Geology of the Moon, Mercury, and Mars

Slides:



Advertisements
Similar presentations
Chapter 6 The Earth and Moon. Distance between Earth and Moon has been measured to accuracy of a few centimeters using lasers (at McDonald Observatory)
Advertisements

© 2010 Pearson Education, Inc. Our Moon and other moons of the Solar System.
25.1 ORIGIN AND PROPERTIES OF THE MOON
Mars Astronomy 311 Professor Lee Carkner Lecture 14.
April 4, 2006Astronomy Chapter 8 Cratered Worlds: The Moon and Mercury The Moon is an object of lore and superstition. The Moon is our nearest neighbor,
Mars Astronomy 311 Professor Lee Carkner Lecture 14.
Mars Astronomy 311 Professor Lee Carkner Lecture 14.
8 February 2005AST 2010: Chapter 8 1 The Moon & Mercury.
13 July 2005AST 2010: Chapter 8 1 The Moon & Mercury.
Mars. Some similarities between Mars & Earth Mars’ Bulk Properties Mars has days & seasons like Earth.
25.1 ORIGIN AND PROPERTIES OF THE MOON DAHS MR. SWEET
Cratered Worlds: The Moon & Mercury Chapter 7. The Moon Mass 1/80 of Earth’s mass Gravity 1/6 of Earth’s Atmosphere –no real atmosphere –few volatiles.
Inner Planetary Geology II
Universe Eighth Edition Universe Roger A. Freedman William J. Kaufmann III CHAPTER 10 Our Barren Moon CHAPTER 10 Our Barren Moon.
Chapter 7 Our Barren Moon Survey of Astronomy Astro1010-lee.com
The Moon. MOON FACTS Natural satellite of earth Gravity 1/6 of earth - WHY? No atmosphere - WHY? Temp. difference: 134 C to -170 C -WHY?
Section 1: Earth’s Moon Preview Key Ideas Exploring the Moon
Formation Maria vs. Highlands Maria is Latin for “seas”. These areas appear dark and have smooth relatively crater free surfaces. They represent the.
Unit 2 Lesson 4 The Terrestrial Planets Copyright © Houghton Mifflin Harcourt Publishing Company.
Chapter 6 Exploring Terrestrial Surface Processes and Atmospheres
Mars Mars is a dry dead world. There are no Martian transits.
Note that the following lectures include animations and PowerPoint effects such as fly-ins and transitions that require you to be in PowerPoint's Slide.
The Moon and Mercury: Airless Worlds Please take your assigned transmitter And swipe your student ID for attendance tracking.
The Moon Chapter 10. The Earth Moon System Primary Surface Features.
The Solar System a1 Mercury Sun Venus Earth Mars Asteroids Jupiter Saturn Uranus Neptune Other objects Observe our solar system Four inner planets.
 Satellite – an object that orbits a more massive object  Ex: The Moon  Ex: Moons of other planets  Many of the planets have satellites.
Mars The Red Plant Mars is the fourth planet from the sun and the second smallest planet in the solar system. Named after the Roman god of war, it is often.
Ch. 28 Sec. 2 The Moon. Reaching for the Moon  Soviet Union launched Sputnik I in 1957 –First step into understanding our space  1961, Soviet astronaut.
Earth’s Moon How did our Moon form? and What’s been happening since?
MARS. The Basics Mars is the fourth planet in our solar system Mars is 56 million km from the earth at its closest point in orbit Mars is million.
Earth’s Moon - Luna. Lunar surface features There are 5 basic surface features.
American Unmanned Mission: Surveyor ( )
MARS.
John Young from Apollo 16, April 1972 Lunar Geology.
Universe Tenth Edition Chapter 10 Our Barren Moon Roger Freedman Robert Geller William Kaufmann III.
Was there ever geological activity on the Moon or Mercury
© 2010 Pearson Education, Inc. Chapter 9 Planetary Geology (abridged): Earth and the Other Terrestrial Worlds.
Chapter 7 Our Barren Moon Survey of Astronomy Astro1010-lee.com
The Moon Researched and compiled by Mrs. Terri Reed 5 th Grade Brookhollow February 2005.
EARTH’S MOON.  Structure  3,476 km in diameter  1/18 the mass of the Earth  No air or liquid water  Temperature range: 100◦C to -120◦C (212◦F to.
EARLY HISTORY OF THE TERRESTRIAL PLANETS
Mars Mars is a dry dead world. There are no Martian transits.
Unit 2 Lesson 4 The Terrestrial Planets
(Lots of pretty pictures. No math.)
© 2017 Pearson Education, Inc.
The Moon “Jupiter! I did a song! You ain’t got one!” "Camembert?"
The Moon and its Surface
The Moon.
Connecting Planetary Interiors and Surfaces
Lecture 23.
Ch. 9 and 10: the other Terrestrial Planets
The Moon 28.2.
The Moon Chapter 10.
Section 1: Earth’s Moon Preview Key Ideas Exploring the Moon
Chapter 9 Planetary Geology: Earth and the Other Terrestrial Worlds
Section 1: Earth’s Moon Preview Key Ideas Exploring the Moon
The Inner Planets.
Notes The Moon.
Unit 3 Lesson 4 The Terrestrial Planets
Earth and The Terrestrial Worlds
Mercury was visited by the U. S. spacecraft Mariner 10 in 1974.
Section 2: The Moon The Moon, Earth’s nearest neighbor in space, is unique among the moons in our solar system. K What I Know W What I Want to Find Out.
Practice Quiz.
The Moon and Mercury: Airless Worlds
Rising Carbon Dioxide Levels
Section 1: Earth’s Moon.
Surface Rocks - There are basically two kinds of surface rock on the Moon.
The Moon – Earth’s Natural Satellite
Information of Mars Mars is the fourth planet from the Sun and is commonly referred to as the Red Planet. The rocks.
Stephen Eikenberry 21 Feb 2019 AST 2037
Presentation transcript:

