Lab exercise: Ice geology on the Galilean satellites
G456/556    66 points

Name________________________
 

Equipment Needed: Internet connection to class website and web browser; image software to open and measure lengths on images in units of pixels (Photoshop or Arcview); calculator.

Objective: You will learn about the geology of Europa, Ganymede, and Callisto and infer geological histories for representative areas on these satellites.

Return to G456/556 homepage.

To make measurements on images, open the images corresponding to the figures using image software, preferably Photoshop, or ArcView.  For information on how to use Photoshop to make measurements, follow these instructions as illustrated for the Io lab.  You will need to download the following images to a temporary folder before opening them: galilean-Fig1.tifgalilean-Fig2.tif,  galilean-Fig3.tif.



Introduction. The three outer Galilean satellites of Jupiter are named after the Italian scientist-inventor Galileo, who discovered them when he pointed his telescope at the Planet. Ganymede and Callisto are ice-rich worlds larger than the planet Mercury and may have subsurface water oceans; Europa is about the size of the Earth's moon and has an icy crust, a probable subsurface water ocean, and a rocky (silicate) interior. The Voyager spacecraft gave us our first close look at these moons in the late 1970s, and more recently, the Galileo orbiter provided even closer views of these intriguing worlds.
 

Figure 1 shows representative Galileo spacecraft images of Europa, Ganymede, and Callisto to the same scale. The three moons all have surfaces rich in water ice, but very different geology. This probably reflects differences in their internal structure.
 
Fig.1. Images of Europa, Ganymede and Callisto to the same scale. Each image covers an area of 6600 km2. Sunlight is coming from the right (the sun is to the right). 

Link to Fig. 1
 

1. What is the scale of Fig. 1?  [1 point]
 

Scale = __________________ km/pixel  (report to 2 significant digits)



Part I-- Europa craters and ridges.
 

2. Feature A in Fig. 1 is a sharp-rimmed, bowl-shaped impact crater. What is the total number of similar impact craters identifiable in the Europa image in Fig. 1? [1 point]
 

Total number of craters_______________________
 

3. The number of impact craters per unit area (the crater density) on a planetary surface is a rough measure of the age of the surface; an older surface has a higher crater density. Using your result from question 2, what is the approximate crater density on Europa? [2 points]
 

Crater density on Europa________________________ craters/km2 (report to 2 significant digits)
 

4. The crater density on Venus is about 2.1 x 10-6 craters/km2, and that on Earth's continents is about 2.2 x 10-6 craters/km2. How many times higher or lower is the crater density on Europa compared to that of Venus and the Earth? Round your answer to 1 significant digit. [2 points]
 
 
 
 
 

5. In order to convert crater density to an actual age, we need to be able to estimate the number of impacting bodies per unit time that collided with the surface. This number of impacting bodies could vary from place to place within the solar system, depending on the nature and source of the impacting bodies (they could be asteroids, comets, or other debris swept up by the planets).  Do you think it is meaningful to calculate an age for Europa's surface based on simple crater density comparisons with Venus and Earth?  Provide two reasons to justify your answer.  [2 points]
 
 
 
 
 

6. The icy crust of Europa has many intersecting ridges. Most have valleys running down their centers (ridges with medial valleys). A typical example is given by feature B in Fig. 1. How wide is ridge B (from edge-to-edge)? [1 point]
 

Width of ridge B = _____________________ km (2 significant digits)
 

7. Ridges on Europa sometimes occur in groups of closely-spaced, parallel ridges (e.g., feature C in Fig. 1). Look closely at the cross-cutting relationships between features B and C. Which do you think (ridge B or the band of ridges centered on C) formed later, and why? [2 points]
 
 
 
 
 

8. Note that ridge B intersects on both ends a different type of landform on Europa (feature D in Fig. 1), characterized by a bumpy or hummocky surface topography. Which unit (B or D) is younger, and how can you tell? [2 points]
 
 
 
 
 

9. Look carefully at the pattern of ridges surrounding unit D in Fig. 1. Based on this pattern, is there any evidence for horizontal displacement of ridges across unit D? [1 point]
 
 
 
 



Part II-- Ganymede's craters and grooves.
 

