What will happen to the Cocos Plate

Plate of Cocos: Location and General Characteristics - Scienc

Other articles where Cocos Plate is discussed: mountain: The Caribbean chains: Plate another small plate, the Cocos Plate, is being underthrust beneath Mexico and Central America. A belt of volcanoes extends from northern Panama to western Mexico, and virtually all of the highest mountains in this belt are volcanic. These volcanoes are built on thickened crust, and crustal shortening has. Stein speculated that the Cocos Plate could have been pulled downward in what he called a sudden bending event that extended along its length and that the earthquakes are just a sideshow for.

The Cocos plate scoots rapidly under the continental crust of the North American plate, which builds up the stress and strain at a faster rate, Bellini says. So you're liable to have. The Juan de Fuca Plate is a small tectonic plate (microplate) generated from the Juan de Fuca Ridge that is subducting under the northerly portion of the western side of the North American Plate at the Cascadia subduction zone. It is named after the explorer of the same name.One of the smallest of Earth's tectonic plates, the Juan de Fuca Plate is a remnant part of the once-vast Farallon Plate. Caribbean Plate. The Caribbean Plate is a mostly oceanic tectonic plate underlying Central America and the Caribbean Sea off the north coast of South America. Roughly 3.2 million square kilometers (1.2 million square miles) in area, the Caribbean. Plate borders the North American Plate, the South American Plate, the Nazca Plate and the Cocos Plate The January 31, 1906 M8.5 earthquake occurred on the shallowly dipping megathrust interface of this plate boundary segment. Along the western coast of Central America, the Cocos plate subducts towards the east beneath the Caribbean plate at the Middle America Trench. Convergence rates vary between 72-81 mm/yr, decreasing towards the north

Cocos and Rivera Plates - Americas:Tectonic

  1. The Juan de Fuca plate is separated into three semi-independent segments, two of which are shown in Fig. 19.1, the Juan de Fuca and Gorda segments. The third, the Explorer segment, is off the Canadian coast. The Cascadia trench, which marks the subduction zone of all three segments, is less than 100 miles from the coastline
  2. The top part of the S American plate rolls to the West, pinned at the tip at Antartica. The Nazca plate just to the West of the S American plate and the Cocos plate that would be pushed by both toward the West, are thus pushed westward during this process
  3. Other articles where Caribbean Plate is discussed: North America: 120 to 30 million years ago: Cuba, was sheared off the Caribbean Plate and became fixed to the North American Plate. An east-dipping subduction zone was reestablished beneath Central America, detaching the Caribbean Plate from the Pacific. Continued subduction of the central Atlantic lithosphere beneath the eastern part of.

Powerful earthquake split a tectonic plate in tw

(Cocos Plate to the north, Nazca Plate to the south). 3. Using the overhead projector and the overhead model that was prepared in advance, demon-strate how magma extrudes at the ridge. Place the red overhead transparency and paper copy of Figure 1 (that has been cut and taped) on the overhead projector. The paper will block out the light The Pacific Plate is the largest of the 7 major tectonic boundaries.With a size of 102,900,000 km 2, it more than doubles the size of the South American Plate.. Plate tectonics are odd because they often consist of oceanic and continental crust.For example, the Pacific Plate underlies the Pacific Ocean with the Hawaiian Islands positioned smack dab in the middle Descent angle of the Cocos Plate = __32.5 degrees ___. Convergent Boundaries—Location 3: The convergent plate boundary along the Aleutian Islands Click each of the volcanoes in the Places sidebar to fly from one to the next. Click their icons for pictures and background information The Nazca plate is an oceanic tectonic plate in the southeastern Pacific Ocean that shares both convergent and divergent boundaries, corners multiple triple junctions, contains three seamount chains, overrides four hotspots, and is responsible for the creation of the Andean orogeny (Figure 1).Over the last half-century, it has garnered much attention from the scientific and political community.

