Spanish and portuguese influence on latin america
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Christopher Columbus was sponsored by Spain to find a quick trade route to Asia but landed in the Americas instead in 1492, claiming the land for Spain. Spain then explored, conquered, and settled parts of Central and South America and the Caribbean. Portugal claimed land in South America along the Atlantic coast up to the Andes Mountains, including most of the Amazon River region which is now Brazil. Both countries spread their culture, religion, and languages across Latin America, developing colonies similar to those in Europe and forcing the native people to convert to Catholicism.
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Spanish colonization spread across Florida, Mexico, Central and South America in the 15th-16th centuries, establishing colonies and converting native populations to Catholicism. Portugal claimed land in South America from the Atlantic to the Andes, including most of the Amazon, establishing Brazil. Both powers diffused their languages and culture throughout Latin America, leading the region to be known today for its shared Latin-derived languages of Spanish and Portuguese.
Culture spanishand portugueseinfluenceonlatinamerica
Christopher Columbus landed in the Americas in 1492 while sailing under sponsorship from Spain, claiming the land for Spain. Spain then explored, conquered, and settled much of Central and South America and the Caribbean, spreading the Spanish language. Portugal claimed land in South America from the Atlantic to the Andes Mountains, including most of present-day Brazil, spreading the Portuguese language. The Spanish and Portuguese colonized the region, forcing native peoples to adopt their culture, religion, and languages of Spanish and Portuguese.
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Spanish and Portuguese Influence on Latin America powerpoint
Christopher Columbus was sponsored by Spain to find a quick trade route to Asia, but instead landed in the Americas in 1492 and claimed the land for Spain. Spain then explored, conquered, and settled areas across Florida, Mexico, Central and South America, and the Caribbean islands, establishing Spanish as the dominant language. Portugal also established colonies along the coast of South America and in Brazil, where Portuguese became the primary language. Together, the Spanish and Portuguese colonies shaped Latin America through spreading their cultures, languages, and Roman Catholic religion across the conquered lands.
Influence on latin america
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1) Between 1400-1700, Portugal and Spain led European global exploration and established vast overseas empires, with Portugal's empire centered in Africa, India, and the Atlantic and Spain's focused on the Americas.
2) Portugal's empire was built on sea trade, establishing commercial outposts along African and Asian coasts and connecting Europe, Africa, and Asia. Spain conquered large swaths of South and Central America and the Caribbean.
3) The Columbian Exchange following the voyages of Columbus resulted in the widespread transfer of plants, animals, diseases, and people between the Old World and the New, with devastating population losses in the Americas due to introduced diseases.
Spanish colonisers spoke and heard different languages than did Dutc.pdf
Spanish colonisers spoke and heard different languages than did Dutch, English and French
colonisers in the North America NORTHEAST(New England). Spanish colonisers brought
Romania Catholicism to the indigenous population. Both protestant, Anglican and Catholic
established presence in the northeast. Spanish came largely to pillage and remove natural wealth.
In the northeast colonists were more motivated by establishing industry and trading with
homelands. Spanish colonisers tended to be dictatorial and northeast colonies tended towards
democracy.
Solution
Spanish colonisers spoke and heard different languages than did Dutch, English and French
colonisers in the North America NORTHEAST(New England). Spanish colonisers brought
Romania Catholicism to the indigenous population. Both protestant, Anglican and Catholic
established presence in the northeast. Spanish came largely to pillage and remove natural wealth.
In the northeast colonists were more motivated by establishing industry and trading with
homelands. Spanish colonisers tended to be dictatorial and northeast colonies tended towards
democracy..
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Seismic waves
Deep underground, rocks are under constant pressure until the strain becomes too great and the rocks suddenly break, releasing seismic waves. These waves travel outward from the hypocenter in three types - P waves which push and pull, S waves which move sides to side, and L waves which cause surfaces to bob up and down. When recorded by a seismograph, the first indication of an earthquake is typically the P waves, followed by larger S waves, with surface L waves arriving last.
Earthquakes
An earthquake is caused by the sudden movement of parts of the Earth's crust and results in shaking and trembling of the ground. There are over one million earthquakes each year, with around twenty having the potential to cause severe damage. Earthquakes are caused by faults in the Earth's crust, such as the San Andreas Fault in California where the land west of the fault moves north and the land east moves south. Underwater earthquakes can generate destructive tsunamis. The focus is the depth below the surface where the earthquake occurs, and the epicenter is directly above on the surface. Seismographs detect seismic waves that travel out from the epicenter, including fast P waves and slower S waves.
Deformation
The video discusses the different forces that act on the earth's crust and how they cause deformation through various mechanisms. Compression causes squeezing and increases density, tension causes pulling and decreases density, and shearing causes twisting. These forces result in fracturing, faulting, and folding of rocks in the crust. Fractures are cracks, faults are cracks with lateral movement, and folds are bends in rock layers. Anticlines are upward folds and synclines are downward folds. Various factors like temperature, pressure, rock type, and rate of force application determine whether rocks fault or fold when subjected to deformation.
