Exam 12: Volcanic and Tectonic Landforms

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Where strata have been tightly folded and altered during continental collisions,a landscape with a series of ridges results.These are known as:

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Using examples from your region or a well-known case study,explain the erosional changes evident in a volcano

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In my region, one well-known case study of erosional changes evident in a volcano is the Mount St. Helens eruption in 1980. This eruption caused significant erosional changes to the landscape surrounding the volcano.

The eruption of Mount St. Helens resulted in the collapse of the north face of the volcano, triggering a massive landslide and the release of a pyroclastic flow. This event drastically altered the topography of the area, creating a large crater at the summit and depositing huge amounts of volcanic debris and ash across the surrounding landscape.

The erosional changes caused by the eruption were further exacerbated by subsequent lahars, or volcanic mudflows, which were triggered by melting snow and ice on the mountain. These lahars carved deep channels and canyons into the terrain as they flowed downhill, carrying with them sediment and debris.

Over time, the erosional changes brought about by the Mount St. Helens eruption have resulted in the formation of new valleys, canyons, and gorges in the area. The once lush forests were decimated, and the landscape was transformed into a barren, moonscape-like environment.

In conclusion, the Mount St. Helens eruption serves as a prime example of the erosional changes evident in a volcano. The catastrophic event not only reshaped the physical features of the region but also had a lasting impact on the ecosystem and environment.

Using annotated diagrams compare and contrast the different types of volcano

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There are three main types of volcanoes: shield volcanoes, stratovolcanoes (or composite volcanoes), and cinder cone volcanoes. Each type has distinct characteristics that can be compared and contrasted using annotated diagrams.

Shield volcanoes are characterized by their broad, gently sloping sides and large, flat summit. They are formed by the eruption of low-viscosity lava, which flows easily and can travel long distances from the vent. This results in the gradual buildup of layers of lava, creating the shield shape. Annotated diagrams of shield volcanoes would show their low-angle slopes and wide base, as well as the layers of lava flows that form the structure.

Stratovolcanoes, on the other hand, have steeper sides and a more conical shape. They are formed by alternating layers of lava, ash, and volcanic rocks, which result in their characteristic steep profile. Annotated diagrams of stratovolcanoes would illustrate the layers of different materials, as well as the presence of a central vent and crater at the summit.

Cinder cone volcanoes are the smallest and simplest type, with steep sides and a bowl-shaped crater at the summit. They are formed by the eruption of pyroclastic material, such as ash, cinders, and volcanic bombs, which accumulate around the vent. Annotated diagrams of cinder cone volcanoes would show the steep sides and the accumulation of pyroclastic material around the central vent.

When comparing and contrasting these types of volcanoes, annotated diagrams can highlight their differences in size, shape, and eruption style. They can also illustrate how each type is formed by different types of volcanic activity and materials. By using annotated diagrams, it becomes easier to visualize and understand the distinct characteristics of shield, stratovolcanoes, and cinder cone volcanoes.

The San Andreas fault is a major normal fault with the potential for severe earthquakes.

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A table-topped plateau of comparatively small extent bounded by cliffs and occurring in a region of flat-lying strata is referred to as a:

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The compass direction of the line of intersection of an inclined rock plane and a horizontal plane of reference is referred to as the:

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A steep cliff-like fault scarp is a common result of reverse faults.

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Lava associated with composite volcanoes is:

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Which of the following types of drainage pattern would be associated with a fully dissected coastal plain?

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Using examples from the Internet,show how remote sensing can contribute to our understanding of volcanoes.

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Compression leads to the folding of the crust which results in the formation of __________________.

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Using an annotated diagram,describe the development of a broad coastal plain.

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Stratovolcanoes produce lava flows that initially follow valleys but are highly resistant to erosion.

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Describe the faulting associated with the Great African Rift Valley

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Compare and contrast the erosion of stratovolcanoes compared to shield volcanoes.

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The streams carving up a landmass are controlled to a high degree by the structure of the rock on which they act.

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Earthquakes can occur in locations far from plate boundaries.

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The chain of Hawaiian volcanoes were created by the motion of the ________ plate over a __________.

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The erosion of shield volcano would result in all of the following except:

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Which of the following statements about reverse faults is correct?

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