Caribbean Plate. The Caribbean Plate is a mostly oceanic tectonic plate underlying much of Central America and the Caribbean Sea off the north coast of South America.. Approximately 3,319,000 sq km (1,281,000 sq mi) in area, the Caribbean Plate borders the North American Plate, the South American Plate, the Nazca Plate and the Cocos Plate.These borders are regions of intense seismic activity. The Cocos Plate was made by ocean floor spreading along with the East Pacific Rise and the Cocos Edge, particularly in a complicated region geologist call the Cocos-Nazca spreading framework. From the rise, the plate is pushed eastbound and pushed or dragged (maybe both) beneath the less dense Caribbean Plate, within the handle called subduction Off the Pacific coast of Costa Rica, for instance, a COCONet station on the isolated Isla del Coco is the only GPS station continuously tracking the Cocos plate as it dives beneath the Caribbean. Caribbean plate The Caribbean plate is an oceanic tectonic plate that underlies Central America and the Caribbean sea. Surrounding the Caribbean plate are the North American plate, the South American plate, and the cocos plate. The North American plate lies to the north and to the east and it is converging

Cocos-Nazca spreading regimes and a major propagator. In addition to these sharply defined tectonic boundaries are overprinted boundaries from volcanism during passage of Cocos Plate over the Galapagos hot spot. The subducted segment boundaries correspond with distinct changes in upper plate tectonic structure and features of the subducted slab This process is called forced subduction. Here we have an example where the Cocos Plate, within 30 million years of being created, is being forced to subduct under the Caribbean Plate because the oceanic lithosphere is converging directly with continental lithosphere. Here is an example of spontaneous subduction occurring off the coast of Japan Both quakes were sparked by heightened tension between the Cocos tectonic plate, which borders the western coast of Mexico, and the North American tectonic plate. As the Cocos plate slid. Today, the plate is bounded to the west by the Cocos Plate, which dives under the Caribbean plate just west of Central America. This movement built and sustains the region's volcanoes

The current continental and oceanic plates include: the Eurasian plate, Australian-Indian plate, Philippine plate, Pacific plate, Juan de Fuca plate, Nazca plate, Cocos plate, North American plate, Caribbean plate, South American plate, African plate, Arabian plate, the Antarctic plate, and the Scotia plate Cocos Plate Eurasian Plate Juan de Fuca Plate Indian Plate Nazca Plate North American Plate Philippine Sea Plate Pacific Plate Scotia Plate South American Plate These plates move because of convection currents that occur beneath them in the semi-molten layers of the Earth. New Zealand sits on the boundary of two of these plates, known as the. There have been several discussions surrounding people with allergies and the COVID vaccine. And while some allergies are a reason to hold off on getting vaccinated, Peter Marks, MD, the director for the FDA's Center for Biologics Evaluation and Research, says most aren't. Right now, the only things that would prevent you from getting vaccinated is if you had a known allergy to one of the. The South American Plate is moving westward while the Cocos Plate and the Nazca Plate are subducted beneath the South American Plate. 22. Towards Central America, there is the Caribbean Plate beneath which, the Cocos Plate is being subducted. 23 To the north of the Caribbean Plate lies the North American Plate and to the south of it lies the South American Plate. To the south west lie the Nazca Plate and Cocos Plate. The CSEC syllabus only requires you to know the Caribbean Plate and those around it but these are just a few of the Earth's crustal plates

Plate tectonics and basin formation. Plate tectonics regards the lithosphere broken into plate that are in motion. The plates move relative to another along plate boundaries, sliding upon the underlying asthenosphere (the layer below the lithosphere that is formed of molten rock). The theory of plate tectonics emerged since the 1960s, and until. The fragmentation of the proto-Cocos Plate has been attributed to pivoting subduction where the combination of trench resistance forces and slab pull forces changed the direction of convergence between the westernmost proto-Cocos Plate and the rest of the Cocos Plate and hence produced localized tension within the proto-Cocos Plate (Bandy. Mexico City Doomed By Its Geology To More Earthquakes : The Two-Way The problem is that just to the west, a huge slab of the Earth's crust called the Cocos Plate is grinding relentlessly toward. The Cocos plate migrates north, coverging and subducting under Central America. During the Neogene era (approximately five to twenty-four million years ago), the Galapagos Spreading Center was located directly over the Galapagos mantle plume which interacted to form two hotspot tracks, the Cocos and Carnegie Ridges The illustration below shows some of Earth's tectonic plates. The arrows indicate the direction in which some of these plates are moving.Based on the direction of the Cocos Plate, what type of plate boundary likely exists between the Cocos Plate and the Caribbean Plate

