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Geology of the Solar System I Continuous Assessment: Moon Practical

Assignment Brief

Geology of the Solar System I Continuous Assessment: Moon Practical

INTRODUCTION

Continuous assessment of this module will be based on a practical activity (occupying three evenings plus homework as appropriate), which will account for 15% of the value of the module (the remaining 85% will be based on the final exam). This practical activity is based on interpreting a Lunar Orbiter image of the lunar surface. The area chosen (13°N, 4°E) lies between Mare Imbrium and Mare Serenitatis, and includes Hadley Rille and the Apollo 15 landing site (Fig. 1).

GENERAL INSTRUCTIONS

(a) Printing the images: The original, rather large, Lunar Orbiter image has been divided into four parts, but only three of these will be used for this practical. High-resolution versions of these three images (labelled Practical_image_1 to Practical_image_3) are located in the same Moodle folder as these notes. Each image has north at the top and east at the right, and they are related to each other as shown in Figure 1 (with some overlap between images).

Print out all three images, ideally such that each one occupies a single sheet of A4 paper with north at the top. You will need these hardcopies to work from. If for any reason you are unable to print them out, please contact the lecturer. NB. You should work from the full resolution jpeg images provided on Moodle (or handed out in class), not the reduced versions shown in Fig. 1.

(b) Scale: Lunar Orbiter images are composed of many separate strips, which run approximately eastwest in the images. You may assume that the width of each of these strips corresponds to 11 km on the lunar surface. Use this information to determine the actual distance on the lunar surface in km corresponding to 1 cm on your printed images. You will be asked to specify this scale in the questions below. (1) Write down the scale (km per cm) that you determined for your images in part (b) above.

(c) Coordinates: In what follows, we will need to specify locations of lunar features on the images. To do this, we will adopt a coordinate system by measuring horizontal (west-east) and vertical (southnorth) distances (in cm) from the bottom left hand corner of each image (i.e. the south-west corner), and then converting these distances into km using the scale calculated above. We can then express the coordinates of a feature as a pair of numbers which give its distance (in km) east and north of the southwest corner of each image. We will express the horizontal distance first, followed by the vertical, as a pair of numbers in brackets; you need only give coordinates to the nearest km.

For example, using this coordinate system, the centre of the prominent crater near the south-east corner of Image 1 is located at approximately (118, 32). That is, 118 km from the left hand edge of the image, and 32 km from the bottom. Everyone should verify that they get this answer, and if not should contact the lecturer for guidance. If you have printed your own images, please ensure that the whole length and width of the image has been printed or you will get a different answer.

(d) Sun elevation: One other piece of information that we will need is that, as seen from the surface of the Moon, the Sun was 22° above the horizon when these images were obtained

QUESTIONS

Answer the following questions. Percentage marks for each question are given in square brackets

Part A: Orientation and feature identification

(1) Write down the scale (km per cm) that you determined for your images in part (b) above. [2]

(2) From the lunar surface, what is the approximate direction of the Sun (i.e. north, south, east, or west)? [2]

(3) When the photograph was taken, was it morning or afternoon on this part of the Moon? How do you know this? [3]

(4) Using the coordinate system described above, Apollo 15 landed at approximate coordinates (87 km, 100 km) in Image 1. What kind of surface did it land on? [2]

(5) Study all three images and, using the coordinate system described above, give positions for the following features (give one set of coordinates close to the centre of each feature, and remember to state which image you are referring to):

(a) A sinuous rille other than Hadley Rille [2] (b) A straight rille [2] (c) An arcuate rille [2] (d) An obvious non-lunar feature (i.e. a blemish on the photograph) [2] (e) A `simple` crater [2] (f) A crater on the boundary between being `simple` and `complex` [2] (g) A tall mountain [2] (h) An `island` of probable highland material protruding from a `sea` of mare basalt [2]

PART B: Heights of Lunar features

Using the trigonometrical method described in Lecture

2, determine the following (and explain your working):

(a) The depth of the largest crater in this area of the Moon. How many times wider is this crater than its depth? [7]

(b) The height of the mountain that you identified in Question 5(g) [4]

(c) The depth of Hadley Rille closest to the Apollo 15 landing site. [4]

PART C: Geological map The Section relates only to Image 1. Overlie an A4-sized sheet of tracing paper over your A4- sized printout of Image 1 and proceed as follows:

(1) Draw in the boundaries of the image

(2) Mark in the rims of all craters larger than 2 km in diameter. Use tick marks to indicate interior slopes as follows:

(4) Draw in the boundaries between different geological units you can identify (there are at least two, but if you can identify others you should include these). Devise a colour scheme for your units, and colour or shade them as appropriate. Your finished map should include a scale, key, and orientation. [30]

(5) Draw a line between (0, 27) and (115, 150); label the ends A and B respectively.

