what can be formed are mountain ranges called oceanic spreading ridges. While the process volcanic, volcanoes, and earthquakes are not as violent as a convergent
Pacific Northwest - <em>Northern part of this peninsula
</em>
Midwest - <em>Includes area around the American
</em>
Baja California - <em>Warm, humid, growing
</em>
South - <em>Vast forests and active
</em>
Further Explanation
The state is a first-level administrative territory of a federal or union state. In most cases, these areas of the state are formed by the federal or central government.
- Pacific Northwest - the geographical area in western North America, the Pacific Ocean borders to the west and the Rocky Mountains to the east.
- Midwest / Midwestern America is one of the four geographic regions defined by the United States Census Bureau, which covers the central north of the United States.
- Baja California is a state in Western Mexico.
- South America is a continent located between the Pacific Ocean and the Atlantic Ocean that is connected to North America via the Panhandle of Panama. This continent is crossed by the equator, and most of the continent's plains are in the southern hemisphere.
Countries in South America:
- <em>Argentina
</em>
- <em>Bolivia
</em>
- <em>Brazil
</em>
- <em>Chile
</em>
- <em>Colombia
</em>
- <em>Ecuador
</em>
- <em>Falkland Islands
</em>
- <em>French Guiana
</em>
- <em>Guyana
</em>
- <em>Paraguay
</em>
- <em>Peruvian
</em>
- <em>South Georgia and the South Sandwich Islands
</em>
- <em>Suriname
</em>
- <em>Trinidad and Tobago
</em>
- <em>Uruguay
</em>
- <em>Venezuela
</em>
<em />
Learn more:
<em>Countries in South America</em> : brainly.com/question/2535146
Details
Grade: high school
Subject: Geography
keyword : The state, Midwestern, South America
Answer:
Subsidence is so slow that there seems to have been no depression of the upper surface of the lithosphere, so depositional environments are mostly the
same as those in surrounding areas; the succession is just thicker. These
successions are also more complete, however—there are fewer and smaller
diastems—so at times the basin must have remained under water while surrounding areas were emergent. (A diastem is a brief interruption in
sedimentation, with little or no erosion before sedimentation resumes.)
Size, shape: rounded, equidimensional, hundreds of kilometers across
Sediment fill: shallow-water cratonal sediments (carbonates, shales, sandstones),
thicker and more complete than in adjacent areas of the craton but still
relatively thin, hundreds of meters.
Hopefully that helps!