Link to Fig. 1
 

10. Impact craters are present on Ganymede (e.g., feature E in Fig. 1). Estimate how the crater density on Ganymede compares with that of Europa, by saying whether it is about the same (within a factor of three) as Europa, significantly less than Europa, or significantly more than Europa. [1 point]
 

Crater density on Ganymede____________________________________
 

11. Ganymede contains both relatively smooth plains (feature F in Fig. 1), as well as a rougher terrain that has been tectonically deformed, which has many ridges and valleys- so-called "grooved terrain" (feature G). Based on cross-cutting relationships, can you tell which terrain (F or G) is older, and if so, which one? [1 point]
 
 
 
 
 

12. Which unit (F or G in Fig. 1) appears to have a higher crater density, and does this observation seem to support or refute the relative age determination you made in question 11? [2 points]
 
 
 
 
 

13. Two larger circular features (feature H and a smaller one immediately to the lower left of H in Fig. 1) occur in an area that has many fractures. Are these circular features depressions or elevations, and what do you think they represent? [2 points]
 
 
 
 
 

14. Based on the subdued and almost unrecognizable appearance of feature H, do you think that this feature would be visible if it had experienced tectonic deformation of the sort that occurred around the letter "G" in Fig. 1? [1 point]
 
 
 
 
 

15. Does your answer to question 14 resolve the relative ages of units F and G? Explain. [2 points]
 
 
 
 
 
 



Part III-- Callisto's craters and hills.
 

Link to Fig. 1
 

16. Voyager spacecraft images of Callisto led to the description of Callisto being "the most heavily cratered surface in the solar system". A more accurate description is that Callisto is one of the most uniformly cratered places in the solar system; the crater density doesn't vary much from place to place. Higher resolution images of Callisto obtained by the Galileo orbiter (Fig. 1) show small and medium-sized craters (e.g., feature I). Looking at Fig. 1, estimate how the crater density on Callisto compares with that of Europa and Ganymede, by saying whether it is about the same (within a factor of 3) as Europa and Ganymede, significantly less, or significantly more than Europa and Ganymede. [2 points]
 

Crater density on Callisto compared to Europa______________________________________
 

Crater density on Callisto compared to Ganymede___________________________________
 

17. Considering your answer to question 5, do you think it is meaningful to determine relative ages of surfaces on the Galilean satellites by simple comparison of their crater densities?  Why or why not?  [2 points]
 
 
 
 
 

18. Based on your answers to questions 16-17, do you think that Europa, Ganymede, or Callisto has the youngest surface on average? Which has the oldest surface on average? If you can't tell for sure based on Fig. 1, indicate this. [2 points]
 

The youngest surface of the three________________________________________________
 

The oldest surface of the three__________________________________________________

19. Callisto also has many hills (feature J). Based on your knowledge of the sun direction, how would you describe the landscape in region K? [1 point]
 
 
 
 
 

20. If the features labeled J are hills, what is feature L? HINT: look at the lengths of the shadows. [1 point]
 
 
 
 
 

21. Is there any evidence for tectonic deformation (producing ridges and valleys) on Callisto as there is for Ganymede? [1 point]
 
 
 
 
 

22. Speculate as to the origin of the numerous hills on Callisto. HINT: Look around feature I. [2 points]
 
 
 
 
 

23. Based on your answers to questions 18-22, summarize the geologic history of this portion of Callisto. Be sure to discuss the relative ages of craters and hills and the relationship between them. [3 points]
 
 
 
 
 
 



Part IV-- Europa "chaos" region.
 

Figure 2 shows an image of Europa obtained by the Galileo orbiter that provides some of the most compelling evidence that large amounts of liquid water were present on Europa's surface recently.
 
 
Fig. 2. This area of so-called "chaos" terrain on Europa shows plate-like features (e.g., feature A) that contain ridges and valleys, and a bumpy or hummocky terrain (e.g., at B) that appears to enclose, and to be lower than, the plates. In some areas (e.g., at C), obvious examples of horizontal displacement can be seen between adjacent plates. Sunlight is coming from the 12:30 position.