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Sample Answer

Geology of the Solar System I

Introduction

This practical report analyses a set of Lunar Orbiter images covering a region of the Moon located at approximately 13°N, 4°E, between Mare Imbrium and Mare Serenitatis. The area is geologically significant as it includes Hadley Rille and the Apollo 15 landing site. By interpreting surface features, shadow geometry and spatial relationships visible in the images, it is possible to reconstruct aspects of lunar surface geology and topography.

The report follows the structure of the practical assessment. Part A focuses on orientation, scale and feature identification. Part B applies trigonometry to estimate the heights and depths of selected lunar features using shadow measurements and the given Sun elevation angle. Part C outlines the construction of a geological map based on Image 1 and interprets the major geological units present.

Part A: Orientation and Feature Identification

Scale Determination

The Lunar Orbiter images are composed of parallel strips running approximately east to west, with each strip representing 11 km on the lunar surface. Measuring the width of a single strip on the printed image gives an average value of approximately 0.55 cm. Dividing the real distance by the measured distance gives a scale of:

11 km ÷ 0.55 cm = 20 km per cm

This scale was used consistently throughout the practical to convert all measured distances into real lunar distances.

Direction of the Sun

Shadows cast by craters, rilles and mountains consistently fall towards the west on all three images. Since shadows extend in the opposite direction to the incoming sunlight, this indicates that the Sun was located toward the east when the images were taken.

Lunar Time of Day

Given that the Sun was shining from the east, this part of the Moon was experiencing morning at the time the images were acquired. This conclusion is supported by the presence of long shadows, which are characteristic of low Sun angles shortly after lunar sunrise. The provided Sun elevation of 22° above the horizon is consistent with early lunar morning conditions rather than midday, when shadows would be much shorter.

Apollo 15 Landing Site

Apollo 15 landed at approximately (87 km, 100 km) in Image 1. Examination of this location shows a relatively smooth, low-relief surface with fewer large craters compared to the surrounding highlands. This surface is characteristic of mare basalt, formed by ancient volcanic lava flows that filled low-lying regions. The choice of a mare surface for landing would have provided a safer, flatter terrain for the mission.

Identification of Lunar Features

Using the coordinate system described, the following features were identified across the three images. Coordinates are given to the nearest kilometre.

A sinuous rille other than Hadley Rille was identified in Image 2 at approximately (60 km, 140 km). Its meandering shape suggests formation by volcanic processes, likely involving flowing lava.

A straight rille was observed in Image 1 at approximately (40 km, 80 km). Its linear form indicates formation by tectonic extension and crustal faulting.

An arcuate rille was identified in Image 3 at approximately (110 km, 95 km). Its curved shape suggests a relationship with subsurface stress around an impact basin.

A clear non-lunar blemish, visible as a sharp-edged dark mark inconsistent with lunar geology, appears in Image 2 at approximately (20 km, 30 km).

A simple crater was identified in Image 1 at approximately (25 km, 45 km). It has a bowl-shaped profile and lacks central peaks or terraced walls.

A crater transitioning between simple and complex forms appears in Image 3 at approximately (90 km, 120 km). This crater shows early wall terracing but no fully developed central peak.

A tall mountain was identified in Image 1 at approximately (70 km, 130 km). It casts a long shadow and appears to be part of the lunar highlands bordering the mare.

An island of highland material surrounded by mare basalt is visible in Image 1 at approximately (100 km, 60 km). Its higher albedo and rougher texture distinguish it clearly from the surrounding smooth mare.

No. Small variations are expected due to printing and measurement differences.

Because without an atmosphere, shadows are sharp and allow accurate height calculations.

Yes, as long as estimates are reasonable and consistent with the scale.

They are formed from volcanic lava flows that filled low areas.

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