The Jodrell Plank Observatory
Wednesday, 17 June 2026
Deep Time and the Cosmos
Tuesday, 16 June 2026
Kurt Thrust is unwell.
![]() |
| Image Credit: SOHO Solar Observatory. Lower image derived from the SOHO image and processed by Kurt on his smartphone. |
" The trouble with having a very old astronomer, like Kurt Thrust as the Observatory Director, is that sooner or later they become a bit unwell and unable to do their job. Quite honestly, the JPO Team has been covering for him for some time and we all have been keeping him going with a steady stream of tea, sympathy and incontinence pads. Anyway and quite unexpectedly, Kurt was admitted to hospital for tests but we hope to see his return to the Observatory in the next few days. In the meantime, he has insisted that posts should continue and that the blog should not go 'Dark'. What an astronomical trooper!ðŸ”🤣" Joel Cairo CEO of the JPO the UK's most easterly Astronomical Observatory
" The above images showing the current view of the solar photosphere were obtained and derived from the SOHO satellite. I was rather annoyed, that I wasn't back at the Jodrell Plank Observatory and able to image sunspot group 4465 using the 127mm apo refractor, a Baader white light filter and our latest fast video camera. I'm down but not out! " Kurt Thrust still the current Director of the Jodrell Plank Observatory.
Wednesday, 10 June 2026
The Flaming Star in the constellation Auriga - NGC 405
![]() |
| NGC 405 The Flaming Star Reflection Nebula in the Constellation Auriga. Seestar S30. Processed in RGB -SHO palette. Image Credit: Pip Stakkert. |
" The one thing we have in depth at the Jodrell Plank Observatory is data! Loads of the stuff held; on drives, memory sticks and discs from times gone by! So when the nights become short in summer or when the weather takes a turn for the worse, our team at the JPO resort to the existing data for 'shots and giggles'.
"The Flaming Star Nebula, designated IC 405, is a complex emission and reflection nebula located approximately 1,500 light-years from Earth in the constellation Auriga. It is one of the most striking examples of a nebular region in which both ionized gas and interstellar dust contribute significantly to the observed appearance.
At the heart of the nebula lies the hot, blue O-type star AE Aurigae, whose intense ultraviolet radiation interacts with the surrounding interstellar medium. The red portions of IC 405 are produced by emission nebula processes: ultraviolet photons from AE Aurigae ionize hydrogen atoms within the gas cloud, and when the electrons recombine with the hydrogen nuclei, they emit characteristic red hydrogen-alpha radiation. Interwoven with these glowing regions are blue filaments and wisps formed by reflection nebula processes, where microscopic dust grains scatter and reflect the blue light of the star. This combination of red emission and blue reflection gives the nebula its distinctive colour contrast.
The nebula's dramatic “flaming” appearance arises from complex filamentary structures of gas and dust that seem to stream away from AE Aurigae in long-exposure images. Current evidence suggests that AE Aurigae is a runaway star, moving at high velocity through the interstellar medium after being ejected from the region of the Orion Nebula several million years ago. As the star travels through the cloud, its radiation and stellar wind compress, heat, and illuminate the surrounding material, helping to shape the nebula's intricate morphology.
Infrared and ultraviolet observations have revealed that IC 405 contains not only ionized hydrogen but also molecular hydrogen, warm dust, and complex carbon-bearing molecules. The interaction between AE Aurigae and the nebular material produces shock fronts and regions of enhanced heating, making IC 405 an important laboratory for studying the physics of star–cloud interactions, dust scattering, molecular excitation, and the evolution of the interstellar medium".
Scientifically, the Flaming Star Nebula is therefore not merely a visually beautiful object; it is a dynamic astrophysical environment in which radiation, gas dynamics, dust physics, and stellar motion combine to create a remarkable example of an emission–reflection nebular complex". - Professor G.P.T Chat visiting astrophysicist at the Jodrell Plank Observatory.
![]() |
| The same image of NGC405 but rendered in modified RGB palette. |
Tuesday, 9 June 2026
Double Bow over the JPO.
"Double Rainbow over the JPO, the UK's most easterly Astronomical Observatory". - Noah the Jodrell Plank Observatory shipping consultant.
The Sun and the Sky at Night - A Perfect Storm
![]() |
| Jolene's completed White and Red light Safety Solar Filter used with the JPO's Seestar S30 to capture recent images of the Solar Photosphere. |
https://www.flickr.com/photos/nightskyobserver/
https://www.flickr.com/groups/bbcskyatnight/
George received an email advising him that one of our solar images would be shown on The Sky at Night program to be broadcast on the 08 June BBC Four and subsequently made available on BBC iPlayer - 'Space Weather: The Perfect Storm'.
