Goyder crater

{{Short description|Impact crater in Northern Territory, Australia}}

{{Other uses|Goyder (disambiguation){{!}}Goyder}}

{{Use Australian English|date=May 2024}}

{{Infobox terrestrial impact site

| name = Goyder crater

| other_name =

| photo = Goyder crater.jpg

| photo_size =

| photo_alt =

| photo_caption = Landsat image of the central uplift of Goyder crater (circular feature in centre); screen capture from World Wind (scale is 3 km)

| map = Northern Territory

| map_alt =

| map_caption = Location of the crater in the Northern Territory

| map_size =

| location = Arnhem Land

| label =

| label_position =

| coordinates = {{coord|13.476|S|135.043|E|display=inline,title}}

| coordinates_ref =

| confidence = Confirmed

| diameter = {{convert|9|-|12|km|mi|abbr=on}}

| depth =

| rise =

| imp_size =

| age = <Mesoproterozoic

| exposed = Yes

| drilled = No

| bolide =

| translation =

| language =

| pronunciation =

| topo =

| access =

| country = Australia

| state = Northern Territory

| province =

| district =

| municipality =

}}

Goyder is an impact structure (or astrobleme), the eroded remnant of a former impact crater. It is situated in Arnhem Land in the Northern Territory, Australia, and was named after the nearby Goyder River. The impact occurred into Mesoproterozoic sedimentary rocks of the McArthur Basin. The deformed area is exposed at the surface and marked by a 3 km diameter ring of fractured and faulted sandstone, which is interpreted as the eroded relic of a central uplift (material that rebounded within the crater to once form a central peak); the original crater rim, long since removed by erosion, being estimated at approximately 9–12 km diameter.{{cite journal | author=Haines PW | title=Impact cratering and distal ejecta: the Australian record | journal=Australian Journal of Earth Sciences | volume=52 | issue= 4-5| year=2005 | pages=481–507 | doi=10.1080/08120090500170351|bibcode = 2005AuJES..52..481H }} [https://web.archive.org/web/20210728081831/http://journalsonline.tandf.co.uk/link.asp?id=n0396841487037g4 Abstract]
Evidence for an impact origin includes the presence of shatter cones and shocked quartz in outcrops of deformed sandstone at the center of the site.{{cite journal | author=Haines PW | title=Goyder impact structure, Arnhem Land, Northern Territory | journal=AGSO Journal of Australian Geology & Geophysics | volume=16 | year=1996 | pages=561–66}}

{{cite web

| title = Goyder

| url = http://www.passc.net/EarthImpactDatabase/goyder.html

| access-date = 13 August 2009

| website = Earth Impact DB

| archive-url =https://web.archive.org/web/20180701022918/http://www.passc.net/EarthImpactDatabase/goyder.html

| archive-date = 1 July 2018

}}

Age

The time of impact cannot be accurately constrained, however, it probably happened more recently than 1325 Ma (middle Mesoproterozoic), which is the age of igneous rocks that are inferred to have been uplifted by the impact based on aeromagnetic evidence, and significantly older than Cretaceous. The site is very remote and difficult to access.

See also

References

{{reflist}}

{{Impact cratering on Earth}}

{{DEFAULTSORT:Goyder Crater}}

Category:Impact craters of the Northern Territory