Convergent boundaries (subduction zone) Just north of the Nazca Plate, the oceanic Cocos Plate subducts under the Caribbean Plate and forms the Middle America Trench. The Cascadia subduction zone is where the oceanic Juan de Fuca, Gorda and Explorer Plates subduct under the continental North American plate The Pacific Plate acts a sort of museum of underwater paleo-geology. As such, it contains the largest area with remnants of the oldest geological players under the seabed inside the Asian oceanic trenches. There are evidences that the minor plates of Juan de Fuca, Nazca, and Cocos are what remain of an earlier plate called the Farallon The Cocos Plate is a minor plate that stretches for 2.9 million square km. It is geographically located off the coast of western Central America. The plate is around 23 million years old, which is relatively young in tectonic plate terms. The formation of the Cocos Plate can be traced to seafloor spreading, which generally occurs at mid-ocean. They also alter our planet's features, depending on how they meet. Giant mountain ranges have formed along boundaries that converge. Earthquakes can occur at any of the plate boundaries. The largest tectonic plate is the Pacific Plate with an area of 41,000,000 square miles (103,000,000 km²) Geologists initially thought the earthquake occurred where the Cocos ocean plate is being overridden by a continental plate. Megaquakes generally occur near the top of where plates converge, an.

In the grand, slow-moving world of tectonic plates, Mexico is situated at an unfortunate location: It rests at the southern edge of the North American Plate, putting it right at the point where it meets the Pacific Plate, the Cocos Plate and the Caribbean Plate. The quakes occur because all of these plates are moving in different directions. 1. Caribbean plate 2. Cocos plate 3. Nazca plate 4. Juan de Fuca plate 5. North American plate 6. Pacific plate 7. Philipine plate 8. Arabian plate 9. Eurasian plate 10. Australian plate 11. Antarctic plate 12. Scotia plate 13.Volcanic eruptions and earthquakes often happen at South American plate 14. African plate 15. Indian plate Refer to. Farallon Plate broke into the Cocos and Nazca Plates either 25 Ma (Hey, 1977) or 27 Ma (Lonsdale and Klitgord, 1978). On the other hand, recent studies of the magnetic pattern in the Cocos Plate have inferred faster spreading rates than were previously recognized, so the age of the Cocos Plate subducting beneath the Nicoya Peninsula may be younger The Ring of Fire is a direct result of plate tectonics and the movement and collisions of lithospheric plates. The eastern section of the ring is the result of the Nazca Plate and the Cocos Plate being subducted beneath the westward moving South American Plate. The Cocos Plate is being subducted beneath theCaribbean Plate, in Central America

Transform Plate Boundaries - Geology (U

The Pacific plate and the North American plate meet and result in many geologicfeatures on Earth. We are very familiar with what happens throughout the state ofCalifornia because of their meeting. But what about Alaska? The Cocos plate. The Pacific plate. The Scotia plate. Tags: Question 23 . SURVEY Caribbean tectonics encompasses the majority of the Caribbean Sea and southeast Pacific regions that include the Caribbean, Nazca, North Andean, Panama plates and the Galapagos and Caribbean microplates (Figure 1). These plates are dominantly oceanic and contain a diversity of interesting tectonic features such as all three of the dominant types of plate boundaries, multiple triple junctions.

This Recent Earthquake Was So Intense, It Has Cracked a

Signs of chocolate poisoning usually take around 6-12 hours to appear after the ingestion. Although dogs tend to recover within 24-48 hours (mostly), these symptoms can last up to 72 hours, in extreme cases. Some of the signs that may indicate the ingestion of chocolate by your pup are as follows: Vomiting. Diarrhea Plate boundaries are defined as the fault zones that separate the rigid interiors of plates. Many plate boundaries are narrow, particularly seafloor spreading centers and transform faults (discussed farther below). However, the following figure clearly shows that earthquakes in continents are often distributed over a broader region than in oceanic crust

Arenal Volcano: Plate Tectonic Setting. The volcanic arc of Costa Rica, where Arenal is located, is a chain of mountains resulting from the subduction of the Cocos tectonic plate under the Caribbean Plate. Costa Rica is part of the Central American isthmus, which connects the North and South American continents. Volcanoes are mostly confined to. Put the silver piece in a bowl or container. Use a container large enough to hold the silver piece you're cleaning. Make sure it's deep enough so you can submerge the silver completely. Lay the silver on the bottom of the container. 2. Pour the Coke into the container until the silver is submerged. Make sure the silver is completely covered.