Geology of the Moon, Mercury, and Mars

How the maria formed A very large impact fractures the crust and creates ringed mountains Structure is called an “impact basin” Low viscosity lava flows up through the cracks and fills the basin This happened after the period of late heavy bombardment, so there are relatively few craters in the maria

Mare Orientale is a textbook example of an impact basin Very little lava flooded Orientale because it happened late – it was probably the last large impact basin to form. (Compare to Mare Imbrium) Ringed mountains Flat mare (few craters) Mare Orientale

Interestingly, the far side of the Moon has no large maria The near-side has many large maria The crust is thicker on the far side, and so impacts are much less likely to fracture it down to molten material But why is it thicker there? We don’t know.

The Moon also has interesting features called “rilles” They’re all over, but we’re going to visit one here

This is “Hadley Rille” Mount Hadley Apollo 15 landing site

Here the Apollo 15 lunar rover is parked next to Hadley Rille 1200 ft deep in this area, ~ 80 miles long “Sinuous Rilles” are lava tubes that ran dry and collapsed, leaving a winding valley

On which side of the Moon is the crust the thickest? A) The far side B) The near side C) They are equally thick D) We have no way of knowing

On which side of the Moon are maria more prevalent? A) The far side B) The near side C) They are equally prevalent on both sides

The surface of the Moon is covered by loose, powdery material called regolith. It is the product of constant bombardment from micrometeorites. It has very different properties from the “soil” of Earth: Very dry and sharp edged Electrostatically charged, so it clings to everything

2 – 4 mm sample of lunar regolith NOTE the glass spherules

Microscopic regolith sample Note the sharp edges

Astronauts inside the lunar lander after an EVA were coated with it Gene Cernan, Apollo 17 This stuff gets into everything, and raises serious technical problems!

Mercury shows similar features, though no large maria Notice that in many areas, like this one, the impact craters are not as closely packed as in the lunar highlands But more so than in the lunar maria. This suggests that this area was covered by lava flows late in the heavy bombardment era

Lobate scarps on Mercury This is a form of tectonics we do not see on any other terrestrial planet

Rank these surfaces from oldest to youngest: B) 1, 3, 2 C) 2, 3, 1 D) 2, 1, 3 E) 3, 2, 1 1 3 2

Percival Lowell and Mars 1879 Giovanni Schiaparelli reported linear features on Mars He called them “canali”, Italian for “channels” 1895 Percival Lowell published maps of “canals” on Mars 1898 H. G. Wells War of the Worlds (Radio broadcast was 1938, Oct. 30) 1950 Ray Bradbury The Martian Chronicles 1965 NASA’s Mariner 4 spacecraft: No Martians

A current map of Mars Volcanism Tectonics

Valles Marineris

~85,000’ 29,029’ 33,500’

Evidence of water on Mars 1

Evidence of water on Mars 2 Mars rovers have found many examples of minerals that are known to form only in the presence of liquid water

Evidence of water on Mars 3 Here gypsum fills a crack in Martian rock. The gypsum was deposited by water flowing through the cracks in the rock.

Evidence of water on Mars … Evidence of recent (last million years or so) water erosion on a crater wall

Evidence that liquid water occasionally flows on today’s Mars Released in summer 2015… Evidence that liquid water occasionally flows on today’s Mars (just below the surface)

Recurring Slope Lineae (RSL) They darken and appear to flow down steep slopes during warm seasons, and then fade in cooler seasons. Scientists discovered hydrated salts in these lines. On Earth these salts are known to lower the freezing point of liquids to as low as -94º F The RSL are “likely a shallow subsurface flow, with enough water wicking to the surface to explain the darkening.”

Astro-Cash Cab! Jesse K. Emily Amanuel JC Katy

1) Matching: A) Regolith _____ B) Impact basin _____ C) Sinuous rille _____ 1) Collapsed lava tube 2) A large, ringed area indicating a very large impact event 3) Loose, powdery material on the lunar surface

2) Put these 3 things in age order, from youngest to oldest: The mare The crater The rille

3) What is this feature on the surface of Mercury called?

4) On which planet will you find the largest volcano in the solar system?