Skip to main content Accessibility help
×
Hostname: page-component-cd9895bd7-jkksz Total loading time: 0 Render date: 2024-12-26T03:02:22.005Z Has data issue: false hasContentIssue false
This chapter is part of a book that is no longer available to purchase from Cambridge Core

11 - The Case of the Alien Agent—Solution

from The Solutions

R. Grant Woods
Affiliation:
The University of Manitoba
Get access

Summary

TOP SECRET

For the eyes of the Core Cell of Alienwatch only.

Analysis of the freutcaquium layer

As you may know, one of your members anonymously sent us top secret documents giving the calculation by the IPP of the volume of freutcaquium fallout in the Earth's crust. He (or she) pointed out that this calculation did not take into account the curvature of the Earth, and might therefore have overestimated the actual amount of freutcaquium that settled on our planet. If this were true, the amount of freutcaquium might have been insufficient to wipe out the ancient aliens that you (and we) believe may have populated the Earth at that time.

However, our calculations seem to indicate that the error made by the IPP did not cause their results to be incorrect by more than at most 3%, which is probably within the experimental error in the field measurements obtained by the IPP geologists. We present our calculations below, and invite you to verify them.

The layer of freutcaquium can be thought of as a solid of revolution obtained as follows. Consider a circle K of radius R with center at the origin. Above the portion of the circle in the first quadrant consider a curve C with the following property: if 0 ≤ θ ≤ α ≤ π/4, and if L(θ) is a line through the origin O lying in the first quadrant and making an angle θ with the Y-axis, then the distance along L(θ), from O to C is R + s(θ), where s(θ) is defined to be d — (dθ/α) (see Figure A).

Type
Chapter
Information
Publisher: Mathematical Association of America
Print publication year: 1998

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure [email protected] is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×