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cally； the lengthwould shorten as you moved away from the poles。 this was not good news for those peoplewhose measurements of the earth were based on the assumption that the earth was a perfectsphere； which was everyone。
for half a century people had been trying to work out the size of the earth； mostly bymaking very exacting measurements。 one of the first such attempts was by an englishmathematician named richard norwood。 as a young man norwood had traveled to bermudawith a diving bell modeled on halley鈥檚 device； intending to make a fortune scooping pearlsfrom the seabed。 the scheme failed because there were no pearls and anyway norwood鈥檚 belldidn鈥檛 work； but norwood was not one to waste an experience。 in the early seventeenthcentury bermuda was well known among ships鈥櫋aptains for being hard to locate。 theproblem was that the ocean was big； bermuda small； and the navigational tools for dealingwith this disparity hopelessly inadequate。 there wasn鈥檛 even yet an agreed length for anautical mile。 over the breadth of an ocean the smallest miscalculations would beemagnified so that ships often missed bermuda…sized targets by dismaying margins。 norwood；whose first love was trigonometry and thus angles； decided to bring a little mathematical rigorto navigation and to that end he determined to calculate the length of a degree。
starting with his back against the tower of london； norwood spent two devoted yearsmarching 208 miles north to york； repeatedly stretching and measuring a length of chain ashe went； all the while making the most meticulous adjustments for the rise and fall of the landand the meanderings of the road。 the final step was to measure the angle of the sun at york atthe same time of day and on the same day of the year as he had made his first measurement inlondon。 from this； he reasoned he could determine the length of one degree of the earth鈥檚meridian and thus calculate the distance around the whole。 it was an almost ludicrouslyambitious undertaking鈥攁 mistake of the slightest fraction of a degree would throw the wholething out by miles鈥攂ut in fact； as norwood proudly declaimed； he was accurate to 鈥渨ithin ascantling鈥濃�攐r； more precisely； to within about six hundred yards。 in metric terms； his figureworked out at 110。72 kilometers per degree of arc。
in 1637； norwood鈥檚 masterwork of navigation； the seaman鈥檚 practice ； was published andfound an immediate following。 it went through seventeen editions and was still in printtwenty…five years after his death。 norwood returned to bermuda with his family； being a2how fast you are spinning depends on where you are。 the speed of the earth鈥檚 spin varies from a little over1；000 miles an hour at the equator to 0 at the poles。
successful planter and devoting his leisure hours to his first love； trigonometry。 he survivedthere for thirty…eight years and it would be pleasing to report that he passed this span inhappiness and adulation。 in fact； he didn鈥檛。 on the crossing from england； his two young sonswere placed in a cabin with the reverend nathaniel white； and somehow so successfullytraumatized the young vicar that he devoted much of the rest of his career to persecutingnorwood in any small way he could think of。
norwood鈥檚 two daughters brought their father additional pain by making poor marriages。
one of the husbands； possibly incited by the vicar； continually laid small charges againstnorwood in court； causing him much exasperation and necessitating repeated trips acrossbermuda to defend himself。 finally in the 1650s witch trials came to bermuda and norwoodspent his final years in severe unease that his papers on trigonometry； with their arcanesymbols； would be taken as munications with the devil and that he would be treated to adreadful execution。 so little is known of norwood that it may in fact be that he deserved hisunhappy declining years。 what is certainly true is that he got them。
meanwhile； the momentum for determining the earth鈥檚 circumference passed to france。
there； the astronomer jean picard devised an impressively plicated method oftriangulation involving quadrants； pendulum clocks； zenith sectors； and telescopes （forobserving the motions of the moons of jupiter）。 after two years of trundling and triangulatinghis way across france； in 1669 he announced a more accurate measure of 110。46 kilometersfor one degree of arc。 this was a great source of pride for the french； but it was predicated onthe assumption that the earth was a perfect sphere鈥攚hich newton now said it was not。
