The name for all the sciences that collectively seek to understand Earth and its neighbors in space, including geology, oceanography, meteorology, and astronomy
The Earth is older than previously thought
300 years ago, geologists thought the Earth was about 6,000 years old
Later, geologists discovered rocks that were formed 40 million years ago
Today, scientists claim the Earth is between 4 and 5 billion years old
How scientists determined the Earth's age
1. Study of rocks
2. Measuring changes in rocks over time
3. Studying the order of rock layers (Law of Superposition)
4. Radioactive dating
Law of Superposition
In undisturbed sedimentary rocks, each layer is younger than the layer below it and older than the layer above it
Igneous rocks and volcanic rocks make it more difficult to determine the age of rocks
Radioactive dating
A reliable method to tell the Earth's age by measuring the amounts of radioactive elements and their decay products in rock samples
Some rocks have been found to be 5 billion years old using radioactive dating
Fossils
Hardened remains or imprints of organisms that lived a very long time ago
Fossils
They provide records of the past, including when glaciers or seas covered the land, when volcanoes erupted, when mountains were pushed up, and the kinds of living things that existed millions of years ago
Types of fossils
Footprints
Impressions in hardened materials like cement
Petrified or changed into rock
Whole bodies or skeletons preserved in materials like ice and amber
Fossils reveal the sizes, shapes, appearances, habits, and habitats of living things from long ago
Geologic time scale
The division of the story of living creatures into eras, periods, and epochs based on the dominant life forms that existed
Geologic eras
Precambrian
Paleozoic
Mesozoic
Cenozoic
Precambrian era
Lasted from the beginning of the Earth to about 600 million years ago
Primitive organisms existed but left few fossils
Mostly igneous and metamorphic rocks
Paleozoic era
Many marine invertebrate fossils found
First animals adapted to breathe air and land plants developed
Reptiles appeared towards the end
Mesozoic era
Continents formed and drifted apart
Dinosaurs were the dominant life forms
Reptiles survived while dinosaurs died out
Cenozoic era
Warm-blooded animals like mammals and birds appeared
Glaciation occurred in the Northern Hemisphere
Earliest human records like stone tools
The Earth is not a perfect sphere due to its equatorial bulge and irregular surface with mountains and valleys
Oblate spheroid
The geometric form closest to the actual contours of the Earth, as computed by J.P. Hayford in 1910
How Eratosthenes measured the Earth's circumference
1. Measured the angle of the sun's rays at two locations 800 km apart
2. Calculated the circumference based on the angle difference
Eratosthenes' calculation of the Earth's circumference was within a few hundred kilometers of the modern value
Latitude
Lines drawn east-west around the Earth, measured from 0° at the equator to 90° at the poles
Longitude
Lines drawn north-south from pole to pole, with the prime meridian at 0° passing through Greenwich, England
The International Date Line is at 180° longitude, directly opposite the prime meridian
Map scale
Enables determining the distance between places on a map compared to the actual distance on Earth's surface
Globes are spherical models of the Earth that show the sizes, shapes, and locations of continents and bodies of water
International Date Line
Line where east and west longitude lines meet at 180° meridian. If you cross this line going west, you add one day.
The International Date Line is directly opposite Greenwich on the other side of the Earth
West longitude
Points west of the prime meridian
East longitude
Points east of the prime meridian
Map
A drawing of the earth, or part of the earth on a flat surface
Globe
A spherical model of the Earth that shows the sizes, shapes, and locations of all continents and bodies of water
Map scale
Enables us to tell the distance between places on a map and compare it to actual distance on Earth's surface
Map features
Roads, rivers, national parks, national highways
Map symbols
Drawings that stand for real places or things, explained in the map legend
Topographic map
Shows roads, cities, mountains, hills, and rivers using contour lines to show relief