Lawn Hill crater
Encyclopedia
Lawn Hill ‘crater’ refers to an impact structure
the eroded remnant of a former impact crater
, situated approximately 220 km north-north-west of Mount Isa in northwestern Queensland
, Australia
. The site is marked by an 18 km diameter ring of limestone
hills. The origin of this circular feature was uncertain until the discovery of shatter cone
s and shocked quartz
from uplifted rocks at the centre was reported in 1987.
The site is heavily eroded and it has been suggested that the original crater was slightly larger, at around 20 km diameter. The age of the impact structure is somewhat contentious, in the absence of any radiometric dating
. The impact–shocked rocks at the centre of the site are early Mesoproterozoic
in age, which gives an absolute maximum possible age for the impact. In the past it has been debated whether the limestones, which are of Middle Cambrian
age (ca. 510 Ma) based on comparisons with nearby outcrops of marine limestone in the Georgina Basin
, were simply deposited in the crater after its formation, or were actually deformed by the impact event. Depending on the differing points of view, the crater may be of earlier Cambrian
or Proterozoic
age, or it could be of younger Paleozoic
age. The most recent study concludes that the impact most likely happened just before or even during the early stages of deposition of the limestone, suggesting an age of around 509–506 Ma (Middle Cambrian
).
Based on the theory that the crater was invaded by the sea just after the impact, the crater may have formed a unique protected microenvironment for primitive life, and could be an important analogue to craters filled with sediment in a similar way on Mars.
Impact structure
The term impact structure is closely related to the terms impact crater or meteorite impact crater, and is used in cases where erosion or burial have destroyed or masked the original topographic feature with which we normally associate the term crater...
the eroded remnant of a former impact crater
Impact crater
In the broadest sense, the term impact crater can be applied to any depression, natural or manmade, resulting from the high velocity impact of a projectile with a larger body...
, situated approximately 220 km north-north-west of Mount Isa in northwestern Queensland
Queensland
Queensland is a state of Australia, occupying the north-eastern section of the mainland continent. It is bordered by the Northern Territory, South Australia and New South Wales to the west, south-west and south respectively. To the east, Queensland is bordered by the Coral Sea and Pacific Ocean...
, Australia
Australia
Australia , officially the Commonwealth of Australia, is a country in the Southern Hemisphere comprising the mainland of the Australian continent, the island of Tasmania, and numerous smaller islands in the Indian and Pacific Oceans. It is the world's sixth-largest country by total area...
. The site is marked by an 18 km diameter ring of limestone
Limestone
Limestone is a sedimentary rock composed largely of the minerals calcite and aragonite, which are different crystal forms of calcium carbonate . Many limestones are composed from skeletal fragments of marine organisms such as coral or foraminifera....
hills. The origin of this circular feature was uncertain until the discovery of shatter cone
Shatter cone
Shatter cones are rare geological features that are only known to form in the bedrock beneath meteorite impact craters or underground nuclear explosions...
s and shocked quartz
Shocked quartz
Shocked quartz is a form of quartz that has a microscopic structure that is different from normal quartz. Under intense pressure , the crystalline structure of quartz will be deformed along planes inside the crystal...
from uplifted rocks at the centre was reported in 1987.
The site is heavily eroded and it has been suggested that the original crater was slightly larger, at around 20 km diameter. The age of the impact structure is somewhat contentious, in the absence of any radiometric dating
Radiometric dating
Radiometric dating is a technique used to date materials such as rocks, usually based on a comparison between the observed abundance of a naturally occurring radioactive isotope and its decay products, using known decay rates...
. The impact–shocked rocks at the centre of the site are early Mesoproterozoic
Mesoproterozoic
The Mesoproterozoic Era is a geologic era that occurred between 1600 Ma and 1000 Ma . The Mesoproterozoic was the first period of Earth's history with a respectable geological record. Continents existed in the Paleoproterozoic, but we know little about them...
in age, which gives an absolute maximum possible age for the impact. In the past it has been debated whether the limestones, which are of Middle Cambrian
Cambrian
The Cambrian is the first geological period of the Paleozoic Era, lasting from Mya ; it is succeeded by the Ordovician. Its subdivisions, and indeed its base, are somewhat in flux. The period was established by Adam Sedgwick, who named it after Cambria, the Latin name for Wales, where Britain's...
age (ca. 510 Ma) based on comparisons with nearby outcrops of marine limestone in the Georgina Basin
Georgina Basin
The Georgina Basin is a large intracratonic sedimentary basin in central and northern Australia, lying mostly within the Northern Territory and partly within Queensland. It is named after the Georgina River which drains part of the basin. Deposition of locally up to ca...
, were simply deposited in the crater after its formation, or were actually deformed by the impact event. Depending on the differing points of view, the crater may be of earlier Cambrian
Cambrian
The Cambrian is the first geological period of the Paleozoic Era, lasting from Mya ; it is succeeded by the Ordovician. Its subdivisions, and indeed its base, are somewhat in flux. The period was established by Adam Sedgwick, who named it after Cambria, the Latin name for Wales, where Britain's...
or Proterozoic
Proterozoic
The Proterozoic is a geological eon representing a period before the first abundant complex life on Earth. The name Proterozoic comes from the Greek "earlier life"...
age, or it could be of younger Paleozoic
Paleozoic
The Paleozoic era is the earliest of three geologic eras of the Phanerozoic eon, spanning from roughly...
age. The most recent study concludes that the impact most likely happened just before or even during the early stages of deposition of the limestone, suggesting an age of around 509–506 Ma (Middle Cambrian
Cambrian
The Cambrian is the first geological period of the Paleozoic Era, lasting from Mya ; it is succeeded by the Ordovician. Its subdivisions, and indeed its base, are somewhat in flux. The period was established by Adam Sedgwick, who named it after Cambria, the Latin name for Wales, where Britain's...
).
Based on the theory that the crater was invaded by the sea just after the impact, the crater may have formed a unique protected microenvironment for primitive life, and could be an important analogue to craters filled with sediment in a similar way on Mars.