European governments
The document summarizes the government and political systems of the United Kingdom, Germany, and Russia. It describes that the UK has a Parliament with two houses, the House of Commons and House of Lords, and citizens elect members of Commons while Lords are inherited titles. Germany is a federal republic with a Chancellor as head of government and largely ceremonial President. Russia transitioned to a federal republic after the Soviet fall, with a dominant presidential system and a two-chamber Parliament.
Plate tectonics review #2
The document discusses different types of plate boundaries, including divergent boundaries where plates move apart, such as at mid-ocean ridges which form undersea mountain ranges as oceanic crust spreads away from the ridge. It also describes transform boundaries where plates slide past each other in opposite directions, such as at the San Andreas Fault in California.
Plate tectonics review
The plates are moving at a very slow rate of between one to ten centimeters per year. In some areas plates are moving together through a process called convergence, while in other areas they are moving apart. There are three main types of convergent boundaries: continental-continental, continental-oceanic, and oceanic-oceanic. At convergent boundaries, one plate dives beneath the other through subduction, which can cause volcanic activity at the surface.
Plate tectonics
The document discusses the theory of plate tectonics. It explains that the Earth's lithosphere is broken into plates that move slowly over time due to convection currents in the mantle. There are three types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where they move together, and transform boundaries where plates slip past each other.
Systems of government powerpoint (unitary, confederation, federal)updated 2010
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This document discusses different systems of government and how power is distributed in each. It begins by asking the reader to identify the different levels of government where they live. It then explains that governments are organized to protect citizens and manage conflict. There are different types of governments like democracies, republics, and monarchies. Geographers study the types of governments and how power is distributed through systems. The main systems are unitary, confederation, and federal. Unitary governments have one central power. Confederation governments give some power to members. Federal governments share power between a central and state/provincial governments. Diagrams and country examples are provided to illustrate each system.Continental drift
Alfred Wegener first proposed the theory of continental drift, which suggested that the continents were once joined together in a super continent called Pangaea before drifting apart to their current locations. Wegener's theory was initially rejected because he could not explain the driving force behind continental movement. Evidence that later emerged in support of continental drift includes: matching fossil and rock formations between continents, matching climate zones in pole and equatorial regions, and magnetic pole reversal patterns in ocean floor sediments. This evidence helped prove that continents have shifted positions over time.
Sea floor spreading
1) The Mid-Ocean Ridge system circles the Earth along the ocean floor and is over 56,000 km long. It forms at divergent plate boundaries where new oceanic crust is continually being formed.
2) Scientists use sonar to map the ocean floor and study its features like the Mid-Ocean Ridge. Sonar bounces sound waves off underwater objects to image the seafloor.
3) Evidence like magnetic stripes in ocean crust and samples dug from the seafloor support the theory of sea floor spreading, where new crust forms at ridges and spreads out over time.
Earths structure
The document discusses the four main layers of the Earth - the crust, mantle, outer core, and inner core. It explains that the crust is the outermost layer and includes both continental and oceanic crust, with oceanic crust being denser. The mantle is below the crust and contains hot, dense rock. The outer core is a liquid layer surrounding the solid inner core, where extreme pressure causes iron and nickel atoms to remain solid.
Geologic time magazine
This document outlines the requirements for a group project where students work with a partner to create a magazine. Each person must complete two 20 point activities and one 10 point activity by certain checkpoint dates. They must also turn in their completed magazine by October 15th, which can include different formats like articles, interviews, or political cartoons, but each format can only be used once and one activity must use a longer writing format.
Geological time scale
The document summarizes the geologic time scale, which is divided into eras, periods, and epochs based on fossil evidence showing changes in Earth's organisms over its 4.56 billion year history. The largest divisions are eras, including Precambrian, Paleozoic, Mesozoic, and current Cenozoic. Each era is characterized by the dominant lifeforms and events of that time period. The geologic time scale helps break up Earth's history into more manageable chunks for study.
Fossils
Fossils are the remains or traces of prehistoric life found in sedimentary rocks. The type of fossil formed depends on how and where the organism died and was buried. Fossils can be unaltered remains like teeth and shells, or altered remains that have changed over time through processes like petrification or carbonization. Trace fossils provide indirect evidence of prehistoric life through things like tracks, burrows, and coprolites. Fossils are important for interpreting ancient environments and changes over time.
Relative and absolute dating
The document discusses methods for dating geological materials and events. Relative dating methods, like the law of superposition and index fossils, are used to determine the sequence of events but not calculate specific ages. Absolute dating methods, such as radiocarbon dating, are used to determine specific numerical ages by measuring radioactive decay. Radiocarbon dating works by comparing the ratio of carbon-14 to carbon-12 in once-living materials, as carbon-14 decays at a known rate. Together, relative and absolute dating methods provide information about the timing of geological events and processes.
Paleontology and uniformitariansm
Paleontology is the study of past life through the examination of plant and animal fossils. Paleontologists study fossils and the environments they formed in to piece together details about past ecosystems. The principle of uniformitarianism, first developed by James Hutton in 1788, holds that the same geological processes shaping Earth today have operated throughout its history. This theory helped establish that Earth is much older than previously believed. Relative dating methods like the law of superposition and use of index fossils allow paleontologists to determine the sequential order of geological events and changing life forms without knowing exact time periods.
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