Many rift valleys are part of triple junctions, a type of divergent boundary where three tectonic plates meet at about 120° angles. Two arms of the triple junction can split to form an entire ocean. The third, failed rift or aulacogen, may become a rift valley.The Atlantic Ocean, for instance, is a result of a triple junction that started in what is now the Gulf of Guinea on the. The map below shows the type of data that helped geologists understand where and why most earthquakes occur. Study the global distribution and depth of large earthquakes that occurred between 1975 and 1995. Then click on the map to compare the locations of earthquakes with plate boundaries. Compare the location of earthquakes and plate boundaries (Coco's, 1150 Colorado Blvd., Saturday 12/14 at 7pm). We had a great turnout at the banquet last year and I'm hoping for the same this year. If I don't see you there, well, here's an early Happy New Year, and may your collecting be ever vigorous. Editor's Page Greg Burns Editor 6 The California Numismatist • Winter 201 Thus the N American Plate and the Pacific Plate were involved in plate adjustments as well as the Caribbean and the Cocos plates! The continuous pressure of the S American roll also caused the Fuego volcano in Guatemala to violently erupt on September 14, 2012. This point in Guatemala also lies on the edge of the Caribbean Plate where it is. The Ring of Fire, also referred to as the Circum-Pacific Belt, is a path along the Pacific Ocean characterized by active volcanoes and frequent earthquakes. Its length is approximately 40,000 kilometers (24,900 miles). It traces boundaries between several tectonic plates—including the Pacific, Juan de Fuca, Cocos, Indian-Australian, Nazca.

  1. Plate tectonics is a scientific theory describing the large-scale motion of the plates making up the Earth's lithosphere since tectonic processes began on Earth between 3.3 and 3.5 billion years ago. The model builds on the concept of continental drift, an idea developed during the first decades of the 20th century
  2. Why Do Earthquakes Happen? African Plate Nazca Plate Pacific Plate South American Plate North American Pl ate Cocos Plate Caribbean Plate Antarctic Plate Somali Plate Philippine Plate Australia Plate India Plate Eur si n Plate Arabian Plate Scotia Plate Juan de Fuca Plate 23 10 29 79 106 46 32 12 6 8 8 14 54 59 74 9 9 21 105 102 1 1 1200 New.
  3. e has been consumed, things may get much worse. If a dog ate a lot of chocolate, he may lose control of his legs and collapse. He may also have a seizure, and if untreated may fall into a coma. Fatalities can and do occur
  4. In recent years, the popularity of coconut and particularly coconut oil has soared because of touted health benefits. Fueling the coconut oil trend, celebrity endorsements have claimed the ingredient to help blast away belly fat, curb appetite, strengthen the immune system, prevent heart disease, and stave off dementia and Alzheimer's disease

Cocos Plate geology Britannic

  1. Scotia Plate is among the 38 small plates covering an area of about 1,600,000 sq. km. On the western boundary, the relative motion between the Antarctic Plate and the Scotia Plate is roughly around 13mm/year. The North Scotia ridge is formed when the northern edge of the Scotia Plate is bounded by the South American Plate
  2. I have taken this idea seriously over the past several years and done field work. The impact was like a magnitude 11. The extreme seismic waves did trigger small earthquakes. We found fault scarp the formed just after (within hours) of the impact.
  3. Caribbean 7 of 10. As can be seen from plate tectonics, Central America is being pushed over the Cocos Plate. When this is done violently during the 7 of 10 roll, the crumbling we have described for these lands will occur. The small islands just to the east of Central America will participate in this crush. The Caribbean Plate will be pushed up.
  4. Furthermore, large earthquakes have not been observed along the flat segment. They occur only on the plate interface updip from the point where Cocos plate commences unbending, ∼10 km inland from the coast. The flat segment shows little inslab seismic activity and the diving slab into the mantle is completely devoid of earthquakes
  5. This final kink in the Cocos plate is located right where the 7.1 earthquake happened, and directly beneath the Valley of Mexico, in which Mexico City is located. This warping of the Cocos plate.
  6. The Cocos plate begins its subduction beneath Central America at the Middle America Trench, about 300 km (186 miles) to the southwest of this earthquake. The location, depth, and normal-faulting mechanism of this earthquake indicate that it is likely an intraplate event, within the subducting Cocos slab, rather than on the shallower megathrust.
  7. The cause was simple plate tectonics — or modern continental drift — which is what causes most major earthquakes, according to Live Science. Usually, the Cocos Plate moves along the coast of.