I have included a short and relevant video clip taken from iPlayer but would recommend those interested in 'space weather', to view the whole program, which is both informative and interesting." -Joel Cairo CEO of the Jodrell Plank Observatory.
Tuesday, 2 June 2026
Sinus Iridum - The Bay of Rainbows
![]() |
| Images captured from the Jodrell Plank Observatory using the 127 mm. Meade Apo Refractor and the Seestar S30. Data and image credit: Pip Stakkert. |
"The other evening, our imaging technician Pip was using the Seestar S30 to photograph the waxing gibbous lunar disc. He noticed that the 'Terminator' or 'daybreak on the Moon' was about to cross the prominent feature Sinus Iridum - The Bay of Rainbows. Sunlight had just touched the peaks of the crater walls creating the effect known as the 'golden handle'. This can just be seen top left in the bottom image". - Joel Cairo CEO of the Jodrell Plank Observatory.
Key features of Sinus Iridum - Lunar notes - from Professor G.P.T Chat visiting astrophysicist at the JPO.
Sinus Iridum
(Latin for "Bay of Rainbows") is one of the most striking
basalt-flooded impact structures on the near side of the Moon. It forms a broad
semicircular embayment on the northwestern margin of Mare Imbrium and is
enclosed by the rugged arc of the Montes Jura mountain range. To lunar
observers it appears as a near-perfect luminous crescent when illuminated at
low solar angles, making it one of the most recognizable features on the lunar
disc.
Position on the Lunar Disc
Sinus Iridum
lies at approximately 44°N latitude and 31°W longitude on the Moon's near side.
Because it occupies the northwestern sector of Mare Imbrium, it appears in the
Moon's upper-left quadrant as viewed through most astronomical telescopes that
present an upright image. The feature is roughly 240–260 km in diameter and
opens southeastward into Mare Imbrium. The enclosing Jura Mountains are
remnants of the original crater rim, rising locally several kilometres above
the mare floor.
Origin as a Large Impact Basin
Sinus Iridum
began as a major impact crater formed during the late stages of the heavy
bombardment that shaped much of the lunar crust. The impact excavated a large
bowl-shaped basin and produced an elevated rim composed largely of anorthositic
highland material. The southeastern portion of the rim was later breached and
largely buried when extensive volcanic flooding associated with Mare Imbrium
spread into the crater.
The result
is not a true bay in the terrestrial sense, but rather the flooded remains of a
large impact structure whose interior became connected to the surrounding mare
plains. The surviving rim forms the dramatic semicircular wall visible today.
Geological Composition
The floor of
Sinus Iridum consists predominantly of mare basalts emplaced during multiple
volcanic episodes. Remote-sensing studies using data from the Clementine
mission, Chandrayaan-1, the Lunar Reconnaissance Orbiter, and China's Chang'E
program show that these lavas vary in composition and age across the basin.
Key
geological characteristics include:
- Basaltic mare plains rich in pyroxene-bearing
volcanic rocks.
- Progression from low-titanium
basalts in older lava units to medium-titanium basalts in
younger units.
- Evidence for increasing olivine
abundance in some younger volcanic materials.
- Wrinkle ridges, tectonic
deformation features caused by contraction of cooling lava plains.
- Small impact craters, crater
chains, and rilles recording later geological modification.
The
surrounding Montes Jura remain compositionally distinct from the mare floor,
consisting mainly of feldspathic highland crust excavated during the original
impact event.
Age and Volcanic History
Modern
crater-count dating reveals that Sinus Iridum experienced a prolonged history
of volcanic resurfacing rather than a single flooding event.
The oldest
exposed mare units have model ages of approximately 3.37 billion years,
corresponding to the Imbrian period. Younger lava flows continued entering the
basin from Mare Imbrium for more than two billion years afterward. Some of the
youngest recognized basaltic units have ages near 1.24 billion years,
making them among the youngest extensive mare volcanics on the Moon.
The sequence
is interpreted as repeated episodes of lava entering the partially enclosed
basin from the larger Imbrium volcanic province. Rather than being filled from
a single central vent, Sinus Iridum appears to have been resurfaced multiple
times by flows arriving from adjacent mare regions.
Tectonic Evolution
Following
emplacement of the mare basalts, the region underwent tectonic deformation
associated with cooling and subsidence of the volcanic plains.
Researchers
using data from the Japanese SELENE (Kaguya) mission and NASA's Lunar Reconnaissance
Orbiter identified wrinkle ridges and compressional structures whose formation
may have continued into relatively recent lunar history. These structures
reflect crustal shortening caused by the weight and contraction of the basaltic
fill.
