Essay Question 1: Compare and contrast the topographical features at divergent and convergent plate margins.
Subject: Earth Environments 1: Geomorphology and Soils
Course Code: GEOG 1231
Divergent and convergent plate margins are both studied in plate tectonics; which is the study of the plates that makeup the lithosphere, their movements and how these movements has influenced changes in the surface’s topography (Strahler, 2011, 389). The driving force that causes these plate movements is the gradual movement of the semi-molten rock that makes up the asthenosphere (Kious, 1996, 28). Features observed at these margins share some similarities but, also vary quite largely. These differences are caused by the different movements displayed at
…show more content…
Finally unlike divergent plate margins convergent zones can have a continental plate colliding with an oceanic plate. In this instance the more dense oceanic plate subducts below the continental plate. This forms a deep sea trench similar to the oceanic plate’s convergence, close to the shoreline. Also volcanic mountain ranges may also develop further in from the shore due to rising magma and folding. Such ranges include the Andes Mountain Range (“Plate Tectonics”).
Diagram 5: showing oceanic to continental plate convergence and resulting features (Pidwirny, 2006)
So divergent plate margins are where crustal plates are moving apart from one another. These margins can either consist of two oceanic or two continental plates. Convergent plate margins on the other hand are where two plates are being pushed towards each other. The combination of plates at this margin can be either two continental, two oceanic or an oceanic to continental. Both of these margins play a major role in shaping the Earths topographical features. Some of which are similar while others different. Both aid in the formation of volcanoes however divergent rift volcanoes do not form cone while convergent andesitic volcanoes do. Both also show faulting however divergent plate margins have normal faults versus the reverse faults found at convergent margins. Deep sea trenches, volcanic islands and fold mountains are exclusive to convergent
This lab uses earthquake data to construct profiles of two convergent boundaries: the Tonga Trench and the Peru-Chile Trench. Where two tectonic plates converge, if one or both of the plates is an oceanic lithosphere, a subduction zone will form. When crust is formed at a mid-ocean ridge, it is hot and buoyant meaning it has a low density. As it spreads away from the ridge and cools and contracts, or becomes denser, it is able to sink into the hotter underlying mantle. When two oceanic plates collide, the younger of the two plates, because it is less dense will ride over the edge of the older plate. The density of the
There are three different types of plate boundaries. The first type of plate boundaries is, the spreading boundary. A spreading boundary is when two plates move apart. The spreading boundary is also known as a divergent boundary. The second type of plate boundary is a colliding boundary. A colliding boundary is when two plates come together, or collide. It is also known as convergent boundary. The third is, a sliding boundary. A sliding boundary is when two plates slip past each other moving in opposite directions. It is also known as transform boundary. Those were the three different types of plate
Be sure to consider topography/bathymetry as well as the earthquake and volcano layers. List several ways and be specific. 3pts In the middle between the two Without the plate boundary feature, you would still see the change in depth where the mountains are, still feel earthquakes, and see volcanic eruptions. Adapted from an activity by Laurel Goodell February 2013
But there are some anomalies as there are earthquakes which don’t take place on a plate boundary and it’s the same with volcanoes. An example of this is Hawaii. Hawaii is a volcanic island which is found in the middle of a tectonic plate. Hawaii is an example of a hotspot. The places known as hotspots are volcanic regions thought to be fed by underlying mantle that is anomalously hot compared with the mantle elsewhere. They may be on, near to, or far from tectonic plate boundaries. There are two hypotheses to explain them. One suggests that they are due to hot mantle plumes that rise from the core-mantle boundary. The other hypothesis postulates that it is not high
There are three distinct types of plate boundaries existing, which are supported by geological observation, geophysical data, and theoretical considerations. Their names and categories are based on if adjacent plates move apart from each other (divergent plate margins), toward one another (convergent plate margins), or slip past one another in a direction parallel to their common boundary (transform plate margins) (Pitman, W.C., 2007).
To support the theory of continental drift is through topography, surveying the floors of oceans, charts of rock magnetism, and statistics on rock ages (Trefil & Hazen, 2010). At one time scientist believed that the deep ocean floors were flat; accumulating the sediment that progressively wore away from the prehistoric landmasses (Trefil & Hazen, 2010). However, they discovered steep-walled valleys and elevated highlands. This was evidences that just as the continents are transformed and are active, so to is the seafloor (Trefil & Hazen, 2010). The Mid- Atlantic Ridge, positioned in the central part of the Atlantic Ocean, is recorded to be the longest mountain range on this planet. Volcanoes, lava flow, and earthquakes are a source of
Plate tectonics are very dangerous when they collide,slide,and move apart. They can create mountains like the Appalachian Mountains that used to tower over everything then erosion took place. The Appalachian Mountains were formed by convergent boundaries, convergent boundaries are collide
Plate tectonics is the scientific theory that attempts to explain the movements of the Earth's lithosphere that have formed the landscape features we see across the globe today” (Briney). Geology defines “plate” as a large slab of solid rock, and “tectonics” is part of the Greek root word for “to build.” Together the words define how the Earth’s surface is built up of moving plates. The theory of plate tectonics dictates that individual plates, broken down into large and small sections of rock, form Earth’s lithosphere. These fragmented bodies of rock move along each other atop the Earth’s liquid lower mantle to create the plate boundaries that have shaped Earth’s landscape. Plate tectonics originated from meteorologist Alfred Wegener’s theory, developed in the early 20th century. In 1912, he realized that the east coast of South America and the west coast of Africa appeared to piece together like a jigsaw puzzle. He further examined the globe and deduced that all of Earth’s continents could somehow be assembled together and proposed the idea that the continents had once been linked in a single supercontinent called Pangaea. To explain today’s position of the continents, Wegener theorized that they began to drift apart approximately 300 million years ago. This theory
and relationships of a working model. If a testable hypothesis is confirmed by a large
Earthquakes, volcanoes, mountains and the Earth’s crust are unique yet have one common denominator; the amazing topic of plate tectonics. Plate tectonics has a place or specifically places a role in each of these natural wonders of the world. In the following, Team C will discuss the theory of plate tectonics and how the theory shaped the form and composition of the movement within the Midwest region of the United States. A discussion of various geological events and the types of rocks that formed because of these events will also be covered including the importance of the economic value of these rocks to the Midwest region
Obduction - Where the Continental Plate runs under the Oceanic Plate causing oceanic ridges to form.
•Describe the relationship, if any, of the boundaries in #1 to the islands that you labeled in #3 Most divergent boundaries are under water. Normally forming submarine called oceanic spreading ridges. Iceland is an exception of this phenomenon since it emerges over the surface unlike other islands submerged deep in the water.
Plate Tectonics Theories Analysis Since the beginning of human kind there has been a cloud of wonder regarding the natural processes and patterns of our planet. Scientist interested in this field through out the years, have developed many different theories to how our planet geological features have come about. The most widely accepted theory in this field is that of plate tectonics. For those who do not know much about the theory of plate tectonics; it states that there are twenty plates that cover most of the Earth's surface area.
The viscosity of this base is a function of the temperature. The study of shifting continental plates is called Plate Tectonics. Plate Tectonics allows scientists to locate regions of geothermal heat emission. Shifting continental plates cause weak spots or gaps between plates where geothermal heat is more likely to seep through the crust. These gaps are called Subduction Zones.
Divergent: This happens when plates are forced apart, this is common on ocean floors as it creates deep sea trenches. It can also cause canyons.