to plicate matters； after picard鈥檚 death the father…and…son team of giovanni andjacques cassini repeated picard鈥檚 experiments over a larger area and came up with results thatsuggested that the earth was fatter not at the equator but at the poles鈥攖hat newton； in otherwords； was exactly wrong。 it was this that prompted the academy of sciences to dispatchbouguer and la condamine to south america to take new measurements。
they chose the andes because they needed to measure near the equator； to determine ifthere really was a difference in sphericity there； and because they reasoned that mountainswould give them good sightlines。 in fact； the mountains of peru were so constantly lost incloud that the team often had to wait weeks for an hour鈥檚 clear surveying。 on top of that； theyhad selected one of the most nearly impossible terrains on earth。 peruvians refer to theirlandscape as muy accidentado 鈥斺�渕uch accidented鈥濃�攁nd this it most certainly is。 thefrench had not only to scale some of the world鈥檚 most challenging mountains鈥攎ountainsthat defeated even their mules鈥攂ut to reach the mountains they had to ford wild rivers； hacktheir way through jungles； and cross miles of high； stony desert； nearly all of it uncharted andfar from any source of supplies。 but bouguer and la condamine were nothing if nottenacious； and they stuck to the task for nine and a half long； grim； sun…blistered years。
shortly before concluding the project； they received word that a second french team； takingmeasurements in northern scandinavia （and facing notable disforts of their own； fromsquelching bogs to dangerous ice floes）； had found that a degree was in fact longer near thepoles； as newton had promised。 the earth was forty…three kilometers stouter when measuredequatorially than when measured from top to bottom around the poles。
bouguer and la condamine thus had spent nearly a decade working toward a result theydidn鈥檛 wish to find only to learn now that they weren鈥檛 even the first to find it。 listlessly； they pleted their survey； which confirmed that the first french team was correct。 then； still notspeaking； they returned to the coast and took separate ships home。
something else conjectured by newton in the principia was that a plumb bob hung near amountain would incline very slightly toward the mountain； affected by the mountain鈥檚gravitational mass as well as by the earth鈥檚。 this was more than a curious fact。 if youmeasured the deflection accurately and worked out the mass of the mountain； you couldcalculate the universal gravitational constant鈥攖hat is； the basic value of gravity； known asg鈥攁nd along with it the mass of the earth。
bouguer and la condamine had tried this on peru鈥檚 mount chimborazo； but had beendefeated by both the technical difficulties and their own squabbling； and so the notion laydormant for another thirty years until resurrected in england by nevil maskelyne； theastronomer royal。 in dava sobel鈥檚 popular book longitude； maskelyne is presented as a ninnyand villain for failing to appreciate the brilliance of the clockmaker john harrison； and thismay be so； but we are indebted to him in other ways not mentioned in her book； not least forhis successful scheme to weigh the earth。 maskelyne realized that the nub of the problem laywith finding a mountain of sufficiently regular shape to judge its mass。
at his urging； the royal society agreed to engage a reliable figure to tour the british islesto see if such a mountain could be found。 maskelyne knew just such a person鈥攖heastronomer and surveyor charles mason。 maskelyne and mason had bee friends elevenyears earlier while engaged in a project to measure an astronomical event of great importance：
the passage of the planet venus across the face of the sun。 the tireless edmond halley hadsuggested years before that if you measured one of these passages from selected points on theearth； you could use the principles of triangulation to work out the distance to the sun； andfrom that calibrate the distances to all the other bodies in the solar system。
unfortunately； transits of venus； as they are known； are an irregular occurrence。 theye in pairs eight years apart； but then are absent for a century or more； and there were nonein halley鈥檚 lifetime。
3but the idea simmered and when the next transit came due in 1761；nearly two decades after halley鈥檚 death； the scientific world was ready鈥攊ndeed； more readythan it had been for an astronomical event before。
with the instinct for ordeal that characterized the age； scientists set off for more than ahundred locations around the globe鈥攖o siberia； china； south africa； indonesia； and thewoods of wisconsin； among many