Spacecraft Investigations
Several
lunar missions have studied Sinus Iridum in detail.
NASA Missions
- The Lunar Reconnaissance
Orbiter has provided high-resolution imagery, topographic measurements
from LOLA, and compositional information used in modern geological
mapping.
- Earlier missions including Clementine
supplied multispectral data that helped determine iron and titanium
abundances.
Japanese Investigations
- SELENE obtained detailed terrain and
imaging data used to investigate tectonic structures and wrinkle ridges
throughout northwestern Mare Imbrium and Sinus Iridum.
Chinese Investigations
- Chang'e 2 produced high-resolution
imagery used in detailed geological mapping and age determinations.
- Sinus Iridum was seriously
evaluated as a candidate landing area for later Chinese robotic and
sample-return missions because of its smooth terrain and geological
diversity.
Although no
spacecraft has yet landed within Sinus Iridum itself, it remains scientifically
attractive because it exposes the interaction between impact-basin formation,
mare volcanism, and tectonic deformation in a single locality.
![]() |
| Captured from the JPO and previously published on the blog |
Sunday, 31 May 2026
Messier 3 - New Data and revised data processing methodology.
![]() |
| Messier 3 - Globular star Cluster in the Constellation Canes Venatici. Seestar S30 in Eq mode. 1 min x 60 subs Credit: Kurt Thrust at the JPO. |
" Our dedicated team of imagers and data processors has been experimenting with the application of the astro-freeware SIRIL and has used it to good affect in increasing the dynamic range of the M3 data captured on a clear night from the JPO in May this year. 'There is gold in them there 'data reduction' hills'" - Joel Cairo CEO of the Jodrell Plank Observatory.
"These images present the globular star cluster M3 — also catalogued as Messier 3 —
suspended against a richly populated stellar background in the constellation Canes
Venatici. Captured with a Seestar S30 smart telescope from the grounds of the Jodrell
Plank Observatory under the direction of Kurt Thrust, the observation reveals
one of the Milky Way’s most celebrated globular clusters: a gravitationally
bound sphere containing roughly half a million ancient stars compressed into a
region only a few hundred light-years across.
At a
distance of approximately 34,000 light-years from Earth, M3 appears as a
concentrated stellar nucleus whose luminosity rises sharply toward an intensely
radiant core. The cluster's structure is immediately apparent: a dense central
condensation surrounded by progressively looser stellar populations that
dissolve into the surrounding galactic field. This radial distribution is the
visible signature of a system that has remained gravitationally bound for more
than eleven billion years, surviving countless passages through the Milky Way's
halo while preserving a fossil record of the Galaxy's earliest epochs.
The warm
golden and reddish tones scattered throughout the cluster arise predominantly
from evolved red giant stars nearing the final stages of stellar evolution.
Intermixed among them are hotter blue-white stars, including the enigmatic
"blue stragglers" that appear younger than the rest of the cluster
population. Their presence suggests a dynamic environment where close stellar
encounters, mergers, and mass transfer events continue to reshape individual
stars despite the cluster's immense age.
M3 is
particularly significant to modern astrophysics because it hosts an
extraordinary population of variable stars, including a large number of RR
Lyrae variables whose rhythmic pulsations provide a fundamental rung on the
cosmic distance ladder. These stars act as standard candles, enabling
astronomers to measure distances across the Milky Way and beyond with
remarkable precision. More variable stars have been identified in M3 than in
almost any other known globular cluster, making it a natural laboratory for
studies of stellar evolution and pulsation physics.
The Seestar
S30 image demonstrates how modern compact smart telescopes can resolve
individual members of a globular cluster once accessible only to larger
observatory-class instruments. The cluster's sparkling granularity is evident
across the halo, where hundreds of individual stars emerge from what appears
visually as a diffuse cloud. Each point of light represents a sun in its own
right, collectively tracing a nearly spherical stellar ecosystem orbiting far
above the plane of the Milky Way.
Seen in this
observation, M3 is not merely a beautiful celestial object but a relic from the
early Universe: an ancient stellar metropolis whose stars formed when the Milky
Way itself was still young. The image captures a moment in an ongoing cosmic
history spanning billions of years, preserving within a single frame both the
elegance of gravitational order and the immense scale of galactic time". Professor G.P.T Chat visiting Astrophysicist at the Jodrell Plank Observatory.
![]() |
| Nucleus M3 - Image Credit: night-sky/hubble-messier-catalog |
