What Caused Mexico's 2 Major Earthquakes in 2 Weeks

JetStream Max: World's Major Tectonic Plates. Since earthquakes are responsible for almost 90% of the tsunamis on record, it is useful to better understand earthquakes and the forces that cause them. Doing this requires looking into Earth's construction. Earth's interior is made up of layers. Scientists define these layers in two ways The Orozco and Cocos plates are oceanic crusts located in the southern part of Mexico. The collision between the two was the cause of the great earthquake of 1985 in Mexico City as well as the most recent earthquake of 2012. Tectonic plates may have three types of edges between them. They are said to be divergent if the plates move away from. 7 Major Tectonic Plates. 1. Pacific Plate. At 103 million square kilometers, the Pacific plate is the largest of all the lithospheric plates. The Pacific Plate is almost entirely oceanic, except for the areas around New Zealand and part of California west of the San Andreas Fault They, the politic activist, successfully convert the NGA page to shadowland and left every corrupted there. My Chinese friend told me the latest incident happen because they finally hit the right spot (because Cover is japan company and Coco is used to be USA citizen) everything is on fire and make hololive left China

Other medical complications can also occur, including possible secondary bacterial infection. In the most critical cases, there may be overwhelming infection with sepsis and septic shock. If your tiredness is progressing and becoming extreme, this is a sign the coronavirus infection is becoming severe, and your pneumonia is worsening At the same time, the Cocos Plate is under subduction by the forces of the Caribbean Plate in Central America. Besides, beneath the North American plate there is the subduction of a small portion of the Juan de Fuca Plate along with a section of the Pacific plate On top of this, the Cocos plate is denser than the landmass of Mexico itself, meaning the country's soft earth crumbles more easily. This combination makes it one of the most seismically active.

Unusual Mexico earthquake may have relieved stress in

Mexico's back-to-back earthquakes, explained by a

But what about the changes that will inevitably happen after we're long gone? Landscape of Costa Rica in 10,000 years. In 10,000 years, Costa Rica could look fairly different. The Cocos plate is currently moving at a rate of 9 centimeters per year in a northwest direction, subducting underneath the Caribbean plate This plate also measures 43,600,000 sq kilometers. Somali plate. This plate encompasses Somalia, an African country. It is a minor plate that measures 16,700,000 sq kilometers. Others are the Nazca plate, Philippine Sea plate, Arabian plate, Caribbean plate, Cocos plate, Caroline plate, and Scotia plate. Plate Movement: How Does It Take Place

Relate the location of folded mountains, earthquakes, and volcanic activity to tectonic plate boundaries. Barys North American Plate Eurasian Plate Pacific Plate Pacific Plate po Nazca Australian Platel Plate African Plate South American Cocos Plate Plate Antarctic Plate KEY Plate boundary Direction that plate is moving What pattern do you see The Puerto Rico Trench: Implications for Plate Tectonics and Earthquake and Tsunami Hazards. The Puerto Rico Trench is the deepest part of the Atlantic Ocean, with water depths exceeding 8,400 meters (figure 1). Its depth is comparable to the deep trenches in the Pacific Ocean. Trenches in the Pacific are located in places where one tectonic. As the Cocos plate moves under the Caribbean plate at a rate of about 75 millimeters per year, it exerts pressure on the Caribbean plate. That pressure formed the mountains and the volcanoes. To ease the pressure, the earth near the edge of the plate shifts from time to time along weak points or faults. The January 8 earthquake did not occur. Cool things happen at subduction zones. In Lesson 6 we explored volcanoes that happen at these plate boundaries. Now let's explore how those plate boundaries move mechanically to generate earthquakes, and a relatively newly discovered phenomenon called slow slip. First of all, let's remember what a subduction zone looks like, and what kinds. Earthquakes are common in Mexico because of most of the land mass being on the North American plate and the Ocean floor being on the Coscos plate and so when the more dense ocean floor plate goes up and hits the North American plate it goes up under the more finer granite part of the North American plate and if you were to push something heavy across the table you'll notice it kinda creates a.