 

Link to Fig. 2
 

24. What is the scale of Fig. 2? [1 point]   Scale of Fig. 2 = __________________ km/pixel (2 significant digits)
 

25. What is the maximum length of plate A? [1 point]
 

Length of A = ________________________ km (2 significant digits)
 

26. How much horizontal displacement occurred between adjacent plates at C? [1 point]
 

Displacement at C = ______________________ km (2 significant digits)
 

27. Which of the two major terrain types, plates or hummocky terrain, do you think is older and why? [2 points]
 
 
 
 
 

28. Based on the appearance of the plates and hummocky terrain and the evidence for horizontal displacement of the plates, what do you think the plates represent?  Think of one word. [1 point]
 
 
 
 
 

29. Considering your answer to question 28, what does the hummocky terrain represent? [1 point]
 
 
 
 
 

30. How many sharp-rimmed, bowl-shaped impact craters do you see in Fig. 2? [1 point]
 

Number of craters____________________
 

31. Do these craters seem to occur mainly on the hummocky terrain, or on the plates? [1 point]
 
 
 
 
 

32. Is your answer to question 31 consistent or inconsistent with your answer to question 27? [1 point]
 
 
 
 
 

33. Feature D in Fig. 2 is a canyon that extends across most of the image, from the upper right to the lower left. Based on cross-cutting relationships, is canyon D a younger or older feature compared to the plates and hummocky terrain? [2 points]
 

Age of D compared to plates_______________________________
 

Age of D compared to hummocky terrain___________________________
 

34. Based on your answers to questions 27-33 and superposition relations, summarize the geologic history of this portion of Europa (Fig. 2) by creating a stratigraphic timeline, placing older features at the bottom and younger at the top. If relative ages are uncertain, indicate this by placing features at the same vertical position. In your stratigraphic sequence include the following: plates, hummocky terrain, ridges on the plates, canyon D, impact craters. [4 points]
 
 
 
 
 
 
 
 



Part V -- Ganymede terrain types.
 

Among the Galilean moons, the one that shows the most diversity of ages on its surface is Ganymede. Europa contains a few impact craters but no heavily cratered areas; and Callisto has a fairly uniform crater density. (Io, the fourth Galilean moon, has no impact craters at all.) Ganymede has both heavily cratered portions and areas with few impact craters. Figure 3 shows a regional view of Ganymede that illustrates the major terrain types and their relationships on this planet-sized moon.

Terrain types in Fig. 3:

A =  heavily cratered area

B, C, D, E = light-colored, smooth plains

F, G, H, I  = light-colored, "grooved" terrain, consisting of parallel ridges and valleys
 
 
Fig. 3 Image of Ganymede illustrating terrain types. Sunlight is coming from the 3:30 direction. 

Link to Fig. 3
 

35. Area A in Fig. 3 is the most heavily cratered, and it is cut by all other units, indicating that it is the oldest unit. Based on crater density, are the smooth plains (B, C, D, E) generally older or younger than the grooved terrain (F, G, H, I)? [1 point]
 
 
 
 
 

36. Note that the grooved terrain at feature I in Fig. 3 appears to merge into the smooth plains at E, and that the grooved terrain in feature H appears to merge into smooth plains at C. Assuming that the grooved terrain contains faults along which water could have moved to the surface, how could units E and C have formed? [3 points]
 
 
 
 
 

37. Looking especially at the narrowness of feature E in Fig. 3, do you think that any water erupting to the surface to form the smooth plains flowed freely across the surface, or was it confined to localized areas only? [1 point]
 
 
 
 
 

38. Considering your answers to questions 37 and 29, which moon, Europa or Ganymede, is more likely to have had large bodies of spatially extensive, and relatively deep liquid water on the surface? [1 point]
 
 
 
 
 

39. Considering your asnwers to questions 38 and 18, which moon, Europa or Ganymede, experienced more internal heating? [1 point]
 
 
 
 
 

40. On Ganymede, impact craters in grooved terrain or smooth plains often show high-albedo ejecta (J and K), whereas bright ejecta never occurs around craters in the cratered terrain. Assuming that the crust of Ganymede consists of bright water ice + darker non-ice components, what does this imply about the composition of crust below the surface in heavily cratered terrain, grooved terrain, and the smooth plains? [3 points]
 
 
 
 
 

41. Using superposition relationships and your answers to questions 35-38, construct a stratigraphic timeline for the formation of features A-K in Fig. 3, placing older features towards the bottom and younger features towards at the top. If age relationships are uncertain, indicate this by placing features at the same vertical position. [3 points]