A study about the Valentine dome : observations and classification.
PRELIMINARY ARTICLE

Submitted By: Raffaello Lena, KC Pau and Cristian Fattinnanzi.

Geologic Lunar Research  group- GLR

Introduction
In a previous paper [1], we have described Mons Rumker reporting the diameter, position and slopes of 4 single volcanic forms on its summit.
In this study we describe another complex dome located to the east of Caucasus Montains and west of crater Linnè B. The dome, known as "Valentine dome", appears flat with a series of protrusions on its summit.
Interestingly, this  dome is reported in ALPO list without specific details as to the position and diameter of the protrusions and the presence of a rille (Rima).
As described by Harold Hill in [2],  the presence of a rille was reported and drawn by  Alika Herring. His observation was carried out on june 25 1966 using a 61'' reflector [2].
By the way , in the Clementine imagery  a rille clearly crosses the dome.
To our knowledge the presence  of the rille is difficult to ascertain; in fact several images we examined don't show the presence of a central rille as in Clementine image
 

The "Valentine dome" has been well monitored from 1999 to 2003 during an observational program carried out by the GLR group. The rille is a difficult feature for visual and CCD observations (though Herring's drawing matches the Clementine image for the  position of the rille) .
Recently the rille was imaged by one of us   under a setting sun, near the moon's last quarter. Since this is period during lunation when comparatively fewer observers are active,this rille could have  generally eluded detection  (though it is noted in Clementine imagery and in Herring's drawing).

In  this study we report further   measurements and include our CCD imaging where the rille crossing  the dome was detected.
This has made it possible to extract additional information for the classification .

Instruments and Measures

Table 1 lists the observers, their instruments, and the number  of the  observations they supplied. For each observation, we calculated the solar altitude (H), azimuth (A), and colongitude, as seen from the dome, using the Lunar Observer's Tool Kit software by Harry Jamieson.
Furthermore we used CLA, LOPAM and  Clementine imagery.
The best images were rotated so that the shadows were oriented orizontally  along the pixel rows. On these images the position and the diameter of the positive forms was measured in units of pixels.
Furthermore  the scale of the images were obtained which allowed diameters of the concerned features A-D  to be expressed in km.
 

Our results are summarized in Tables  II and III.
 

Table I  Contributing observers  and  instruments
 

contributing
observers                 telescope                               type            Number of submitted reports

Bares  A.           Mewlon  250 mm f/10                  CCD                              2

Cicognani M.    Cassegrain 410 mm f/17       Visual and CCD                     2

Fattinnanzi C.     Newton  250 mm f/6                 Web-cam                          1

Giuntoli M.         SC 200 mm f/10                        Visual                              1

Lena R.              Refractor100 mm f/15               Visual                              3
                            SC 250 mm f/10

Mengoli G.          SC  250 mm f/10                         CCD                             2

Pau KC          Newton Cassegrain 200 f/11          Web Cam                        2
                            Newton 250 f/6
 
 

Table II- Valentine dome
 

Longitude       Latitude            Xi          Eta             Diameter (km)
+10.18  °       +30.66 °        +0.152      +0.510          27 x 33

Table III- Prominences located on the surface of the Valentine dome

Prominence     Longitude       Latitude        Diameter   (km)
1                       +10.25  °       +31.00 °        5.2x5.6
2                       +10.03  °       +30.88 °        5.4x4.8
3                       +10.11  °       +30.70 °        4.8x4.6
4                       +10.19  °       +30.49 °        5.4x5.2

Observations

Fig. 2 reports the Valentine dome. This image was obtained by Mengoli on 29 may 2001 at 18:57 UT ( H= 5.34 °, A =  94.06°, C =  356.47° ) using a SCT 250 mm f/10.
In addition Fig. 3 shows the Lunar Orbiter frame (LOIV-098) taken on May, 17, 1967 at 18:16 UT (colongitude 12.66°).
The image proposed in Figure 4  reveals much finer detail in the dome including the rille.
This image was obtained by Pau  on 16 september 2003 at 21:11 UT using a Newton 250 mm f/6 ( H= 8.69 °, A = 266.03°, C =  160.43° ) .
 
 


FIG 1 Clementine Image

Fig.2

Fig.3
 

Fig4
 
 

Discussion
The coordinates and the diameter of the Valentine dome is reported in Table II. From our measurement (coordinates 10.18° E and 30.66 º N) we estimated a diameter of 27 x 33 km. It should be noted that we have found differing coordinates for the same dome in the ALPO dome list  . Furthermore,  close inspection of several our images reveals diameter and , position  of 4 single prominences  on its summit (likely cones or tumuli, or peaks).
This dome is a difficul subject and,  as reported  by Hill in [2] it has been described by observers variously "as circular, elliptical as well as  heart shaped in outline".

Figure 4 (PAU) reveals the presence of a transversal rille crossing the summit of the dome that "matches" the figure 1.

Using all our available images  this dome may be newly  classified, according to the Westfall classification scheme,  as DW/3a/5g/8p 9 n.
 

The fact that  there have been, to our knowledge, only two previous reported observations of this rille in correct position, strongly suggests that this may be a very difficult object requiring specific lighting conditions in order to be clearly defined (appendix 1).

Conclusion
This report  demonstrates that lunar domes are difficult features for the lunar
observer. They require extreme patience and specific conditions of lunar solar altitude
and good seeing.
Finally the  rille was correctly imaged, suggesting it can be detected also in smaller earth-based telescopes.

This combined effort  clearly shows that the study and classification of these volcanic structures on the moon is far from being complete.
More observations and observers are needed worldwide in order to observe these important geologic lunar formations.
 

appendix 1

 dates and times to reproduce
 

   UT Date    Time
 2003/10/16   9: 5
 2003/11/14  21:38
 2004/ 1/13   0:55
 2004/ 3/12   5:33
 2004/ 7/ 8   7:56
 2004/ 9/ 5   6: 7
  UT Date    Time
 2004/11/ 3   5:48
 2005/ 1/ 1   8:55
 2005/ 1/30  23:30
 2005/ 3/31   4:20
 2005/ 5/29   6: 0
 2005/ 7/27   4:22