Juan de Fuca Plate - Wikipedi

  1. Cocos Plate: The Cocos Plate is a tectonic plate that lies under the Pacific Ocean off the west coast of Central America. Eurasian Plate : The Eurasian Plate contains most of the continents of Europe and Asia. The plate also contains some of the northeast region of the Atlantic Ocean
  2. e these and related questions. Location of study area in the equatorial Pacific (white box). Right panel was constructed in GeoMapApp and shows existing multibeam bathymetry data at the western end of the Cocos-Nazca spreading center. Located at ~ 2°20'N and ~ 35 km east of the.
  3. tall beds), so slugging can occur in even some large units. Bubble sizes larger than two-thirds the diameter of the bed can cause slugging. Geldart Group C. Geldart Group C powders are typi-cally less than 30 μm and are the most difficult to fluidize
  4. A perfect example of an oceanic- continental plate boundary is the one between the Cocos Plate and the Caribbean Plate. In this case the Cocos plate is more dense therefore sub ducting underneath the Caribbean Plate as shown on the picture above. This Spontaneous subduction zone, because of the gravitational instability of the oceanic.
  5. ated by plate interactions of the Caribbean plate with the North American and Cocos plate, the present-day subduction zone and transform margin, respectively (Donnelly et al., 1990). In the first case, oblique convergence with the Cocos plate has produce

Caribbean Plate Geology Pag

They think that seawater infiltrated into the Cocos plate and potentially accelerated the cooling, which also made it more prone to the types of earthquakes seen in older and colder locations As can be seen from plate tectonics, Central America is being pushed over the Cocos Plate. When this is done violently during the 7 of 10 roll, the crumbling we have described for these lands will occur. The small islands just to the east of Central America will participate in this crush The Caribbean Plate lies in a complex area. It borders the North American Plate, the South American Plate, the Nazca Plate and the Cocos Plate plus several microplates. These two major plates and two minor plates bordering it includes oceanic and continental crust. Caribbean Sea covers most of the plate The submarine Cocos Ridge is a bathymetric high of more than 1000 km length and 250-500 km width, that raises about 2000 m above than the adjacent seafloor [4,19,20] (Figure1a). The ridge is oriented NE-SW parallel to the recent motion of Cocos Plate, and extends from the Cocos-Nazca spreading center north of Galápagos Platform to the Middl

M 7.7 - 123km NNW of Lucea, Jamaica - USG

Impatiens in Containers. Impatiens planted in pots require water more frequently, as potting soil in containers dries quickly. Check the impatiens daily and water whenever the top of the potting soil feels dry. During hot, dry weather, impatiens may require water twice daily. Never allow the potting soil to dry completely Plate tectonics is the theory that Earth's outer shell is divided into large slabs of solid rock, called plates, that glide over Earth's mantle, the rocky inner layer above Earth's core Effective Monday July 1 a new H.O.A. reform bill goes into effect essentially ending the run of so called H.O.A dictatorships in Florida Earth's Major Plates: The current continental and oceanic plates include: the Eurasian plate, Australian-Indian plate, Philippine plate, Pacific plate, Juan de Fuca plate, Nazca plate, Cocos plate, North American plate, Caribbean plate, South American plate, African plate, Arabian plate, the Antarctic plate, and the Scotia plate

CONTINENTAL DRIFT - Paleontology and Geology Glossary

Juan De Fuca Plate - an overview ScienceDirect Topic

The Andes were formed by tectonic activity whereby Earth is uplifted as one plate (oceanic crust) subducts under another plate (continental crust). To get such a high mountain chain in a. The Mexico Trench is located north of the Galapagos Islands at the Cocos and Caribbean plate boundary. Tectonic plate motion is responsible for most of the seismic activity in the region. Earthquakes are driven by stresses inside the earth. Earthquakes are located at boundaries between the tectonic plates. The great earthquakes (magnitude 8. Figure 10.4. 1 A map showing 15 of the Earth's tectonic plates and the approximate rates and directions of plate motions. 10.04: Plate Plate Motions and Plate Boundary Processes#fig10.4.1. Rates of motions of the major plates range from less than 1 cm/y to over 10 cm/y. The Pacific Plate is the fastest, followed by the Australian and Nazca. North American Plate Movement. The east-side of the North American Plate straddles the Eurasian Plate and African Plate.This is the Mid-Atlantic Ridge where divergent tectonic plates pull apart from each other. In turn, we find some of the youngest geologic rocks at these mid-oceanic ridges The country sits atop three of the Earth's largest tectonic plates — the North American plate, the Cocos Plate, and the Pacific Plate. Whenever these chunks of crust grind or butt up against.

Mexico earthquake: soft soil makes capital shake like itPlate_Tectonics_Notes (1)What are the 7 major crustal plates of the Earth? - QuoraAna's Blog: February 2019