fault, but a thrust fault , where a relatively shallow slab of rock from the south is being pushed against and over the northern part.

And over the OWL. These models were developed in study of the western segment of the Seattle Fault.

In the center segment, where it crosses surface exposures of Eocene rock associated with the OWL, the various strands of the fault — elsewhere fairly orderly — meander.

The significance of this and the nature of the interaction with the Eocene rock are also not known. Examination of the various strands of the Seattle Fault, particularly in the central section, is similarly suggestive of ripples in a flow that is obliquely crossing some deeper sill.

This is an intriguing idea that could explain how local and seemingly independent features could be organized from depth, and even across a large scale, but it does not seem to have been considered.

This is likely due, in part, to a paucity of information on the nature and structure of the lower crust where such a sill would exist.

Other faults to the south also show a similar turn, [68] suggesting a general turning or bending across the OWL, yet such a bend is not apparent in the pattern of physiographic features that express the OWL.

With awareness that the Seattle Fault and the RMFZ are the edges of a large sheet of material which is moving north, there is a distinct impression that these faults, and even some of the topographical features, are flowing around the corner of the Snoqualmie Valley.

If it seems odd that a mountain should "float" around a valley: bear in mind that while the surface relief is about three-quarters of a kilometer half a mile in height, the material flowing could be as much as eighteen kilometers deep.

It is worth noting that Cedar Butte — a minor prominence just east of Cedar Falls — is the southwestern-most exposure in the region of some very old Cretaceaous pre-Cenozoic metamorphic rock.

In such a context the observed arcuate fault bends would be very natural. It is generally assumed [ by whom? As has been shown, study of features that should interact with OWL has yielded very little: a tentative age range between 45 and 17 million years , suggestions that the ur-OWL arises from deep in the crust, and evidence that the OWL is not contrary to expectations itself a boundary between oceanic and continental crust.

The lack of results so far suggests that the broader context of the OWL should be considered. Following are some elements of that broader context, which may — or may not — relate in some way to the OWL.

The broadest and fullest context of the OWL is the global system of plate tectonics , driven by convective flows in the Earth's mantle. The primary story on the western margin of North America is the accretion, subduction, obduction, and translation of plates, micro-plates, terranes, and crustal blocks between the converging Pacific and North American plates.

For an excellent geological history of Washington, including plate tectonics, see the Burke Museum web site. The principal tectonic plate in this region Washington, Oregon, Idaho is the North American plate , consisting of a craton of ancient, relatively stable continental crust and various additional parts that have been accreted; this is essentially the whole of the North American continent.

The interaction of the North American plate with various other plates, terranes, etc. Since the breakup of the Pangaea supercontinent in the Jurassic about million years ago the main tectonic story here has been the North American Plate's subduction of the Farallon Plate see below and its remaining fragments such as the Kula , Juan de Fuca , Gorda , and Explorer plates.

As the North American plate overrides the last of each remnant it comes into contact with the Pacific Plate, generally forming a transform fault , such as the Queen Charlotte Fault running north of Vancouver Island , and the San Andreas Fault on the coast of California.

Between these is the Cascadia subduction zone , the last portion of a subduction zone that once stretched from Central America to Alaska.

This has not been a steady process. This had repercussions on all the adjoining plates, and may have had something to do with initiation of the Straight Creek Fault, [72] and the end of the Laramide orogeny the uplift of the Rocky Mountains.

This event may have set the stage for the OWL, as much of the crust in which it is expressed was formed around that epoch the early Eocene ; this may be when the story of the OWL starts.

Other evidence suggests a similar plate reorganization around 80 Ma, [73] possibly connected with the start of the Laramide orogeny.

Ward claimed at least five "major chaotic tectonic events since the Triassic". Each of these events is a possible candidate for creating some condition or structure that affected the OWL or ur-OWL, but knowledge of what these events were or their effects is itself still chaotic.

Complicating the geology is a stream of terranes — crustal blocks — that have been streaming north along the continental margin [74] for over Ma [75] and probably much, much earlier , what has recently been called the North Pacific Rim orogenic Stream NPRS.

Roughly million years ago during the Jurassic period the Pangaea supercontinent began to break up as a rift separated the North American Plate from what is now Europe, and pushed it west against the Farallon Plate.

The Farallon plate is notable for having been very large, and for subducting nearly horizontally under much of the United States and Mexico; it is likely connected with the Laramide Orogeny.

The period 48—50 Ma mid-Eocene is especially interesting as this is when the subducted Kula—Farallon spreading ridge passed below what is now the OWL.

Around 30 Ma ago part of the spreading center between the Farallon Plate and Pacific Plate was subducted under California, putting the Pacific plate into direct contact with the North American plate and creating the San Andreas Fault.

