Anne Phillips (geologist)


Anne Phillips was an English geologist. She is most notable for discovering a fragment of conglomerate that helped clarify the history of the Malvern Hills. and assisting her brother John Phillips.

Early life

Anne Phillips was born in Midford, Somerset, in 1803 to Elizabeth and John Phillips. She had two older siblings, John, who also became a geologist, and Ann; Ann died during infancy. John was born in 1800 in Marden, Kent. In 1801, the family moved to Midford, Somerset, and they are believed to have stayed at a property, Tucking Mill House, owned by Elizabeth's brother, William Smith. He was a geologist known for authoring the first geological map of England and developing the basis for the science of stratigraphy. After Anne's birth in 1803, the family moved to Steeple Aston, Oxfordshire. Anne's younger brother, Jenkin, was born in 1807; the family subsequently moved to Coventry. Although some information has been published through letters from her brother John, much of Anne's upbringing and education remains a mystery.
The elder John Phillips died in Coventry in January 1808, and Elizabeth in turn died in July after the family had moved to her hometown of Churchill, Somerset. Following the death of her mother, Anne's maternal uncles took care of the orphans. Daniel Smith looked after Jenkin in the village of Churchill, near Chipping Norton in Oxfordshire, while William Smith took John and Anne to Broadfield Farm, which was owned by John Smith.

Relationship with John Phillips

Having been orphaned at a young age, Anne Phillips and her brother John became close. In 1829, for reasons still undiscovered, Anne was residing in the home of Monsieur and Madame Goussaerts in Chateau Koekelberg, in Belgium. John arranged to meet her in Brussels, then later in Paris. During their meeting in Paris, John asked Anne to return to York, where he would supply Anne with employment. In 1829 she was appointed his housekeeper, a position she held for thirty-three years. In September of the same year, she began aiding John in his geological work. Both remained unmarried; he regarded her with great respect and depended on her, including in his work. His scientific friends accepted her because of their close relationship and, most likely, her geographic knowledge. John's letters present evidence for Anne’s intellectual accomplishments by asking about the details of geologic studies with the use of his drawings and requesting her applied geological assistance.
Anne became involved in her brother John's geological work, working primarily as his field assistant starting in 1829. John Phillips worked to further William Smith's ideas on using fossils to prove stratigraphy correct. One of John Phillips greatest contributions was naming the major geological eras and the mass extinctions that separated them. John Phillips initially believed that Murchison's accepted view on formation was wrong and his sister helped prove his doubts right. This idea would go on to be seen as Anne's greatest geological achievement. John Phillips success can be attributed to years of hard work but also the support of his sister Anne. The 234 letters written by John to his sister help us understand that Anne was able to provide John plenty of scientific and emotional support for her brother.

Scientific contributions

Anne Phillips' most notable geological achievement was the discovery of scattered broken pieces conglomerate, now known as Miss Phillips Conglomerate. This type of rock became popular as samples of it soon became collectable items on geological field trips.
Sir Roderick Murchison was the primary advocate of the first Malvern theory which was labeled “The Silurian system”. This system asserted that first the Silurian sediments were formed, and afterwards were interjected with the hot rock of the Malvern Ridge. He felt that the Malvern ridge was intruded as a hot body after the Silurian sediments were laid down.
Miss Phillips Conglomerate supported the position of John Phillips. Phillips believed that the Silurians are not truly changed by the intrusives even though they are in sparing contact with them. The piece of evidence credited to Anne Phillips was the literal conglomerate of rock she found in the Malverns that demonstrated that her brother's theory was in fact the correct one, as it showed the two different types of rock meeting without any sort of overrunning of one into the other.
In 1842, Anne, accompanied by her brother and his employer, Sir Henry De la Beche, located a place where conglomerate could be seen in contact with one or more intrusive rocks. This survey proved the idea of how rocks in the Malvern Hills were initially moulded, and how the Silurian Sediments were positioned by an ancient sea that broke down due to the Malvern’s igneous shores. This was a major geological contribution as it resolved the mystery at the time of the origin of these hills and proved Sir Rodrick Impey Murchison wrong. Sir Rodrick was a British geologist and the husband of Scottish geologist, Charlotte Murchison. He had argued that the igneous rocks were younger than the Silurian sediments which then formed and made their way up. However, Anne discovered an outcrop of conglomerate containing fragments of igneous hills near the Dingle Quarry in Malvern, proving Murchison's theory as incorrect. This meant the Malvern hills had formed first. The conglomerate provided an anti-murchisonian theory. John gave his sister full credit for the discovery of the conglomerate. The report of the discovery was published in London, Edinburgh and Dublin Philosophical Magazine and Journal of Science in October 1842:
"My sister, knowing the interest I felt in tracing out the history of the stratification visible in these trap hills, sought diligently for organic remains... In this most unpromising search she was entirely successful, and collected... several masses richly charged with organic remains"
In the article he explains that his sister knew about how much he was interested in finding the history of the hills and how he was looking for organic remains. Phillips was not publicly recognized for any further discoveries, however, in letters penned to her by her brother, she was applauded and thanked for her assistance in his work and for always being successful in every search. In the letters, he also asks for geological help and refers to the work she did for his Guide to Geology, as he goes on to say that it was 'Your Little Book'. In a 1864 review written by Longmans it is noted that John was not yet a professor but was Secretary of the British Association and a member of the Royal Society. Longman states the first edition included problems of mineral composition, rock masses, distribution of life, and formation of igneous rock.
Anne and John had a good relationship with William Smith and they always kept in touch. Smith acknowledged Anne’s work and referred to the contributions she made to her brother’s book. In one of his letters to Anne he thanked her for the second edition of John’s book Guide to Geology and wrote that her love for fossils encouraged him to do more searches.
It is believed that Anne may have contributed to more geologic research.

Death and legacy

Over the course of her life, Anne Phillips acted mainly as John's geological companion. His requests often included having Anne send boxes of fossils to his office in London or colouring detailed maps for his novels. Her contributions assisted John in his geologic endeavours. John is publicly grateful towards his sister as he states in 1838 “Whatever I possess is as much yours as mine, for without you I should not have won it ." Towards the end of 1862, Anne Phillips moved to a household that was rented by her brother, where she aided him by sorting and cataloging the fossils and minerals he collected.
Anne died in 1862, where she is buried alongside her brother, John Phillips, in the city of York. The Hope Library at the Oxford University Museum of Natural History holds 234 letters sent between John Phillips and Anne Phillips.
As information currently known about Anne was taken from the letters written by her brother John, given that none of her own letters are intact.