The remainder of the Farallon Plate split, with the part to the north becoming the Juan de Fuca Plate ; parts of this subsequently broke off to form the Gorda Plate and Explorer Plate.

By this time the last of the Kula Plate had been subducted, initiating the Queen Charlotte transform fault on the coast of British Columbia; coastal subduction has been reduced to just the Cascadia Subduction Zone under Oregon and Washington.

Unlike anything on the OWL, these lava flows can be dated, and they show a westward age progression from an origin at the McDermitt Caldera on the Oregon-Nevada border to the Newberry Volcano.

Curiously, the Yellowstone hotspot also appears to have originated in the vicinity of the McDermitt Caldera, and is generally considered to be closely associated with the Newberry magmatism.

Alternative models include: [85] 1 flow of material from the top layer of the mantle asthenosphere around the edge of the Juan de Fuca Plate a.

A paper by Morgan [88] suggested that this seamount—OWL alignment marks the passage some Ma ago of the Bermuda hotspot. This same passage has also been invoked to explain the Mississippi Embayment.

The paper also suggested that passage of a hot spot weakens the continental crust, leaving it vulnerable to rifting. But might the relation actually run the other way: do some of these "hotspots" accumulate in zones where the crust is already weakened by means as yet unknown?

The supposed Newberry hotspot track may exemplify this see Megashears, below , but application of this concept more generally is not yet accepted.

Application to the OWL would require resolving some other questions, such as how traces of a ca. Possibly there is some explanation, but geology has not yet found it.

The OWL gets faint, perhaps even terminates, just east of the Oregon—Idaho border where it hits the north-trending Western Idaho Shear Zone WISZ , [91] a nearly vertical tectonic boundary between the accreted oceanic terranes to the west and the plutonic and metamorphic rock of the North American craton the ancient continental core to the east.

From the Mesozoic till about 90 Ma mid- Cretaceous this was the western margin of the North American continent, into which various off-shore terranes were crashing into and then sliding to the north.

Near the town of Orofino just east of Lewiston, Idaho something curious happens: the craton margin makes a sharp right-angle bend to the west.

The truncation occurred between 90 and 70 Ma ago, possibly due to the docking of the Insular super-terrane now the coast of British Columbia.

Then another curious thing happens: before the west-trending craton margin turns north, it seems to loop south towards Walla Walla near the Oregon border and the Wallula Gap see orange-line here , or dashed-line here.

Although southeastern Washington is pretty thoroughly covered by the Columbia River Basalts, a borehole in this loop recovered rock characteristic of the craton.

Afterwards, however, Kruger showed a vague hint of empathy after allowing Grisha to stay with him to watch the airship, citing that since he was here, he may as well see it.

Amidst the conversation, he looked into the traumatized Grisha's eyes, seeing pure hatred and a desire for revenge. Two years later, Kruger inherited the power of the " Attack Titan " from an unknown predecessor, gaining the power of the Titans.

Thirteen years after inheriting his power, when the "Curse of Ymir" was beginning to take hold of his health, [17] Kruger was present when Grisha was tortured by the Public Security Authorities.

He asked if he confessed to the Owl's identity, and Grisha assured he did not know. Kruger announced the boat that will send the Restorationists to Paradis Island was ready.

During the operation at Paradis Island, Kruger escorts Grisha from the top of a thirty-foot wall, telling Grisha that as punishment for treason, he will be transformed into a Titan.

Grisha tells Kruger that he remembers him from all those years back when his sister was murdered, with Kruger emotionlessly acknowledging this.

He also calmly watched the Restorationists being turned into mindless Titans and chase after their comrade. As it was Dina Fritz 's turn to be transformed, Kruger violently silenced a yelling Grisha and held him in place.

When Gross was about to throw Grisha off the Wall, Kruger suddenly intervened and pushed his comrade off the wall, and revealed to a shocked Grisha that he was the Owl.

While mutilating his hand, he taught Grisha how to use the power of the Titans before, in his Titan form, destroying the Marleyan steamboat and slaughtering all the remaining soldiers.

Kruger then set Grisha free and answered all the questions of the latter, justifying his deeds and telling him about his life.

Before letting a determined Grisha inherit his ability in order to fulfill the Eldian Restorationists goal, Kruger revealed him the name of the Titan he would become [1] and explained the history of the Founding Titan and King Fritz 's vow with the Founding Titan renouncing all war.

As he prepared to inject Grisha with a Titan serum , he urged him to find a family and complete his mission for the sake of Armin and Mikasa.

Grisha was confused by these names, and Kruger admitted that he did not know whose memories he was seeing. Sign In Don't have an account?

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